. -Forestry. Main Library •b\°l STUDIES IN FORESTRY NISBET HENRY FROWDE OXFORD UNIVERSITY PRESS WAREHOUSE AMEN CORNER, E.G. MACMILLAN & CO., 66 FIFTH AVENUE STUDIES IN FORESTRY BEING A SHORT COURSE OF LECTURES ON THE PRINCIPLES OF SYLVICULTURE DELIVERED AT THE BOTANIC GARDEN, OXFORD During the Hilary and Michaelmas Terms, 1893 BY JOHN NISBET, D.OEC. OF THE INDIAN FOREST SERVICE AUTHOR OF 'BRITISH FOREST TREES' EDITOR OF THE SIXTH EDITION OF BROWN'S 'THE FORESTER' TRANSLATOR OF KAUSCHINGER AND FURST'S 'PROTECTION OF WOODLANDS,' AND OF HARTIG'S 'ANATOMY AND PHYSIOLOGY OF PLANTS,' ETC. AT THE CLARENDON PRESS 1894 SD37-3 N/fc .« Arric.-Ft>r*Btrv. Main Librar? PRINTED AT THE CLARENDON PRESS BY HORACE HART, PRINTER TO THE UNIVERSITY PREFACE THE various chapters of the present work formed two short courses of lectures on the Principles of Sylviculture, which were delivered, during the Lent and Michaelmas Terms of last year (1893), at tne Botanic Garden in Oxford, where Professor Vines, F.R.S., was good enough to arrange for their delivery in his class-room. I am further indebted to him for kind assistance given during the revision of the proofs, and gladly take this opportunity of tendering my thanks to him on both accounts. With the permission of the Secretary of State for India, I have been enabled to make several of the chapters more complete than they might otherwise have been, by utilizing freely the greater portion of a series of six Essays on Sylvi- cultural Subjects, which were written by me in Bavaria during 1892, and were published in 1893 by the Government of India for distribution among their Forest Officers. As will be apparent throughout every chapter, my convictions regarding economic Forestry, i. e. Sylviculture, have been formed in a Teutonic school. But Science is Truth ; and in acquiring information with regard to the growth of Forest Trees, or concerning any other branch of natural knowledge, it ought to be a matter of perfect indifference from what well this may 78M6O viii Preface be drawn. I have therefore had no hesitation in boldly acknowledging the German sources from which many of the lessons I am trying to teach have been learned. With regard to Forestry, Britain stands in a very peculiar position. Although she has now only a very insignificant area under woodlands in comparison with any other great European power, yet all her national and commercial prosperity is mainly due to her forest wealth — first of all, in the time of the formation of the coal-measures, and later on again in the days of the ' wooden walls of England.' For what could the ' Hearts of Oak ' have achieved in the way of naval supremacy without the ships of home-grown Oak? It is not because Germany has a forest area fully eleven times as large as the woodlands and nurseries of Great Britain and Ireland that we must look mainly to that country for instruction and guidance with regard to Forestry; it is because at Universities, Academies, Institutes, and Forest Schools, many Professors of high scientific attainments are engaged not only in teaching the Science of Forestry and the Art of Sylviculture, but also in individual and conjoint efforts and investigations for ascertaining the natural laws which regulate the growth of timber-crops. In Britain, however, nothing of this sort is going on. There is no body of men of anything like good scientific attainments who are known to be carrying on investigations that have for their object the improvement of our natural knowledge regard- ing the growth of timber. Times have changed since one of the oldest and most remarkable of the English works on Forestry, John Evelyn's classic Silva or a Discourse of fores I Trees, was read by him in its first form as a paper before the Royal Society in October, 1664; for at that time we were certainly abreast of continental knowledge. But, with the Preface ix subsequent decrease in the woodland area throughout Britain, we have lagged far behind continental countries with regard to the improvement of our knowledge of Forestry. With the present shrinkage in the agricultural and pastural value of land, however, there certainly is now scope for applying a knowledge of economic and purely financial Forestry, i. e. Sylviculture, to considerable tracts that are now lying waste and unproductive. It may perhaps be convenient, for the sake of ready refer- ence, to give a short list of the chief works that have been frequently quoted throughout the various chapters of this book. These are : — GREBE, Die Betriebs- und Ertragsregelung der Forste, and edit., 1879. NEY, Die Lehre vom Waldbau, 1885. WEBER, Die Aufgaben der Forstwirthschaft, in Lorey's Handbuch der Forstwissenschaft, vol. i. 1886. WILLKOMM, Die Forstliche Flora von Deutschland und Oesterreich, 2nd edit., 1887. HESS, Der Forstschutz, and edit., vol. i. 1887 ; vol. ii. 1890. GAYER, Die Forstbenutzung, 7th edit., 1888. — Der Waldbau, 3rd edit., 1889. R. HARTIG, Lehrbuch der Baumkrankheiten, and edit. 1889. Anatomic und Physiologic der Pflanzen, 1891. C. HEYER, Der Waldbau, 4th edit., vol. i. 1891 ; vol. ii. 1893. RAMANN, Forstliche Bodenkunde und Klimatologie , 1893. J. NlSBET. 145 NORWICH ROAD, IPSWICH : March, 1894. CONTENTS CHAPTER I. FORESTRY IN BRITAIN CHAPTER II. THE BRITISH SYLVA, AND THE GROWTH OF WOODLAND CROPS IN GENERAL .......... 29 CHAPTER III. THE CHIEF SYLVICULTURAL CHARACTERISTICS OF OUR WOOD- LAND TREES *. ....... 46 CHAPTER IV. THE NUTRITION AND FOOD-SUPPLIES OF WOODLAND CROPS . 67 CHAPTER V. SOIL AND SITUATION IN RELATION TO WOODLAND GROWTH . 90 CHAPTER VI. ON THE ADVANTAGES OF MIXED TIMBER-CROPS OVER PURE WOODS ........... 115 CHAPTER VII. CONCERNING THE FORMATION AND GENERAL TREATMENT OF MIXED WOODS . . ..... .. .138 CHAPTER VIII. CONCERNING THE FORMATION AND REGENERATION OF WOOD- LAND CROPS .......... 158 xii Contents CHAPTER IX. PAGE THE TENDING OF WOODS . . . * , . . .179 CHAPTER X. METHODS OF STIMULATING THE INCREMENT IN TIMBER-CROPS WHEN APPROACHING MATURITY . . . • • . 2IO CHAPTER XL THE PRACTICAL EFFECTS OF UNDERPLANTING . . . .230 CHAPTER XII. THE CONSERVATION OF THE PRODUCTIVE CAPACITY OF WOOD- LAND SOILS . . 253 CHAPTER XIII. THE FUNGOID DISEASES OF FOREST TREES, AND THEIR PRE- VENTION » 276 CHAPTER XIV. THE PROTECTION OF WOODLANDS AGAINST INSECT ENEMIES . 307 INDEX . 333 STUDIES IN FORESTRY CHAPTER I V FORESTRY IN BRITAIN IN the Agricultural Returns of Great Britain, published for 1892 by the Board of Agriculture, it is shown that, whilst the total area of the United Kingdom is 77,642,099 acres, the extent to which it is utilized agriculturally and sylviculturally is as follows : — Total Area of Land and Water 77,642,099 acres Percentage of Total Area Arable Land .... Permanent Pasture . Woodlands (and Nurseries) 2577 » 27,533,326 „ 3,005,670 „ 25-5 35-5 3-8 Though the acreage covered with forest is undoubtedly extensive, amounting as it does to 470 square miles, or 3-8 % of the total area of land and water, yet it does not at first glance convey the full extent of the important interests repre- sented by it. On arable land, and in fact on all land utilized agriculturally, the sowing of the seed is followed within one year by the reaping of the harvest; but in woodlands such can never be the case. With the exception of willow-beds cut over annually when once the stools are in vigorous bearing, and coppice-hags of Oak for tanning-bark, or of various woods for other purposes, long periods must necessarily elapse before the timber-crops reach their highest material, technical, and financial value ; hence the advantageous time of maturity may be Studies in Forestry [CHAP. i. •* 4. -4- co O 00 ON M CO O M-.t^ M Uiir^ o M -. ^f M UiCO VO J>. M GO ui O vo vo ro ONVO Ui SN VO ^ ro M ••3- M M rO HI OO Jt^* M M CO M o CO ro ON vo CO 00 UJ ON ro M i | <*£. 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M vo O M M .1^00 Ui rj-cc « rOVO MM M VO 00 M O OO Ui M O r^ O 00 M M ON ro M M GO u. 2 00 ""£ "t ON 1 M MM M W *^ CO M -t^- M vq^ ui 2 • OT •*-> ^r 1 H3 i a H d 3 1 8 f* £ o w ^ *J ^ w >> § | w H Q i o pu H Q 2 i-. ' rt ' ' "C ' o £ v> 5 | .0 . .^1 $ <-* "» i i "* ° TI w ^ is o H o p ' fi ' lj.ll 1 nsions . 0) 1 CS Jl-t OH ft «J tn 1 O, PORTS. 1 8 -H T5 g i Z cC o to a S a, C "rt tn ^ S Jy • ^ *:> rt o 3 •tf • 1 S o 1 • 1 oJ «-• 5? o ,0 • fc G K aK 1-1 1 s 3 £ <5 'S •'c 'c "5 | K at C5 P «.« O llllll "O 13 "o tn s for Tim M-l "c^ ? 0) ^3 IS > O *»" 1 ^ > C/) 1* O D 1 8 *^I 6 c G >> 3 15 c £= = =, = : ^1 R * s s ^5 c/) *3 0 c3 P-.&CQ E2 . « i2 CHAP, i.] Forestry in Britain 7 sylviculture (i. e. when forestry is conducted scientifically), we could supply a great many of these requirements by home-grown timber ; but the argument will be strictly pertinent if it be shown in what respects our woodland owners can, and should, strive to compete with foreign importers. Taking the countries in which identically the same species of trees are grown as may be produced in forests in Britain, there still remain the fol- lowing imports that may be regarded as utilized by us, and not exported again : — Imported from Russia, Sweden, Norway, and Germany during 1892. Timber in the Rough Converted Timber . Loads. 1,400,927 3.362,425 Value. £2,257,401 ^6,950,504 Total 4,763,352 £9,207,905 It may be unhesitatingly maintained that, if due attention were given to the selection of proper species for given soils and situations, and if the principles relating to the most favourable density of plantations, or sowings, or natural reproductions, and to the operations of tending (clearing, thinning, &c.) were properly understood and practised throughout Britain, there would be not the slightest necessity for the insertion (as at present obtains) of any clauses into Government contracts stipulating for the use of foreign wood in preference to home- grown timber. But if woods are allowed to grow up so that a considerable portion of the energy of growth of the indi- vidual trees forming the crop is dissipated in branch develop- ment, in place of being concentrated in the formation of a clean, smooth, full-wooded bole of high technical quality, then no one need be surprised at every person concerned in its utiliza- tion giving a solid preference to foreign timber grown under more rational conditions, and consequently of higher technical value, owing to its comparative freedom from branches and knots. One economic point of great importance may here be noted, 8 Studies in Forestry [CHAP. i. viz. the steady appreciation of forest produce during the past '. And this is bound to become accentuated in the future • for whilst population and the demands for timber, &c., are con- stantly increasing, the woodland area, and consequently the possibility of satisfying these demands, are constantly decreas- ing over the whole surface of the globe. On this point Professor Weber remarks 2, in speaking of the increasing demands for forest produce, and the ever-growing utilization of timber as a raw product for various mechanical and chemical industries, that : — *A proof of the strength of those influences is yielded in the fact, shown by the statistics of prices for the different dimensions of wood, that the mean annual increase in the price of timber during the last fifty years has been from 2 to 2 \ % throughout Germany.' This consideration is one that should most certainly not be lost sight of when we are face to face with the fact 3 that in fifty years' time the forests of America will have become exhausted, even if the rate of timber extraction does not increase at all beyond its present dimensions. The natural consequences of this must not only be that America will, long before the close of that period, not have any surplus timber to export for the supply of our requirements, but also that she must be a competitor with us for any surplus timber that may then be available, in any other part of the world, for export beyond the limits of the countries where it is grown. It is not contended that any considerable portion of the £1,365,075 paid away in 1892 for wood-pulp and rosin could have been retained in exchange for the produce of our own coniferous woods ; for the manufacture of cellulose, and the collection of rosin, are usually conducted in localities where 1 See G. Heyer, Anleitung zur Waldiverthrechnung, 3rd edit. 1883, p. 9. 2 Lehrbuch der Forsteinrichtung, 1891, p. 37. 3 See Article on American Forests in the Journal of the Society of Arts for February, 1893. CHAP, i.] Forestry in Britain 9 wood and labour are comparatively very cheap. But surely what- ever oak-bark is required by tanners might quite easily be grown at home on vacant land along the railway lines in the vicinity of the centres consuming it, so as to undersell foreign imports which incur costs of repeated handling and transport before reaching us. New sources of employment might ftius easily be created and developed for many thousands of people, especially during the early spring, and partly also in the winter months. To confine this statement to the practically useful, there is little doubt that if any encouragement were given to the dis- semination of sound knowledge concerning forestry through- out Great Britain, we should not only be able to obtain better returns — materially, technically, and financially — from the exist- ing woodlands, but should also in other respects be in a much better position for profitably utilizing some of the existing waste lands for the purpose of entering into direct competition later on with these foreign imports, consisting chiefly of coniferous species of timber ; for these trees can attain as fine development as on the continent of Europe, and often finer, especially in Scotland. There is indeed no climatic reason why a very con- siderable portion of the timber now annually imported from Russia, Scandinavia, and Germany, should not in future be supplied of home growth, when once the crops raised have been subjected to rational treatment from the time of their formation onwards until their maturity. This latter condition is essential ; for woods that are crowded at thirty, forty, or fifty years of age, may not have been of sufficient or normal density at ten or fifteen years of age, but may have become crowded in canopy through excessive and uneconomical rami- fication and coronal development. From the Minutes of Evidence (pp. 4, 5, and 42) accom- panying the Report of the Select Committee on the Adminis- tration of the Department of Woods and Forests and Land Revenues of the Crown, submitted to the House of Commons io Studies in Forestry [CHAP. i. on July 26, 1889, it appears that the total area classifiable legally as Crown forests is only 109,139 acres, of which merely 57,304 acres are actually under timber crops, i.e. only 2 % of our three million acres of woodlands are owned by the State, whilst 98 % belong to private landowners. Comparatively slight though this Crown ownership may appear in amount, Yet 57>3°4 acres, or ninety square miles, represent a very considerable monetary capital invested in soil and timber crops. Over two hundred years ago John Evelyn, whose classic work Sylva, or a Discourse of Forest Trees, was read by him before the Royal Society of London in 1664, bemoaned the great decadence and destruction of the woodlands, or as he termed it * the impolitic diminution of our timber j that had been handed down to us from primeval times, and ' which our more prudent ancestors left standing for the ornament and service of their country? But he probably little suspected that the very same causes, which had led to what he considered excessive clearance of the remnants of the aboriginal forests, would ultimately lead to their being partially restored by re-planting, that is to say, the desire to get the best possible monetary returns from the soil. The effect of the gradual depression of agriculture that has been making itself felt during the last fifteen to seventeen years has, of course, first affected the area under the plough. As Major Craigie remarks (Agricultural Returns for 1891, p. io) :— ' Turning to the details of the cultivated area, it is again necessary to note the remarkable changes which have been taking place in the ratio of arable to pasture land in Great Britain. The two great divisions of arable and pasture now claim, for the first time, an almost exactly equal share of the surface. Twenty years ago the arable land was to the grass as 3 is to a. It exceeded by 6,000,000 acres the surface of permanent grass, there being 18,403,000 acres returned as arable to 12,435,000 acres of pasture.' Again, in the Returns for 1892 (pp. 10, u, 21) he has the same sad tale to tell : — CHAP. I.] Forestry in Britain ii ' The arable land, as has been the case in mery year but two since 1872, again shows a reduction. The surface appearing in this category is 157,000 acres less than in 1891. The permanent pasture in 1892 is also less than that returned in 1891 by 76,000 acres. This is a change in an opposite direction to those recorded for a considerable period, but it is wholly explained by a stricter definition of the term Permanent Grass now enforced in certain mountainous counties, where some of the additions made in 1891 to this category were found on closer inquiry not to have been fully justified, the areas in question being again relegated to the class to which they properly belonged, of uncultivated hill grass ' Between 1872 and 1882 about 936,000 acres were apparently with- drawn from arable tillage and reappeared in the opposite category of the cultivated area in the form of permanent pasture. * In the later ten years a similar process has continued. Between 1882 and 1892 the arable area has again diminished, and this time by 1,165,000 acres. . . . The more important alterations between 1891 and 1892, occurring in the entire United Kingdom, may be summarized in the accompanying Table : — Acreage. 1892. 1891. 1892 compared with 1891. Increase. Decrease. Total Cultivated Area . . Acres. 47»977,9°3 Acres. 48*1 79,473 Acres. Acres. 201,570 Total of Permanent Pasture Total of Arable Land . . 27,533,326 20,444,577 27,567,128 20,612,345 . . 33,802 167,768 Owing to the gradual agricultural depression, the poorer classes of arable soil have during the last twenty years gone out of plough cultivation, and have been transformed into pastures; and the immediate consequences of the past year or two must inevitably result in the poorer classes of pasture being ultimately planted up again, thus reverting into some- thing of their original state, as sylviculture will probably hold out better hope of some profitable return from the land than any agricultural or pastoral utilization of the soil \ 1 During September 1893 the Board of Agriculture drew the attention of landowners to the increased facilities for the planting of woods and trees in 12 Studies in Forestry [CHAP. i. Of course, in such an enlightened country as Great Britain, it might reasonably be expected that everything has already been done by Government to provide for the due instruction of those to whom are confided the responsible task of ad- ministering or working these woodlands. That would certainly be the natural inference when one looks abroad at other countries, and at the same time thinks of the many tens of thousands of pounds spent on, and in connexion with, the fine collections of stuffed birds, fishes, reptiles, &c., palatially housed in the magnificent building forming the Natural History Museum at South Kensington, and on the other vast sums of national money originally and annually disbursed for the housing and maintenance of aesthetic and other technical edu- cation. But one would be vastly mistaken in making any such common-sense assumption. When Governments are badgered about any subject in an inconvenient manner, they seem to have a stereotyped way of gravely appointing a committee for the purpose of reporting on this, that, or the other subject ; and after such report has been submitted, there is often practically an end of the business in the meantime, until they are worried again on the subject. This solemn farce has been twice recently enacted with regard to Forestry in Great Britain. During 1885 a committee was appointed for the purpose of considering ' whether by the establishment of a Forest School^ or otherwise, our woodlands could be rendered more remunerative] and on August 3, 1887, they delivered themselves of a report, from which the following excerpts contain the principal conclusions arrived at : — Scotland afforded by the Improvement of Land (Scotland) Act, 1893, which received the Royal assent on August 24, 1893. Hitherto owners of land in Scotland have been able, with the sanction of the Board of Agri- culture, to charge their estates for the planting of woods and trees, only in cases where the planting is for the purpose of providing shelter. By the Act in question, this limitation has been removed, and applications may now be made to the Board for sanction to charge estates under the provisions of the Improvement of Land Act, 1864, with the cost of planting whether for shelter or otherwise. CHAP, i.] Forestry in Britain 13 ' The woodlands belonging to the State are comparatively small, though even, as regards them, the difference between skilled and unskilled management would itself more than repay the cost of a forest school. ' Your Committee are satisfied that, so far as Great Britain and Ireland are concerned, the management of our woodlands might be materially improved. Moreover, the present depressed values render economical and skilful management even more important than if the range of prices were higher, though it is probable that, with the waste of forests elsewhere, a brighter future is in store for home forestry, and that some considerable proportion of the timber now imported, to the value of£ 16,000,000, might, under more skilful management, be raised at home. 1 Nearly every other civilized State possesses one or more forest schools. In this country, on the contrary, no organized system of forestry instruc- tion is in existence excepting in connexion with the Indian service. ' Your Committee recommend the establishment of a forest board. They are also satisfied by the evidence that the establishment of forest schools, or at any rate of a course of instruction and examination in forestry, would be desirable, and they think that the consideration of the best mode of carrying this into effect might be one of the functions entrusted to such a forest board.' As regards the outlay connected with so flimsy a scheme for the improvement of the natural knowledge of forestry in general, it was also stated that — ' The expense of secretarial staff and examiners need not, in the opinion of the Committee, exceed £500 a year, and the cost might be considerably reduced by fees for diplomas? I believe I am correct in stating that, up to date, all that has been done by Government for the advancement of forestry in Britain has been to pay £100 a year to Edinburgh University for a lectureship during the last two years, to provide half of the annual stipend of £500 a year to the Professor of Agri- culture and Forestry at the Durham College of Science, Newcastle, for the chair founded there in 1890, to pay (tem- porarily) £ 150 a year to the free class for foresters, wood-reeves, and gardeners, now being conducted experimentally at the Royal Botanic Gardens, Edinburgh, and to give an equal sum for the elementary course of instruction begun in 1892 at the Glasgow Technical Institute. 14 * Studies in Forestry [CHAP. i. The second Committee was appointed in 1889 ( to inquire into the Administration of the Department of the Woods and Forests and Land Revenues of the Crown] and duly delivered itself of a somewhat lengthy report on July 30, 1890, which terminated as follows : — ' The Committee are of opinion that on the whole the estates are carefully administered, and that the Commissioners discharge their duties faith- fully and efficiently.' This certainly does not tally with the previous finding of the Forestry Committee, that — ' The woodlands belonging to the State are comparatively small, though even, as regards them, the difference between skilful and unskilled manage- ment would itself more than repay the cost of a forest school? From the evidence adduced before the Forestry Committee it is impossible to deny the truth of the latter statement, and therefore we must look for some explanation of this glaring discrepancy. It is to be found in the fact that the inquiry into the administration of the Crown Woods and Forests and Land Revenues was not at all a satisfactory one, so far as the national Woods and Forests were concerned. The chief Crown appointments with regard to the adminis- tration of the actual Woods and Forests are the following : — Salaries. Allowances. Total. One of the two Commissioners of Woods £1200 £1200 Deputy Surveyor, New Forest, &c. . . 680 £369 £1049 „ „ Dean Forest, &c. . . 550 304 854 ( Windsor Parks and ) I Woods I • 5°° 340 840 Surely the manner in which appointments are made to these chief administrative and executive posts must have enormous influence on the administration itself? Had any body of purely business-men been put to the task of satisfying them- selves as to the real nature of the administration of these valuable public estates, they would undoubtedly have asked each of these fortunate public servants what professional educa- tion or qualifications he had obtained previous to receiving CHAP, i.] Forestry in Britain 15 his appointment ; for no private landowner would entrust the management of his estates to any steward or agent without knowing something about the qualifications and capacity of the latter. Yet no inquiries of this description were made by the Committee ; and appointments to the Department of Woods and Forests still continue to remain in the patronage of the First Lord of the Treasury, under Acts 14 and 15 Victoria, chapter 42, section 7, and are in practice more often filled by the appointment of those having influence with politicians, than of men having the best qualifications for the work required of the officers. Whether or not our three million acres of woodlands can, by better general knowledge of the natural laws governing tree-growth, be made to yield \, or f , or i % beyond what they now give as a return on the capital represented by the soi\fl/us the growing stock (and the cost of production of which exceeds 20 \ millions of pounds sterling), is surely a matter of considerable national importance. It is by no means advisable, or even justifiable, to pin one's faith to the Laird o' Dumbiedyke's advice to his son, part of which has been adopted as the motto of the Royal Scottish Arboricultural Society : — l Jock, when ye hae naething else to do, ye may be aye sticking in a tree; it will be growing, Jock, when ye 're sleeping^? This is in itself fundamentally wrong, for the activity of the chlorophyll of the foliage, and consequently the most active assimilation, can take place only under the influence of sun- light ; whilst all our trees have a long period of winter rest — during which even the evergreen conifers merely transpire through their foliage but do not grow. 1 Waverley Novels, A. & C. Black's edit. 1860, vol. xi. p. 294. If the foot-note accompanying the Laird's advice be actual fact, and not also included in the fiction, then it simply shows how ' enterprises of great pith and moment ' are sometimes lightly embarked on in the crassest and most unthinking ignorance. The judicious formation of plantations is no pastime for an idle holiday; unless knowledge, circumspection, and thought are brought to bear on the subject, it bodes an ill omen for the thriving and ultimate development of the young woods. 1 6 Studies in Forestry [CHAP. i. But even during the period of active vegetation the trees may perhaps be growing in a way that is not at all economical ; they may be dissipating their vital energy in an excessive development of branches and crown instead of conserving and utilizing it for the rapid formation of a longer, straighter, and more full-wooded bole yielding the maximum of technically useful, and at the same time financially profitable, timber. Moreover, whilst that may be a very suitable motto for an Arboricultural Society, concerned to a certain extent with the planting of trees for their natural beauty, the full aesthetic effect of which can only be attained by letting them hang as they grow, it would be utterly out of place so far as Forestry is concerned; for woodland trees require to be tended, and educated, and carefully ministered to, during all the several stages of their development, in order to produce the largest re- turns during the various periodical thinnings, combined with the largest and most valuable final yield, materially and financially, when the crop attains its full maturity, and has to be cleared for the reproduction of a younger generation of trees. And can any one in his sound senses think that Forestry, any more than Agriculture, may be conducted profitably and economically merely by following old saws or unthinking rule of thumb ? Does the old Horatian maxim, doctrina sed vim promovet insitam, not equally hold good with regard to sylvi- culture, as well as to other arts and sciences ? Is Forestry so essentially different in its natural laws and fundamental prin- ciples from Agriculture, that whilst University chairs have been founded for the latter at Edinburgh, Belfast, Newcastle, and in a manner also at Oxford1, and properly equipped Schools of Agriculture are located at Edinburgh, Carlisle, Cirencester, and Downton, absolutely next to nothing has yet been done for the dissemination of sound and properly quali- fied instruction in sylviculture ? 1 The Sibthorpian Professorship of Rural Economy at Oxford is at present suspended, but has hitherto been held only by an Agriculturist. CHAP, i.] Forestry in Britain 17 It may be urged against this, that at some Agricultural Schools there are classes of Estate Management and Forestry. This is quite correct, but it does not follow as a matter of course that the teachers there have a really sound know- ledge of the scientific principles and practice of Forestry. Hence a question may very pertinently be asked similar to the Quis custodiet ipsos custodes ? For where shall such men at present get the scientific and practical training in Forestry, without which they are in a certain degree like the blind leading the blind ? In order that this picture may not seem harsh, ungenerous, and overdrawn, permit me to quote from the evidence given before the parliamentary Committee on Forestry on June 15, 1887, by the lecturer on Estate Manage- ment and Forestry at Cirencester (pp, 27-29 of Report dated August 3, 1887). 468. You are Professor of Estate Management and Forestry at Ciren- cester College ? — I am ; I am also a Fellow of the Royal Highland Agri- cultural Society of Scotland, by examination, 470. Have you had practical instruction in forestry yourself? — No, only on estates. 474. Would you give the Committee some idea of the course of instruc- tion in practical forestry ? — There is a course of lectures forming a part of the syllabus of estate management, consisting of about six or seven lectures, as the case may be, and those are illustrated by field- classes in the woods, timber measuring, and valuing standing timber, different processes of planting, grafting, layering, and so on. This is done in the woods. 485. And are they (the students) shown specimens of good forestry and bad forestry, and how to distinguish good from bad ? — We have not that opportunity ; we have no bad forestry. 487. You show them what mistakes to avoid in wood management I presume ? — Yes, but at present it is only on a very small scale in my syllabus ; we have not an opportunity of going fully into the matter. 509. I gather, from what you have stated, that you do not consider the course at Cirencester is sufficient for the education that land agents should receive in forestry ?— No. 515. Is it your belief that instruction in forestry would be a national gain ? — It is so. 521. Are you acquainted with the system of forest instruction pursued in France and Germany ? — No, I am not. C 1 8 Studies in Forestry [CHAP. i. 527. You were taught yourself at Cirencester College, were you not ? — Yes. (Compare 509.) 528. And after then where did you go? — I went into King's College in London for twelve months, and then up to Edinburgh, and took the Highland Agricultural Society's Diploma ; that was about the year 1868. 529. So that you have had yourself as good an education in forestry as t's possible in Great Britain ? — There was no teaching in forestry in my time. 530. But you have had a good insight into forestry ? — / have had an insight into forestry. 541. Do you think it would have been an advantage to yourself if you had had an opportunity of being trained in some regular school, or do you think you have been able to acquire a practical knowledge? — I have been fortunately situated with regard to that. I have had a very long and happy experience with regard to forestry; but others who might follow in my steps might not have the same opportunities of instruction, and others ought to have the opportunity of hearing lectures upon the matter. Nothing that is said above is meant, malo grato^ to depre- ciate the instruction given in Forestry at these Agricultural Colleges. But the evidence tendered by one of the instruc- tors himself is plain and to the point, as it shows most conclusively that the instructors in Forestry have not them- selves had good opportunities of qualifying for their special task, so far as it relates to Forestry conducted on sound scientific and economic principles, i. e. to Sylviculture as contrasted with Arboriculture. Perhaps the only place, with the exception of Cooper's Hill, at which really properly qualified instruction in Forestry is being given at the present moment is the Durham College of Science at Newcastle. But as the lectures on Forestry there only form a minor portion of the course of professorial tuition dealing principally with Agriculture, they can hardly be expected to be adequate to the proper qualification of youths for the management of our existing woodlands in full accordance with the principles and the practice of modern scientific Sylviculture as fully expounded and demonstrated in Germany, the home of Forestry in its highest technical and practical perfection. CHAP, i.] Forestry in Britain 19 The course of lectures which was organized in 1889 at Edin- burgh University is, as at present constituted, merely a make- shift ; and even as a temporary compromise it is only satis- factory on the broad principle that ( half a loaf is better than no bread.' At the present moment reference is made only to a course of technical instruction fitting young men of liberal education for the management of estates containing a considerable area of woodlands. It does not take into consideration the wants of that other very important class of less highly educated men occupying the position of foresters, wood-reeves, bailiffs, overseers, &c., for whose improved edu- cation an experimental system of instruction has recently been inaugurated by Professor Balfour at the Botanic Garden in Edinburgh. For the ultimate success of both of these Schools every lover of Forestry and of woodland growth must hope. The only educational institution properly equipped with duly qualified teachers for granting a sound Sylvicultural edu- cation at the present moment is Cooper's Hill College, near Staines in Surrey, originally built and fitted up as an Indian Engineering College at a cost of £134,000. Without con- sidering the causes which led to the necessity for terminating the original course of study of the probationers for the Indian Forest Service in Germany and France, and without discussing whether the cessation of the continental training has proved itself beneficial or not, it may be said that Cooper's Hill was not primarily selected for any local or other advantages it offered per se. Its selection was mainly due to other reasons; because it was an expensive establishment already in the hands of the India Office,, and needed financial support after the reduction in the number of young officers annually required in the Public Works or Civil Engineering Depart- ment (in consequence of the fall in the rupee), for the education of whom alone the maintenance of the College had become unduly expensive. Previous to the education of the probationers for the Indian Forest Service being c 2 2o Studies in Forestry [CHAP. i. begun there in 1885, an annual deficit had for some years to be met ; but by arranging for the education of these, and charging them the usual College fees of £183 a year, this deficit was transformed into a surplus, — thereby proving that the sum charged is in excess of what it actually costs to feed and educate the lads. Had the large sums of money which are being granted annually as salaries to the teaching body there — which consists of three Professors, three Lec- turers, and one Instructor on the Forest branch of the College Staff, with the additional assistance of one Director of Practical Study on the Continent, who superintends the course of study and the tours of inspection made throughout different parts of Germany in order to see practical work on a large scale — been devoted to the foundation of two chairs, one of Sylviculture and Management of Forests, the other of Pro- tection of Forests and Utilization of Forest Produce, at each of the three Universities, (i) Oxford or Cambridge, (2) Dublin or Belfast, and (3) Edinburgh, or perhaps better still St. Andrews or Aberdeen, from their proximity to extensive forests, Great Britain might now have had a course of sound scientific instruction at central points in England, Ireland, and Scotland, fairly abreast of continental Forestry in so far as our own particular requirements are concerned. The present instruction in Forestry at Cooper's Hill can never be regarded as capable of being converted, without previous translation to some University or Agricultural College, into a national place of education in Sylviculture. Because, in the first place, the lectures on Forestry are not capable of being listened to ex via along with any simultaneous course of instruction in what may be more likely to prove better bread-winning studies (although at a University this might very easily be arranged for) ; whilst, in the second place, the charge of £183 a year, and a three years' course, make such a training absolutely prohibitive for the majority of those who otherwise might profit by a shorter and less expensive course CHAP, i.] Forestry in Britain 21 of instruction ; for, after reckoning all extras, clothing, tra- velling, and various incidental expenses, it must cost a parent or guardian at least £700 to £800 to provide his son or ward with a three years' course at Cooper's Hill. This is, however, not a matter that really concerns British Forestry ; for Cooper's Hill is maintained by the India Office, and if the Government of India choose to maintain an ex- pensive institute for young men who might easily be educated at one or other of the great Universities, it is no direct concern of the British public, and is, at any rate in the meantime, beyond the legitimate sphere of their control. There are three distinct classes for which it has, face to face with the existing decline in the agricultural and pastoral value of many kinds of land, now become really of national importance that some scientific instruction in Forestry should be provided ; these classes are : — I. The owners of woodlands, or of waste lands, or of lands of poor quality now likely to be soon thrown out of arable or pastoral occupation. II. The higher educated class which supplies the land-agents, estate factors, stewards, and the like. III. The class of smaller stewards, bailiffs, foresters, wood- reeves, overseers, &c. There is no need to prove that each and all of these classes really require instruction in Forestry. It has been often admitted, and is apparent throughout both of the Forest Reports previously quoted. Even should a man be born to inherit broad acres of stately woods, it does not follow that he is naturally endowed with an intuitive knowledge of the laws of nature regulating the normal development and the best technical methods of tending woodlands ; whilst estate agents and managers may be satisfied with results, that would perhaps not seem to them the best attainable if they were better acquainted with the principles and practice of scientific Forestry. The necessity for instructing landowners is nowhere 22 Studies in Forestry [CHAP. i. more apparent than in Sir Herbert Maxwell's paper on Woodlands in the Nineteenth Century for July 1891, in which in less than a dozen lines he points out one great blemish in our method of treatment of woodlands, and then at the same time, in tendering advice on the subject, commits himself to the expression of an opinion which distinctly shows that his ideas on Forestry have no true scientific founda- tion and are opposed to the very best and most thorough natural knowledge on the subject 1. He boldly advocates the formation of pure forest in preference to mixed woods. I am, however, perfectly certain that, if once the formation and retention of mixed woods be departed from on any extensive scale, the woodland owners throughout Britain will begin to form an intimate and unpleasant acquaintanceship with many noxious insects, some of which, rejoicing in the euphonious names of Gastropacha, Liparis, Tomicus, Pissodes, Hylesinus, &c., will give ample reason for genuine regret at having transformed mixed woods into pure forests. And there are many other objections that can be named; but this is not the proper time and opportunity for doing so. The necessity for men of the second class receiving a better instruction is also everywhere apparent throughout the Report on Forestry. It may be summed up in the quotation of two answers given to the Committee by Mr. Britton, the manager and valuer of a large timber-firm in Wolverhampton : — 783. Do you find that many land-agents possess a capable knowledge of forestry ? — Very few in all my experience ; / think I could pretty well count them upon my fingers' ends. 829. What is the general result that you have come to ? — The general result I have come to is, that very few land-agents know anything of forestry, or very little. And the same holds good with regard to Scotland, although there are a few really good practical foresters holding charge of important wooded estates. Thus the late Mr. Macgregor 1 See Chapter VI, On Mixed Woods and their Advantages over Pure Forests. CHAP, i.] Forestry in Britain 23 of Dunkeld, the Head Forester of the Athole woods, extending to over 20,000 acres, gave the following evidence : — 877. Do you consider that the land-agents, or the factors, as they are called in Scotland, are fairly well informed as to the management of woods and timber ? — Very few of them, I think. 878. What, in your opinion, are the subjects on which factors and woodmen are deficient ? — They are deficient in the knowledge of what trees ought to be planted on suitable soils, and when thinning out ought to commence ; and, in fact, the general management of the woods altogether. And if the majority of the men concerned with the adminis- tration of woodlands are thus ill-provided with knowledge respecting the formation, the tending, and the management of timber crops, it is certainly open to reasonable doubt if they can possibly be in a position to have the soundest ideas with regard to the utilization of the latter when they have- reached their financial or their economic maturity. It is, of course, by no means improbable that a shrewd, observant, practical forester may often arrive at proper methods of treating certain crops without at the same time having any true scientific knowledge of the natural laws influencing either tree-growth in general, or the various individual species of trees in particular. Mr. Macgregor again spoke with no uncertain voice on this point : — 1047. You have had no instruction (on forestry) ? — No. 1048. Do you think you would have done better if you had had a course of scientific instruction ? — / have not the slightest doubt of it ; I have felt the want of it all along. I had to read up, and there are very few books to read. 1049. That is your own experience, and you are prepared to recommend that men beginning life as foresters should have some definite instructions ? — Certainly. The preparation of text-books on the various branches of Forestry was to have been one of the functions of the Board of Forestry recommended by the Committee in 1887. But practically nothing has been done in this direction. It would not be at all right if at the same time I did not point out that evidence was given before the Committee on Forestry tending to show that planting up in England could 24 Studies in Forestry [CHAP. i. not promise remunerative returns, owing to the fact of the timber marts being glutted with foreign timber, to the general depression in trade which was then making itself felt, and to the use of substitutes in many ways in which timber was formerly employed. But it is important to note that among Messrs. Thompson, Macgregor, and McQuorquodale, the able practical head foresters then in charge of the Strathspey, Athole, and Scone forests, there was a consensus of opinion that properly managed woodland crops are undoubtedly profit- able. On this point the late Mr. Macgregor's evidence may be briefly quoted : — 1 122. Then you think the forest area in Scotland might be largely increased? — Very largely ; it can be very much extended. 1123. With profit ?— With profit. This practical advice becomes of all the greater importance when collated with my previous statement relative to the gradual appreciation which can be proved in the case of timber up till now. Simply as a commercial speculation, timber can and should be grown to a much larger extent than at present. If any one studies the relative and steady appreciation of timber in the past, it requires no subtle arguments to make out a fair case for the judicious sylvicultural utilization of the soil in many parts of our island. I do not venture to make this indictment against the Governments of late as well as of previous years, of being utterly neglectful of really important national interests relative to the already existing three million acres of woodlands, with- out being in a position to offer some practical suggestion for the removal of this blot on our system of technical education. But though I cannot agree with the Committee on Forestry in attempting to remedy the defect for so small a sum as £500 a year (reducible by fees for diplomas), yet it need cost a mere nothing in comparison with the housing and maintenance of our national Natural History Museums at Kensington and elsewhere. Sir Herbert Maxwell, in his paper on Woodlands CHAP, i.] Forestry in Britain 25 already referred to, stated that if the landowners of Britain really wanted instruction to be provided at any educational centre or centres, they could easily arrange for it among them- selves without the necessity of appealing to aid from the State. From one cause or another, though probably not that they are already perfectly satisfied with the existing state of affairs, the landowners have failed to subscribe sufficient for even half the amount necessary for the endowment of one rather poorly-paid Chair of Forestry at Edinburgh. Despite the efforts which have continuously been made in this direction by the Highland and Agricultural and the Arboricultural Societies of Scotland, the Secretary of the former had to report to the Council at its meeting on November 2, 1892 : — ' that he had sent out over 5.500 circulars requesting subscriptions for the endowment of the Chair of Forestry in the University of Edinburgh. He regretted that the result had been disappointing, but that the sum now subscribed from all sources amounted to over ^"2,300.' This apathy on the part of landowners does not, however, justify any laissez faire policy on the part of Government ; on the contrary, it should make the latter all the more anxious to remedy the educational defect for the benefit of the rural working-classes, and of our timber-consuming industries, both of which would be very directly and materially benefited. To commence with the lowest scale of requirements, those affecting the forester or wood-reeve class, the experimental tuition now being given under Professor Balfour's auspices at the Botanic Garden and Arboretum in Edinburgh is a step in the right direction. But whilst it affords the very best oppor- tunities of providing lectures on elementary scientific subjects affecting Forestry, it fails in one essential to practical success ; for the work the men are engaged on, whilst going through the course, is, and must continue to be, either Horticulture or at best Arboriculture, but is certainly not Sylviculture or Forestry. If we were to follow the excellent Bavarian example— and I do not think we could do better — we should establish 26 Studies in Forestry [CHAP. r. Sylvicultural Schools for young lads at Dunkeld in Athole, or Grantown in Strathspey for Scotland, and at Coleford in the Forest of Dean or Lyndhurst in the New Forest for England, where it would be easy to provide a fair practical education for a limited number. Of course in this event there would not be the scientific teachers within easy reach to give short courses of elementary instruction ; but a little extra payment for travel- ling expenses might no doubt circumvent the difficulty, and overcome that drawback. For the first and second classes, those of landowners, land- agents and factors, nothing short of the establishment of Chairs of Forestry at Universities seems in any way to meet the neces- sities of the case ; for, as I have already asserted, it is only at such educational centres, and not at any special colleges, that an opportunity can be given to students of hearing lectures on this subject concurrently with other and more usual studies fitting them for the ordinary vocations in life, And perhaps, taking all things into consideration, the most suitable Univer- sities for the dissemination of scientific instruction would be Oxford for England, Edinburgh, and either St. Andrews or Aberdeen for Scotland, and Dublin or Belfast for Ireland. Even if Government were willing to establish Chairs of Forestry at any or all of these places, it by no means follows that the Universities applied to would accept the proposals, and permit the incorporation of such Chairs into the existing teaching body, unless they were granted a perfectly free hand with respect to the selection and appointment of the Professors. If any such Chairs be formed from national funds, then the salaries attached to them should be sufficient to obtain the services of really highly-trained men, and should not be less than £700 a year at Oxford, Edinburgh, and Dublin, or £600 at St. Andrews, Aberdeen, or Belfast ; and the lectures should be free to all who wish to hear them — whether matriculated students of the year or not. The reason of this will be apparent when it is stated that the attendance given to the CHAP, i.] Forestry in Britain 27 lectures at Edinburgh was 7 in 1889-90, 6 in 1890-91, 40 in 1891-92, 10 in the winter of 1892-93, and 5 in the summer of 1893, during the first, second, and fourth of which sessions the fee for the course was £3 3^., whilst it was free (to matricu- lated students only) for the merely incomplete course given during the winter session of 1891-92. If formed, none of the appointments should be filled except by men thoroughly trained in Forest science, and fully quali- fied to give lectures over the whole range of Forestry ; that is to say, in — 1. Sylviculture, treating of the formation, tending, and repro- duction of woodlands. 2. Protection of Woodlands ', showing how to safeguard them from inimical inorganic agencies (winds, frost, &c.) or organic enemies (fungoid diseases, insects, game, &c.). 3. Management of Woodland Estates, and Valuation of Timber Crops, for the framing of Working Plans, and in order to determine the most profitable methods and times of utilizing the timber crops. 4. Utilization of Woodland Produce, showing how it can most economically be prepared for, and brought to, market. The matter is either one of true national importance, or it is not. If not, then the owners of woodlands may well be left to go on as indifferently and unintelligently as they have hitherto been doing ; for they can help themselves out of the difficulty whenever they choose to combine and open their purse-strings to no very great extent. But if it really be of national importance, then now, when large areas of land are likely to be thrown out of arable and pastural occupation, is the proper time for the Government to initiate a sound system of instruction in Forestry. Even if my suggestions were carried out to their very fullest extent ; if Chairs of Forestry could be founded at Oxford, Edinburgh, Dublin (each at £700 a year), and at St. Andrews, Aberdeen and Belfast (each at £600 a year), and if small schools of Practical Sylviculture for youths 28 Studies in Forestry [CHAP. i. were arranged for at Dunkeld, Grantown, Coleford, and Lynd- hurst (at about £150 a year each), the total annual expenditure involved would only amount to £4,500. This is surely a very slight insurance to pay for the probable better management of woodlands already amounting in actual minimum cost to over twenty-and-a-half millions of pounds sterling, and most likely to be very considerably added to in the immediate future. It amounts, in fact, to less than three farthings per acre per annum for the land already actually under timber. CHAPTER II THE BRITISH SYLVA, AND THE GROWTH OF WOODLAND CROPS IN GENERAL AT the time of the Roman invasion of Britain a very con- siderable portion of our island was still covered with forest, as the gradually advancing requirements of increasing popula- tion had not yet necessitated any very extensive clearance of the primeval woodlands in order to permit of the expansion of tillage and pasturage. The species of forest trees of which the woods consisted comprised Oak, Beech, Hornbeam, Scots Pine, Birch, Ash, Willow, Alder, Scots Elm, Yew, Aspen, Mountain Ash, and Hawthorn. The uplands of central and southern England, and more especially those tracts having limy or chalky soils, bore dense woods of Beech (which, however, was not indi- genous to Scotland, where it was not introduced until the beginning of the eighteenth century), whilst a stately growth of Oak covered the richer alluvial stretches having deeper soil. The sandy hills of southern England and all the mountainous tracts extending from Yorkshire to the northern portion of the island were probably mainly covered with Scots Pine (the only species of the Abietineae indigenous to Britain), Birch, and Mountain Ash, whilst Oak, Ash, Scots Elm, Aspen, Willow, Alder, and Yew were for by far the most part restricted to the dells, valleys, and lower-lying localities, where the soil was 30 Studies in Forestry [CHAP. n. generally deeper and more productive, and the climate was less rigorous. During the Roman occupation of Britain (A. D. 44-410) many species of trees were introduced from the continent of Europe, including Sweet Chestnut, English Elm, Poplar, and Lime, together with a good many other ornamental and fruiting trees which failed more or less to establish themselves, and never actually attained anything like true forest growth. Even these four species named have only naturalized them- selves to a certain degree ; for they cannot in our climate, and more particularly in that of the northern portion of the island, with its shorter and considerably cooler summer as compared with the south of England, be relied on to produce seed of normal germinative quality. To compensate for this, however, they are richly endowed with the power of throwing out stoles or suckers from the roots, and these are capable of being transplanted like seedlings. Of the various other species that are now entitled to rank among our forest trees, Sycamore or Scots Plane, white and crack Willows, and white and grey Poplars were introduced before the end of the fifteenth century ; Spruce, and Cluster Pine during the sixteenth century; Silver Fir, Maple, Horse Chestnut, and Larch during the seventeenth century (although the Larch was not introduced into Scotland till 1727); Weymouth, Mari- time, Cembran, and Pitch Pines in the eighteenth century ; and Austrian, Yellow, and Jeffrey Pines, Nordmann's and Douglas Firs, Menzies Spruce, &c., during the present century. The Forest Trees of any country may be considered, from a sylvicultural point of view, as belonging to one or other of two classes ; for they must be either Principal or Ruling Species, forming, or capable of forming, pure forests without any assis- tance from other kinds, or else Subordinate or Dependent Species, which are practically found thriving best in admixture with one or more of the ruling species. The terms principal and subordinate are of course here used CHAP, ii.] The British Sylva 31 in a purely sylvicultural, and not in any financial, sense ; for, as a matter of fact, the most valuable species of timber are usually to be found among the latter class. To the former belong, among the conifers, Scots Pine, Spruce, Silver Fir, and occa- sionally Larch, and among the broad-leaved trees, Beech, Oak, Birch, and Alder principally ; whilst the latter include all the other indigenous and exotic trees now of woodland growth in Britain, of which the principal are the Douglas Fir, the Menzies Spruce, the Black Pines (Austrian and Corsican), and the Wey- mouth Pines among conifers, and the Ash, Maple, Sycamore, Elm, Hornbeam, Aspen, and Willow among broad-leaved species. For the sake of brevity the following details will be con- fined to the above-named trees only. Whilst in growth trees extract supplies of nutriment partly from the atmosphere (in the shape of carbonic acid, the carbon being assimilated, and the oxygen being set free) and partly from the soil occupied by their root-systems (mineral nutriment). If the trees were to be allowed to die off and then rot, in place of being utilized as timber whilst still in healthy growth, the supplies of mineral nutrients extracted from the soil would be restored to it, by the formation of humus or mould, on the ligneous tissue becoming decomposed under the action of sunlight, moisture, and a moderate degree of warmth. But, with the removal of the timber crops, the natural balance is disturbed ; and, unless protection be afforded to the agencies active in causing the chemical changes that result in the de- composition of its mineral constituents, the soil runs a risk of becoming gradually deteriorated and finally exhausted. In agriculture, a similar danger is obviated by manuring the land, the manure not only helping to replace the nutrients previously withdrawn, but also stimulating to increased nitrification and decomposition of the soil. In sylviculture, however, such measures would be neither practicable nor remunerative ; and the only recompense that can practically be given consists in the fall of dead foliage, twigs, &c. Fortunately, however, in 32 Studies in Forestry [CHAP. n. these debris is stored up a large portion of the mineral sub- stances extracted from the soil. But the work of decomposing and dissolving the mineral nutrients is indirectly aided by the leafy canopy of the woodlands. This both prevents insolation of the soil, and also safeguards the retention of a certain amount of soil-moisture requisite for rendering the mineral nutrients soluble ; because it is only in the form of soluble salts that food can be- imbibed by the rootlets. By ramifying throughout the soil, the root-systems help to cleave and fissure the subsoil previous to other changes taking place; whilst shrubs, grasses, and mosses, thriving under the shade of the trees, also die off, decompose, and are transformed into forest mould, which, from its strongly hygroscopic nature, absorbs and retains the atmospheric moisture and precipitations, and assists in regulating the flow of water within the soil. When the leaf-canopy overhead is much interrupted or broken, the soil is apt to be overrun with a rank growth of noxious grasses and weeds, which consume the nutrients un- profitably ; whilst at the same time it is exposed to the inimical influences of sun and wind, whose action is apt to reduce the quantity of moisture in the soil below that which is most favourable for tree-growth. For the retention of the soil-moisture, and the protection of the soil generally, those species of trees are the most favourable crops, which have a dense crown of foliage and maintain them- selves in close canopy until their maturity — qualities with which the different kinds of trees are very unequally endowed. Among broad-leaved genera the Beech ranks highest in this respect, its canopy being close and its foliage dense, whilst the dead leaves are rich in potash and form mould of excellent quality and strongly hygroscopic power. The leaves of Oak do not form good humus, as a considerable amount of tannic acid is evolved during decomposition. Hornbeam foliage yields good mould, but the crop of leaves is lighter in every way than in the case of the Beech ; Lime shades the soil CHAP, ii.] The British Sylva 33 well and is thickly foliaged, though, as the leaves are thin in texture, the amount of humus formed is only slight ; the Chest- nut has a thick crown of foliage yielding good mould. None of these last three genera occur, however, to any great extent form- ing pure woods in Britain. Oak, Elm, Ash, Maple, Sycamore, and the other valuable broad-leaved species are, owing to the com- parative lightness of their crowns of foliage, not naturally well endowed with capacity for protecting the productive power of the soil, when they form crops by themselves, without the assistance of other trees with denser crowns, — although they may be found doing well on soils of so moist a character that insolation and evaporation are rather beneficial than prejudicial in diminish- ing the amount of soil-moisture. Among conifers the species best endowed with soil-improving and soil-protecting qualities are in particular Spruce, Menzies, Douglas, and Silver Firs, and in a less degree the Weymouth and the Austrian and Corsican Pines, the fine growth of mosses beneath which also acts like humus in sponge-like absorption and retention of moisture. Scots Pine and Larch are, owing to the sparseness of their foliage, least endowed in this respect, although during the earlier stages of their development a good layer of moss is usually to be found covering the soil, and protecting it from the inimical and exhausting effects of sun and wind. When once the canopy begins, however, to get broken, this beneficial covering of moss disappears ; and then the soil, with its new growth of rank grasses, whortleberry, or heather, rapidly begins to deteriorate, unless underplanting is taken in hand. Where marshy land is, planted up with Alders, Birch, Willows, and Poplars, the action of sun and wind is often beneficial, just because it tends to reduce the quantity of moisture, which is apt to be excessive on such low-lying situations. One of the leading principles in the Management of Forests is that in woods of normal composition, having crops of all ages and classes properly represented from zero up to maturity on areas of equal productive capacity, the annual fall of mature timber 34 Studies in Forestry [CHAP. n. shall, under ordinary circumstances, be equal to the annual pro- duction of the total area during one year; and this is repre- sented, as the total growth throughout x years, by the mature timber standing on the fall about to be harvested. To cut down more than this, is to consume a portion of the capital represented by the growing stock ; whilst to utilize less, is simply not to treat the woodlands in an economic manner. In order, however, that such normal average increment may take place annually, it is necessary that the woods must be of normal density, that is to say, neither too crowded on the one hand, nor too sparsely stocked on the other, although of course the suitable and proper degree of density that may be termed normal varies with each species of crop. Crowding is disadvantageous. If the individual trees forming the crop have not a sufficiency of growing-space, then they cannot possibly obtain the supplies of light, air, and warmth requisite for their most favourable development, and therefore soon fall into a sickly condition of growth, which predisposes them to dangers from wind, snow, insects, and fungoid diseases. The constant struggle, too, which is being waged for supremacy among the individual trees in woods becomes thereby unduly prolonged ; and in this is dissi- pated the energy which, with judicious tending and thinning, can be advantageously utilized for the better and more vigorous formation and development of the individual poles or trees of more robust growth, from among which the trees finally form- ing the mature crop must ultimately be selected. But if the number of individuals per acre falls below the normal average density for any particular species of tree and any given class of soil and situation, or, in other words, if the growing-space allotted to each individual be in excess of what is requisite to maintain the pole or tree in vigorous growth, then its vital energy becomes dissipated in branch-formation, instead of being con- served so as to be concentrated and utilized in the formation of a long, straight, full-wooded bole or stem, free from knots, and consequently of higher technical utility and commercial value. CHAP, ii.] The British Sylva 35 And, at the same time, from the leaf-canopy formed by the crowns being much more apt to be interrupted here and there, or sometimes quite broken in its continuity, the surface of the soil must be exposed to the action of sun and wind and to the consequent danger of rank growth of weeds, subsequent deterioration, and perhaps final exhaustion. This normal density, which should be maintained unbroken or uninterrupted in order that the productive capacity of the soil may be fully utilized, and yet at the same time protected against deterioration, consists of a full or close leaf-canopy. The different species of forest trees are very unequally endowed with capacity to retain close canopy when once they have en- tered on the later stages of development, for they make different demands with regard to individual growing-space, and then the density of the foliage forming the crown also varies with each individual species. To estimate these differences it is only necessary to compare the crown of a Beech or a Silver Fir with that of a Birch or a Larch, although in these cases extremes are purposely chosen in the two classes of broad-leaved trees and conifers. This physical fact, that all trees of forest growth are not alike endowed with the capacity of shading the soil and protecting it against the exhausting influences of sun, wind, and rank growth, is a matter of very great moment from the sylvicultural point of view. Although all our forest trees may be grown in pure woods, if worked with a low rotation, owing to timber crops being naturally dense during the thicket period (that is, till the crop begins to clear itself naturally of dead branches), and during the pole-forest stage of growth (which means till the leading stems have attained a girth of about two feet measured at breast height), yet after that, when once they have entered into the tree-forest or high-forest stage of develop- ment, their natural individual differences with regard to demands for light, i.e. growing-space, and with respect to density of foliage in the interior of the leafy crown, begin to make themselves unmistakably apparent. Thus whilst thickly foliaged kinds of D 2 36 Studies in Forestry [CHAP. n. trees, like Beech, Silver Fir, and Spruce, can be grown in pure forests until they attain their full technical and mercantile maturity, without the productive capacity of the soil being endangered, it would be contrary to one of the leading prin- ciples of sylviculture — viz. the conservation of the productive capacity of the soil — to cultivate pure high forests of light- demanding genera like Oak, Ash, Maple, Pine, or Larch, except under special circumstances where the productive capa- city of the soil is not endangered by insufficient cover, as, for example, on some classes of marshy land where the evaporation caused by insolation and by the free play of winds is directly beneficial, or on low-lying tracts with fresh soil, whose depth and porosity might perhaps be injuriously affected by any accu- mulation of humus. It is solely with regard to the soil-protecting capabilities of the different forest trees that the classification above given of Ruling and Dependent Species is based; for it may be briefly stated that the productive capacity of woodland soil is only safeguarded to the necessary extent when the timber crop consists either of thickly-foliaged species growing in close canopy, and providing the soil with a good layer of leaf-mould, or else of conifers having evergreen foliage, under which a covering of mosses performs the functions of the humus or mould elsewhere. The species of trees naturally fitted to be grown in pure forests under the first of these conditions are pre-eminently Beech, Spruce, Menzies, Douglas and Silver Firs, and in a less degree Hornbeam, Lime, and Chestnut; whilst those falling under the second condition comprise the several varieties of the Pine genus, so long as they are not worked with too long a period of rotation, i. e. so long as their fall is not delayed too long after the time when they sink so far below the normal density of canopy that the growth of mosses gives place to weeds and berries, and the soil begins to deteriorate through insufficient protection against insolation and exhausting winds. Unfortunately the broad-leaved trees best qualified by nature for the formation of pure forests are CHAP, ii.] The British Sylva 37 not in Britain of sufficient technical and commercial value to lead to their cultivation on any large scale ; but among them the Beech and, on moister varieties of soil, the Hornbeam are of great sylvicultural importance as the ruling species or matrix, either in the shape of underwood or of tree-forest, along with which the more valuable classes of timber trees, Oak, Ash, Maple, Sycamore, Birch, &c., may be most profitably grown on localities where the soil would be liable to deterioration if the woods consisted of these thinly-foliaged and light-demanding species only. For the formation of woods of normal density or full leaf- canopy the number of individuals per acre varies, as has already been stated, according to the species of tree ; but wherever reliable data have been collected, it appears that, on soils of the best quality for the requirements of each genus of tree, at the age of 120 years there are 37 % more Beech, 24^ % more Silver Fir, and 60 % more Spruce than individual stems of Scots Pine per acre. It also appears that at all ages there is on soils of the best quality invariably a very much smaller number of individual trees of any particular species than on the poorer classes of soil. The difference may often be enormous, for at eighty years of age Scots Pine woods on the best class of Pine soil consist of only one-third of the number of trees that are generally found on the poorest class of soil. So far as these different results are concerned, with one and the same species of tree, they are explainable through the fact that the general development and the natural process of selection of the fittest— the struggle for light and air, for domina- tion, and for individual existence— is more energetic and decisive on good soils than on those of inferior quality. The differences exhibited by the various species of trees, however, is dependent on their different sylvicultural characteristics with regard to the natural development of their crowns, and their special requirements as to growing-space. Through- out the Spessart forest it has been found that the following Studies in Forestry [CHAP. II. average density of crop is necessary for the formation of close canopy : — Age of Forest, years. Beech. Oak. Soil of best Quality. Soil of best Quality. 60 120 5*7 2IO 1.234 326 Although at first glance this almost looks as if it might be argued that the Oak is more capable of bearing shade than the Beech, which would be contrary to experience, it actually proves nothing more than that the Oak takes considerably longer than the Beech to develop in that locality, and that the Beech finds lateral expansion of its crown a sine qua non of existence at an earlier period of age than the Oak. Whilst the number of individual poles or trees forming the crop is larger on poor than on good soils, yet the full normal density of leaf-canopy is maintained longer on the better classes of soil. But the actual extent to which the ground is overshadowed varies also with the species of tree ; for experiments and measurements have shown that in a Spruce forest, of normal density for Spruce, the soil is overshadowed to more than twice the extent that obtains in a Scots Pine forest, of normal density for Pine. If what has been stated above be correct — viz. that the pro- ductive capacity of the soil can be best protected when close canopy is maintained throughout woodland crops — then it must naturally follow that the greatest production of timber per acre must take place in woods having a leaf-canopy of normal density. And practical experience shows that such is the case. In general, other things being equal as to the productive capacity of the soil, the increment per individual stem is greater in trees revelling in the full enjoyment of light, air, and warmth, than CHAP, ii.] The British Sylva 39 in those whose crowns are limited to a more or less restricted growing-space; because they have larger root-systems, can draw greater supplies of nutriment from the soil, and enjoy better opportunities for carrying out assimilation and for utilizing their nourishment in the formation of ligneous tissue. On soils similar as to quality the total production per acre in close- canopied forest is not only greater than in the more open forest, but the technical quality of the timber produced is also much higher owing to the better dimensions attainable by the bole or stem, and to freedom from knots formed where the branches emerge from the trunk of the tree. The larger the growing-space allowed to each individual tree, the greater is the tendency to branching growth taking place at the expense of the bole; hence, for the production of long straight stems, it is necessary to maintain as close canopy as is consistent with the general health and vigour of the crop until it has passed through the pole-forest stages, during which its growth in height is most active, although this again varies according to species of tree and other factors. When crops attain their chief growth in height after being maintained in canopy of normal density, experience has shown that the stems rapidly increase in girth when the canopy is interrupted, artificially, for the purpose of permitting the individual trees to obtain larger supplies of light, air, and warmth. This sylvicultural operation, although pur- posely diminishing the number of individual trees per acre, often leads to a greater increment and a more valuable yield than if the crop had been allowed to remain growing in normal canopy, — but this is a subject that will receive full attention subsequently (see Chapter X). As, in woods growing in close canopy, the crown is circumscribed, and can for the most part obtain only from above the light and warmth necessary for the work of assimilation, the poles compete with each other for a larger measure of exposure to these invigorating influences, so that the growth in height becomes stimulated. And as, owing to the crowns being limited to the upper portion of 4Q Studies in Forestry [CHAP. 11. the stem, a larger proportion of the assimilated food is utilized in the upper part of the tree than in the lower, the result is that the boles are more full-wooded, i.e. they approach more to the cylindrical in form, than is the case with poles growing in crops below the normal density in leaf-canopy. Until the chief growth in height has been completed, therefore, the mainten- ance of close canopy affects not only the actual length of the bole or clean stem and its shape, but also the proportion of timber obtainable, as compared with branchwood ; and these are matters of great technical and financial importance. When seedling growth or young plantations, after having passed through the thicket stage of growth, develop into pole- forest, and finally into tree-forest or high-timber, the crop consists of various classes of growth named, according to the position they may occupy in the struggle for increased growing space : (i) predominating, (2) dominant, (3) dominated, and (4) sup- pressed, although of course there are no hard and fast lines existent between these different classes. Until far on in the life-history of the crop, the predominating class comprises within it all the individuals that are likely to form any portion of the mature fall of timber ; hence, in all clearings and thin- nings undertaken with a view to the tending of woodlands — a subject that will be considered later on (see Chap. IX) — the removal of the suppressed and, to a greater or less extent (according to the species), the dominated classes, is advisable. Such cultural measures are not only for the purpose of assist- ing nature in the work of eliminating the individuals no longer required in the maintenance of a leaf-canopy of normal density, and of helping the more vigorous stems towards their more rapid development, but also for removing all poles and young trees of enfeebled energy and perhaps sickly growth, which might offer dangerous attractions to noxious insects. Compared with the total number forming the crop, the per- centage of individual stems necessary for the retention of a leaf- canopy of normal density varies essentially according to (i) the CHAP, ii.] The British Sylva 41 species of tree, (2) the nature of the soil and the situation, and (3) the previous treatment that has been accorded to the crop. In consequence of the competition for possession of the soil, which takes place when different species of trees have been intermixed either naturally or artificially, the law of nature regarding the survival of the fittest has brought it to pass that, wherever they have long had free scope to make their special characteristics and influence felt, certain species of trees usually predominate numerically over large tracts of country. As has already been mentioned, the primeval woods of Britain consisted mainly of Oak on the better soil, Beech on limy and upland tracts, and Scots Pine on the higher hills and on slopes having only inferior qualities of soil. If we look at the continent of Europe, we find the Scots Pine the chief tree over the bulk of the sandy stretches comprised within the North German plain, and the Spruce asserting itself throughout Scandinavia and north-western Russia and on the humid mountainous tracts of central Europe, pre-eminently on the Harz Mountains ; a covering of Beech clothes the lower hills of central and north-western Germany, forming the Deister, Soiling, and Thuringian forests ; the Silver Fir occupies similar situations in south-western Germany and France, in the Black Forest, and the Jura mountains ; whilst Austria has large tracts wooded chiefly with Black Pine and Larch, and Russia can show its well-defined areas on which Pines, Firs, Hornbeam, Birch, Alder, and Aspen are the dominant species. Speaking generally, the ruling species of trees throughout the forests of central Europe, as they now exist, may be said to be Scots Pine, Spruce, Silver Fir, and Beech in the first degree, followed by other Pines, Larch, Oak, Alder, and Birch. These are the species which form the bulk of the individuals in woodland crops ; whilst Ash, Elm, Maple, Sycamore, Poplars, Willows, and exotics like Weymouth Pine and Douglas Fir, are only to be found in smaller numbers, or in situations specially suited for their growth. It is, however, rarely that any of these species 43 Studies in Forestry [CHAP. n. are now to be found forming pure forests in countries where attention has been paid to the most recent developments of scientific sylviculture ; for the tendency is now rather towards the formation and maintenance of mixed woods as combining important sylvicultural and financial advantages. But, if entirely left to themselves, certain species of forest-trees will ultimately suppress and eliminate most other kinds over tracts of soil better suited to the former than to the latter. Evelyn was to a certain extent aware of this more than two hundred years ago, when he remarked, in one of his letters published in Aubrey's Surrey, that : — 'Where goodly Oak grew, and were cut down by my grandfather almost a hundred years since, is now altogether Beech ; and where my brother has extirpated the Beech there rises Birch.' What might just be expected happens. The shade-bearing and densely-shading species — Beech, Spruce, Silver Fir, and in a less degree Hornbeam and Black Pines — assert themselves over large tracts; whilst other kinds of trees of woodland growth are ousted, and occur merely as subordinate clumps, or groups, or patches, or as individuals scattered here and there over areas and situations unsuited for the predominating species, either on account of the nature of the soil or situation, or for some reason connected therewith (frost, want of moisture, shallowness of soil, &c.). There can, of course, never be rigid lines marking off the domain of the various species ; for there must always, in consequence of the various factors connected with the physical conditions of soil and situation, be belts of land where the advantage lies sometimes with one species and sometimes with the other. At the present time on the continent one has many opportunities of seeing how, in consequence of bad management and of servitudes, under wru'ch the peasants were entitled to rob the woodlands of their soil-protecting layer of dead foliage, the domain of the Oak and the Beech is being encroached on by the Pine and the Spruce, which are both more easily satisfied as to soil and situation ; whilst these CHAP, ii.] The British Sylva 43 latter again have often to contend with the still more easily satisfied Birch and Willow for the possession of their own areas. It might be argued against what is here stated, that the Scots Pine asserts itself to the exclusion of shade-bearing species on the vast plains south of the Baltic ; but this is solely due to the fact that, for the poor sandy soil there, the Pine has proved itself better suited and more accommodating than any other species of tree, and is in fact merely another example of the survival of the fittest. Even on that sandy plain, near the fertile lands along the riverine tracts, there is still to be found a stately growth of Oaks, Ash, Elm, Maples, &c., able to hold their own against any attempts at encroachment made by less noble species of woodland trees ; whilst the Alder and Willow coppices of those districts are famed. From a study of the growth of trees in their natural habitats, and of their development in varying situations into which they may have been brought by artificial means, we are enabled to classify and arrange them according to their sylvicultural characteristics ; and a thorough knowledge of these is necessary before we can hope to attain anything like the highest and most successful results with regard to the formation, tending, and reproduction or regeneration of woodland crops. To give only one instance of error made in regard to a valuable species of tree, owing to want of scientific knowledge regarding its habit and conditions of growth, take the case of the Larch, which was introduced into England in 1629, into the Lowlands of Scotland in 1725, and into the Highlands in 1727. Of this tree, 27,000,000 plants are said to have been planted out in Scot- land between 1738 and 1820; but it certainly has not fulfilled all the anticipations that were then made as to its future value. The Larch is essentially a tree of the mountains, where it ascends higher than even the Spruce. It is found on the Bavarian Alps at from 3,000 to 6,000 ft. above sea-level in excellent development and often forming pure forests; lower down it is naturally associated along with Spruce and Beech in 44 Studies in Forestry [CHAP. n. the zones more congenial to these genera. The climate in which it thrives best is the Alpine climate, that is to say, one in which a long cold winter is succeeded by an exceedingly short spring, and followed by an equable, warm summer, which again, after a very short autumn, gives place to the long period of winter rest and defoliation. Removed far from its true Alpine home, and subjected to climatic conditions essentially differing therefrom, can it be wondered at that its development has been, on the whole, disappointing ? In place of having the good straight bole, which is characteristic of its growth where indigenous, it tends to curved, sabre-like form ; the stem and branches are prone to favour the development of hanging lichens ( Usnea barbata, &c.) ; the foliage is damaged by cater- pillars of the mining-moth (Coleophora laricelld] and of another Tortrix (Grapholitha pinicoland] ; whilst the boles are specially liable, at from about ten to twenty-five years of age, and more especially after bad attacks of these insects, to become infected with the serious cankerous, fungoid disease due to Peziza Willkommii. This has often necessitated a clearance at the age of forty to fifty years, or long before the crops would, under more favourable circumstances, have been anything like tech- nically or financially mature. The investigations of Professor R. Hartig of Munich have shown that the fungus which occa- sions this disease is indigenous to the Alpine home of the Larch, and sometimes occasions canker on stems there ; but it has followed the tree to central and Northern Germany, and to England and Scotland, where, owing to climatic condi- tions and to its less vigorous growth, the stems are more liable to become infected, whilst the ravages committed are at the same time more serious. His own words are as follows : — ' The enormous distribution which the Larch fungus, Peziza Willkommii has obtained on the German plains, is almost solely explained by the rich development of fully matured fruits and spores in the damp, and more especially in the stagnating, atmosphere of close-canopied forests CHAP, ii.] The British Sylva 45 in low-lying localities ; whilst with the free play of aerial currents in Alpine tracts the fruits almost always dry up before they ripen V The crookedness of the stem may be due either to want of depth of soil interfering with the normal development of the strong tap-root, or else to the growth of the tree being stimu- lated beyond normal and healthy limits, owing to the much longer period of activity necessitated by our climate, in which spring and autumn are gradual and prolonged stages between the periods of foliation and defoliation. 1 Lehrbuch der Baumkrankheiten, 2nd edit., 1889, p. 45. CHAPTER III THE CHIEF SYLVICULTURAL CHARACTERISTICS OF OUR WOODLAND TREES THE differences in sylvicultural characteristics exhibited by the various species of our forest trees may be conveniently classified with reference to the following matters : — I. Climatic requirements. II. Requirements as to soil and situation. III. Capacity for bearing shade. IV. Normal shape of the stem and crown. V. Increment or rate of growth in height, girth, and cubic contents. VI. Reproductive capacity. VII. Attainment of economic maturity and normal duration of healthy growth. When John Evelyn, as a Fellow of the Royal Society, read his Sylva, on October 15, 1662, we were quite abreast of continental knowledge relative to woodcraft; but since then we have lagged behind nearly every other country, whilst Germany has acquired by far the largest and richest stores of natural knowledge with respect to the science of Forestry. Yet, even in Germany, it is only within the last ten or twelve years that Professor Karl Gayer's observations and classifi- cations have found general acceptance as the fundamental principles upon which the modern practice of Sylviculture — that branch of Forestry which treats of the formation, tending, and reproduction of woodland crops — has a firm, logical, and CHAP. III.] Characteristics of Trees 47 scientific basis. The first edition of his great work on Sylvi- culture was issued in 1880, and the final expressions of his matured conclusions, in the third edition of 1889, are the source from which most of the following data have been drawn *. I. Differences of Forest Trees as to Climatic Requirements. The natural causes influencing the geographical distribution of the forest trees of Europe are partly climatic, and partly de- pendent on the physical conditions of soil and situation. The energetic growth and development of any particular species can only take place in localities that have such period of vegetation, and such intensity of summer warmth, as to enable the processes of assimilation and of the formation of ligneous tissue to proceed satisfactorily. For the least exacting species in this respect a three-monthly period of vital activity and a mean summer temperature of 54° to 57° Fahr. are the requisite minima2; whilst on the other hand the minima of the cold during the winter months also fixes their limits, so that large tracts of arctic Russia and Scandinavia are destitute of forest growth. The polar or northern limits of some of the more common forest trees are as follows : — Species. Western Europe (Scandinavia & Germany). Eastern Europe (Russia). Scots Pine . . Spruce . . . Oak (Q. pedunc.) Beech. . . . Silver Fir . . 68-70° 67-71° 60° 49-52° 6{i2° And, in a similar manner, the reduction of the temperature 1 Waldbau, 3rd edit., 1889, pp. 18-49. 2 Weber, Die Aufgaben der Forstwirthschaft, in Lorey's Handbuch der Forst-wissenschaft, 1886, vol. i. p. 13. 48 Studies in Forestry [CHAP. in. in atmosphere and soil, with increasing height above sea-level, also causes a more or less irregular and inconstant distribution of species according to vertical zones in the mountains of central Europe, although in this respect the variations due to soil, situation and aspect are so great that it would perhaps be misleading to attempt any classification. It must, however, be remarked concerning the Scots Pine and the Spruce that their limits towards the north, and towards Alpine heights, are not so much due to the actual intensity of cold during winter, as to the fact that transpiration by the leaves is stimulated on bright sunny days in winter at a time when the frost-bound soil can yield no supplies of moisture to replace what is evaporated through the leaves J ; hence the natural consequence is that the foliage grows yellow, the tree turns sickly, and death ensues. These results can most frequently be observed after long, dry, hard winters with frequent sunny days. The southern limits of the forest trees of northern Europe are mainly determined by the quantity and the regularity of the rainfall during summer. As the results of careful experiments conducted in Austria, von Honel2 found that, computed by the unit of weight of their dry foliage, among broad-leaved trees, Ash and Birch require the largest supplies of water for transpiration, then Beech and Hornbeam, then Elms, and finally Maples and Oaks. Among conifers, the order was Spruce, Scots Pine, Silver Fir, Black Pine. He also found that, taken as a whole class, the broad-leaved species consumed on the average about ten times as much water as the conifers, and that, owing to the light foliage of the Pine, this species required very much less soil-moisture than Spruce or Silver Fir. But although the actual total of average annual rainfall may be considerably greater than what is required for transpiration through the foliage during the active period of . 1 R. Hartig, Lehrbuch der Battmkrankheiten, 2nd edit., 1889, pp. 104, 261. 2 Compare, however, the more recent data set forth in Chapter IV. CHAP, in.] Characteristics of Trees 49 vegetation (and, even for Beech, a summer rainfall of twelve inches would suffice according to Ramann 1), yet when rain does not fall on the average once every 6 to 8 days throughout the summer months, the woodland crops are, in the dry climate of central Europe, exposed to more or less danger of being killed off by being unable to obtain from the soil the constant supplies of moisture requisite for the maintenance of healthy and vigorous growth by means of normal transpiration ; or in other words, they are liable to suffer from drought and to die off. So far as the climate of Great Britain is concerned, it is, both as regards temperature and atmospheric precipitations, suited to all the species of woodland trees that occur in central Europe ; but the Mountain Ash, the Wych Elm, the Scots Pine and the Birch are more characteristic of, and grow better in, Scotland than in England, where again the Beech, the pedunculate Oak, the English Elm, and the Silver Fir thrive better than in the northern half of the main island. Pine, Spruce, Larch, Silver Fir, sessile Oak, and Sycamore, are naturally the inhabitants of upland tracts and mountain ranges, whilst Ash, Alder, pedunculate Oak, Aspen, Elm, and Willow belong rather to low-lying localities ; Beech, Hornbeam, Maple, and Birch seem capable of thriving equally well on plains or on hilly country. But, on the whole, the nature of the climate, soil, and situation mainly determines the quality of any given species of tree in any particular locality. Very little is as yet known regarding the absolute amount of atmospheric warmth necessary for the most favourable development of the different kinds of woodland trees. But experience has shown that Elm and pedunculate Oak require most warmth ; that Black Pines, Silver Fir, Beech, Weymouth Pine, sessile Oak and Scots Pine can thrive with less than Birch, Maple, Sycamore, Ash, Alder, and Spruce ; whilst Larch does with least. So far as their development is apt to be prejudicially 1 Forstliche Bodenkunde und Standortslehre, 1893, p. 311. E 50 Studies in Forestry [CHAP. HI. influenced by frost, Ash and Beech are most liable to injury ; Oak; Silver Fir, Maple, Sycamore, Spruce, Douglas Fir, and Alder are somewhat liable; whilst Hornbeam, Elm, Birch, Larch, Aspen, and Pines are the most hardy species. It is not, however, the winter's cold that is injurious to these species, but the late frosts in spring, when the flush of young leaves and shoots is still tender, and the early frosts in autumn before the summer shoots have had time to harden sufficiently so as to resist the effects of the cold. The relative humidity of the atmosphere is also a climatic factor exerting very considerable influence on the vigour and general development of the various kinds of woodland crops. Experience has shown that, so far as any difference can be made in a generally damp climate like that of our islands, the species thriving best in localities with great relative atmospheric humidity are Willow, Poplar, Alder, Maple, Sycamore, and Ash ; Silver Fir, Scots Pine, Beech, Aspen, Birch, and Douglas Fir do best with a moderately damp climate ; whilst Oak, Elm, Black Pines, and Larch naturally prefer a rather dry atmosphere. It may be of interest to note that the Scots Pine, which thrives so well in our moist insular climate, does not thrive in Denmark, and is essentially a tree of dry localities in Germany ; whilst Spruce, which thrives best in humid localities throughout central Europe, does not appear to grow anything like so well in Britain. II. Requirements as to Soil and Situation. The aspect or exposure of any particular locality tends to exert an influence in the same direction as vertical elevation, though on a much smaller scale ; for, as the mean annual tem- perature of slopes facing from S.E. to S.W. is higher than that of hill-sides with N.E. to N.W. aspect, this naturally affects the thriving of woodland crops. Near their limits of vertical distribution, however, all trees ascend the mountains to CHAP, in.] Characteristics of Trees 51 a greater height on the southern than on the northern sides, in consequence of their requirements as to warmth. The root-systems of the various species of forest trees vary greatly with regard to shape and to the depth to which they reach ; but even shallow-rooting kinds derive advantage when the soil over which they grow is deep, owing to the greater supplies of nutriment within easy reach of their roots. Some are characterized either by a strong tap-root, or else by a deep heart-shaped root with stout ramifications, as in the Oak, Elm, Pine, Silver Fir, Maple, Sycamore, Ash, and Larch ; others have no pronounced tap-root, but develop strong side-roots penetrating into the soil for a moderate depth, as in Beech, Hornbeam, Aspen, and Birch ; others again, like the Alder, throw out strong side-roots, whence strands are sent down into the soil ; whilst some are unmistakably shallow-rooting, as in the case of the Spruce. Spruce, Aspen, and Birch require least depth of soil, and Oak and Larch greatest. Of the other trees, Scots Pine, Silver Fir, and Douglas Fir need deeper soil than Austrian and Weymouth Pines ; whilst Beech, Hornbeam, and Alder, although by no means shallow-rooted, can do with a less depth than Elm, Maple, Sycamore, and Ash. In referring to von Honel's experiments regarding the tran- spiratory power of the various species of trees per unit of weight of foliage, it will be remarked (Chapter IV) that his researches give us no reliable data for estimating the absolute quantities of soil-moisture necessary for woodland crops so as to supply their normal requirements throughout the annual period of active vegetation. Practical experience, however, shows that Alder, Ash, Willow, Poplars, Maple, Sycamore, and Elm, then Larch, Weymouth Pine and Spruce, prefer soils with a considerable degree of moisture ; whilst pedunculate Oak, Hornbeam, Birch, and Aspen, and in a less degree Silver and Douglas Firs, also make greater demands than Beech and sessile Oak, or Scots, Corsican, and Austrian Pines, which are the three species that can best accommodate themselves to dry soils (the former on those of a sandy, the latter on those of a limy nature). E 2 52 Studies in Forestry [CHAP. m. On the whole, the conifers are more moderate in their demands on soil-moisture than the broad-leaved genera of trees. But the limits within which the different trees can thrive vary greatly according to the species ; or in other words, the various kinds of woodland trees exhibit great differences as to their accommodative power with regard to the degree of moisture contained in the soil. Although trees derive the greater part of their nutriment from the carbonic acid which they absorb from the atmosphere, still they are also .dependent on the soil for supplies of mineral nutrients; and these can only be taken up when held in solution by the soil-moisture. Whether the soil be loose or binding is also a matter of very considerable importance to the thriving of the various woodland trees. As a rule the broad-leaved species do better than conifers on the stiffer classes of land, although soils of merely average tenacity are on the whole most suitable for all kind of trees, owing to their better endowment as regards physical properties. The chief constituents of soils are clay, lime, and sand ; and as clay yields the most valued nutrients for plants, the qualities of soils are often determinable to some extent by the quantity of clay found in them. The effects of the mineral constituency of soils are, however, very greatly modified by the physical properties inherent in them, and these become prejudiced whenever any one of those three most important constituents occurs in undue excess. Clay soils are tenacious and interfere with the movement of soil- moisture ; sands are too porous, and limes are too easily heated ; hence on the average, the mixed classes of loamy soils are in general most fertile. The absolute demands of the various species of trees on the mineral strength or fertility of soils is not yet fully known, although they can to a certain extent be estimated from the weight and analysis of the ash left after reducing the different kinds of timber by combustion. On this point, however, sylvicultural experience shows that Elm, Maple, Sycamore, and Ash, make the greatest demands ; and that Oak, Beech, CHAP, in.] Characteristics of Trees 53 Silver Fir, and Willow are more exacting than Larch, Hornbeam, Alder, Spruce, and Aspen ; whilst Poplars, Pines, and Birch can thrive fairly well on indifferent classes of soil. Here again it may be noted that, on the whole, the broad- leaved species of trees are more exacting than the conifers. As a broad generalization it may be asserted that the power of any species to accommodate itself to soils and situations not naturally suited to its normal requirements varies in the in- verse ratio of the demands it makes as to mineral strength ; for it is greatest in Scots Pine and Birch, and least in Elms, Maple, Sycamore, and Ash. It would be wrong to state broadly that a clayey, limy, sandy, or loamy soil is, or is not, suited for any given species of tree; because so very much depends on other considerations, and particularly on the amount of humus present in it, owing to the very favourable influence which this exerts on the physical properties of the soil. Gustav Heyer even went so far as to maintain l that almost any soil was capable of producing any given kind of timber, provided that it contained the requisite amount of moisture. Ney 2 thus summarizes the best practical opinions that have yet been expressed on this subject : — 4 As regards the chemical composition of the soil, even slightly sour marshy soils are unfavourable to all species of trees except Alder, Birch, and Spruce ; whilst sour soils, liable to dry up at certain seasons, are unsuited to all except Birch, Spruce, Scots and Weymouth Pines. Only these last-named species thrive on pure peat, and not even the Spruce when it is dry. Ash, Maple, Sycamore, and Elm require a moderate quantity of lime in the soil, and Beech, Hornbeam, Oak, as also Larch and Austrian Pine, thrive best on soils that have at least some lime in their composition. The hardwoods — Oak, Ash, Maple, Sycamore, Elm, Chestnut, Beech, and Hornbeam— also appear to de- mand the presence of a considerable quantity of potash ; whilst, on the other hand, Spruce, Silver Fir, and especially Scots Pine and Birch, thrive on soils rich neither in lime nor potash.' 1 Forstliche Bodenkunde und Klimatologie, 1856, p. 488. 2 Lehre vom Waldbau, 1885, p. 64. 54 Studies in Forestry [CHAP. in. The influence of the sum total of the factors dependent on soil and situation find their expression in the amount of timber produced per acre, and in the quality of the timber, since this latter must determine its adaptability for technical purposes. Practically speaking, the best and the most convenient general standard for estimating the quality of timber is to be found in the specific weight, as, for one and the same kind of wood, the heavier specimen is the more durable1, owing to the thick deposits of ligneous substance in the cells. This does not, however, apply to any comparison of different species ; for the light wood of conifers is more durable than heavy Beech timber. High specific gravity, length, straightness, and full- woodedness of bole, with freedom from knots and branches, are the best indications that soil and situation are eminently suitable to the woodland crops covering them. III. Capacity for bearing Shade. All trees require a certain amount of light in order to carry out the work of assimilation of the carbonic acid which forms so important a part of their nutriment. Hence the want of a due intensity of light exerts an injurious influence ; otherwise there is no reason why the density of the foliage in the interior of the crowns of trees should not be as great as it is near the circumference. It is true that excess of light may tend to paralyse the action of chlorophyll ; but, so far as the forest trees of Britain are concerned, they are exposed to no danger from this cause in our climate; they will thrive all the more vigorously the more light they receive the benefit of. But, with regard to the measure of light necessary for the performance of the assimi- lative functions by the foliage — or, in other words, to the capacity for bearing shade — marked differences occur among the various species of trees ; and though affected by soil 1 Gayer, Die Forstbenutzung, 7th edit., 1888, p. 66. CHAP, in.] Characteristics of Trees 55 and situation, these differences are, especially in woodlands, sufficiently distinct to admit of general classification into shade-bearing trees, light-demanding trees, and trees that occupy an intermediate position. The different species of our forest trees may accordingly be classified as : — Light-demanding trees: Larch ; Birch. Scots Pine ; Aspen, Poplar, Willow. Oak, Ash, Elm ; Douglas Fir. Trees less impatient of shade : Alder, Maple, Sycamore ; Weymouth, Corsican, and Austrian Pines, and Menzies Spruce. Shade-bearing trees : Spruce ; Hornbeam. Beech ; Silver and Nordmann's Firs. The capacity of the various species for bearing shade under any given circumstances, or in other words, their demands for light, may be gauged by the general density of the foliage of the crown and the capacity of overshadowed twigs to retain life. But, so far as regards the absolute quantity of light requisite for the performance of the assimilative functions of any species, we know as little as about the necessary amount of warmth. For general sylvicultural purposes, Larch, Birch, Scots Pine, Oak, Ash, Aspen, and Willow, may be considered the principal light-demanding species of trees, and Silver Fir, Beech, Spruce and Hornbeam the chief shade-bearers ; whilst the attitude of the other woodland trees in this very important matter is mainly dependent on the conditions of the soil as to depth, moisture, and general quality. The length of the annual period of vegetation also makes itself 'felt to a certain degree ; for in the far north, or at high eleva- tions, where this is shorter than in lower latitudes or levels, the demands for light become greater than obtain under the oppo- site conditions. The same may also be said of cool northern 56 Studies in Forestry [CHAP. in. exposures and misty regions, as compared with warmer southern aspects and localities where the crowns can revel in the undis- turbed possession of genial sunlight and warmth. The relative powers of the various species of trees to bear shade under any given conditions as to soil and situation are of great, and indeed vital, importance in practical sylviculture. For on these are mainly dependent the measures that may seem prudent with regard to the selection of species of trees for woodland crops, the extent to which admixture of species may be advisable, the best method of treatment and tending to be accorded to the woods, the most advantageous time for harvesting the mature crops and reproducing them, &c. In fact, without a due consideration of their individual characteristics in this respect, it is impossible to accord rational scientific and practical treatment to woodland crops. IV. Normal Shape and Development of the Stem and Crown. The essential characteristic of a tree as compared with a shrub is its habit of developing a bole or stem before be- ginning to ramify and form a crown of foliage-bearing branches. Some kinds of forest trees have a greater tendency to ramifi- cation than others, as, for instance, the broad-leaved trees generally in comparison with conifers ; but the individual tendencies of each kind with regard to the length and straight- ness of the bole are often to a very considerable extent de- pendent on (i) the growing-space allotted to if, (2) the age of the crop) (3) the nature and quality of the soil and situation. Douglas Fir, Spruces, Silver Firs, Larch, and Weymouth Pine, then Scots Pine, sessile Oak, and Alder have naturally a strong tendency towards the formation of a good bole or stem ; whilst Hornbeam, pedun- culate Oak, and Willow are prone to branching growth. The other species of woodland trees occupy an intermediate position between these two classes. But the natural tendency CHAP, in.] Characteristics of Trees 57 to assume their normal shape has only free scope when the individual trees are growing in full exposure to light and air. Those in which the leading-shoot develops more vigorously than the side-shoots then assume a conical form; whilst others, whose side-shoots compete on anything like equal terms with the axial shoot, remain short and stunted, and have low wide- spreading crowns. The true characteristics of any tree are best observable when it is grown in the open; but, when the growing- space allotted to each tree is limited, these natural tendencies are checked, and a struggle upwards for individual exposure to light and air ensues, which transforms the whole vital energy into activity of growth upwards. This impulse is greatest in light- demanding trees, and, within reasonable limits, may be said to vary inversely to the growing-space allowed. Even when grown in the open, Spruces, Douglas Fir, and Silver Firs, Larch, and Weymouth Pine retain a distinctly noticeable central axis, which is yet traceable, though less clearly, in Scots, Corsican, and Austrian Pines, Alder, Beech, and sessile Oak, and to a still less degree also in Ash, Maple, Sycamore, and Elm ; whilst on the other hand the pedunculate Oak and Hornbeam have a marked tendency to ramification and to the formation of a diffuse crown at no great height above the ground. In woodland crops of normal density the leafy crowns of Larch, Pines, Oak, Birch and Aspen reach only a little way down the stem; those of Spruce, Douglas Fir, Beech and Hornbeam descend for about one-third of the bole ; whilst in Silver Fir they often extend almost half-way down. The effect of the concentration of the crown of leafy foliage towards the summits of the stems ensures the conservation of the assimilated nourishment for the forma- tion of long, straight, full-wooded stems of the highest possible technical and financial value, in place of this being dissipated over a large branch-system and a stunted stem. That such timber must be more full-wooded, i.e. that the relative proportion between the upper girth or diameter and the lower should show less difference, is easily intelligible, owing to the larger 58 Studies in Forestry [CHAP. nr. supplies of assimilated nourishment offered under the above circumstances to the upper portion of the bole than to the under part. In the earlier stages of development the age of the crop is of little practical importance. All species of trees, when grown in woods of normal density, assume a conical or spindle-shaped crown till they outgrow the pole stage and become tree-forest ; but, having passed through the most active period of their growth in height, they then begin to exhibit their natural tendencies more distinctly. Thus Larch, Spruces, Douglas Fir and Silver Firs continue to develop more vigorously upwards than side- wards • Pines, Elm, Beech, Maple, Sycamore, Birch, sessile Oak, Ash, and Alder begin to assume an oval crown ; whilst English Oak and Hornbeam get rounded off with a broad, obovate crown. As they approach the limits of age of healthy vigorous growth, all trees, except Larch, Spruce, and Douglas Fir, assume a blunted or rounded off growth near the summit, due to the growth in height declining sooner than the lateral expansion. So far as soil and situation affect the shape and habit of growth, fresh, fertile loams stimulate to full-foliaged coronal development and large girth of bole, though somewhat at the expense of its length. Deep, fresh, light sandy soils favour length of stem ; but, as the crowns are thinner, and the branch- development is sparser, the girth consequently remains less. Shallow and rocky soils affect the stem-development very prejudicially, and cause branching growth and excessive root- systems spreading far around in search of moisture and nutri- ment. Great elevation above sea-level, and raw, cold exposures, militate against the formation of good stems. In Scotland, at 2,500 ft., the Scots Pine is more like a shrub than a tree. The conclusion deducible from the above facts is that wood- land crops formed of shade-bearing genera able to thrive with a small growing-space, i.e. Beech and Hornbeam, but more particularly Spruces, Silver and Douglas Firs, are able to main- tain close canopy better and longer than woods formed chiefly CHAP, in.] Characteristics of Trees 59 of Larch, Pines, Ash, Maple, and Sycamore. And when, as in the case of Oak, Birch, and Chestnut, a tendency to branch- ing growth is combined with strong demands for light, the leaf-canopy is apt to be interrupted early and to an injurious extent; and the natural impulse in this respect is all the greater, the less favourable the soil and situation may be for the particular species of tree in question. V. Increment, or Bate of Growth in Height, Girth, and Cubic Contents. Growth in height varies, both in energy and duration, accord- ing to the species and the age of the tree, the soil and situation, and the methods of formation and treatment of the woods. It is most active in Douglas, Spruce, and Silver Firs, Larch, Scots and Wey mouth Pines, which can attain an average height of from 110-140 ft. — the Douglas Fir grows to over 300 ft. in height, and 1 8 ft. in girth, in its home in North America; Oak, Ash, Beech, Maple, Sycamore, and less frequently Elm, Poplar, and Birch reach a height of 100-130 ft. ; whilst Black Pines, Horn- beam, Alder, and Willow are seldom over 80-100 ft. high when mature. These data are only for crops of normal density. But the maximum heights usually attained by the various species of trees are reached in different periods of time. This fact, combined with their varying demands as to light, is of immense importance from the practical sylvicultural point of view ; as these are two of the main points to be considered (when once the protection of the productive capacity of the soil has been duly safeguarded) with regard to the formation and tending of mixed woods. Birch and Larch, above all others, then Poplar, Alder, Ash, Maple, Sycamore, Elm, Willow, Weymouth and Scots Pines, and Douglas Fir, are the trees that shoot up most rapidly during their youthful period of growth ; whilst Oak, Beech, Hornbeam, and Black Pines may be classed as of moderately 6o Studies in Forestry [CHAP. III. rapid growth, and Spruces and Silver Firs as relatively slow in initial development. These results show that, in a general way, the rate of growth in height during the earlier stages of tree-life coincides with the demands made by the species on light and growing-space. Some species, like Douglas Fir, Larch, and on good soils Pines and Birch, maintain the advantage gained ; but others, like Ash, Maple, Sycamore, and Aspen, are caught up in growth and overtopped by Spruce, Silver Fir, Beech, and Oak, whose vigour increases on their attaining the pole-forest stage of development. The duration of active growth in height in any given species depends to a great extent on the quality of the soil and situation; but, coeteris paribus, it is maintained longer by Larch and Firs than by Pines among conifers, and longer by the sessile Oak, Elm, and Beech than other species among broad-leaved trees. The average heights (in feet, and ap- proximate only) of some of our more common forest trees, on soils of merely average quality for each different kind of tree, are about the following in well-managed woods of normal density : — Age of Crop. Years. Beech. Silver Fir. Spruce. Scots Pine. 2O 10! IO II 17! g 34 1 35 1 33 57 39 55 80 67 72 75! 65 TOO 76 M 88 75 I2O 83 85 95! 80 It is at once perceptible from these figures how careful the tending will require to be in mixed crops between the fortieth to sixtieth years, and even earlier on soils of inferior quality ; for wherever light-demanding species are overtaken by shade- bearing species they must be killed off in the struggle for supremacy, unless favoured to a greater or less extent during the special operations of tending. CHAP, in.] Characteristics of Trees 61 Growth in girth is in all species of forest trees practically proportional to the growth in height, as they are each the expression of the vigour of the individual tree. In most of the light-demanding species of trees this begins early, often attains its maximum vigour between the twentieth to thirtieth year, maintains itself till about the fiftieth to sixtieth year, and then gradually declines. It begins later with Oaks and shade-bearing species, but is often vigorously maintained till the seventieth to ninetieth year before beginning to sink gradually. In crowded woods the development in girth is more prejudiced than the energy of growth in height ; but whenever the growing- space allowed is more than sufficient for the normal require- ments of any given species, growth in girth takes place at the expense of growth in length. When trees still in vigorous growth are heavily thinned after being accustomed to but a limited growing-space, they rapidly thicken in the bole in consequence of the greater exposure to light and air, and of the increase in foliage and assimilative power due thereto. The largest girths are attainable by Douglas and Silver Firs, Spruces, Wey- mouth and Scots Pines among conifers, and by Oak, Elm, Beech, and Black Poplar among broad-leaved species of trees. Growth in cubic contents, or total increment, is the final expression of the resultants of growth in height and growth in girth, and is a convenient measure of the general energy of growth. Owing to the reduction in the number of individual stems per acre, consequent on increased demands for growing- space, increment culminates earlier in light-demanding than in shade-bearing species. So far as whole crops are concerned, Gayer classifies their energy in total increment as follows : — Spruce and Silver Fir woods. Larch, Weymouth and Scots Pine woods. Beech woods. Oak, Ash, and Hornbeam woods. Birch woods. But he specially characterizes the energy of the Firs as nearly 62 Studies in Forestry [CHAP. in. twice as great, and that of the Pines as about half as great again as that of Beech, which is the most energetic of the broad-leaved species. It will be seen, from what has previously been said, that the productive energy of the individual tree may be widely different from the productive energy per acre of a pure forest of that species ; and it will therefore readily be intelligible how advantageous — alike from the material, the financial, and the sylvicultural points of view — the judicious formation of mixed crops may be as compared with pure forests, more especially if formed of the light-demanding species. VI. Differences with regard to Reproductive Capacity. Trees may reproduce themselves either by means of seed, or else by means of shoots from the stool, or through suckers thrown up from the roots. Reproduction from seed is the normal process of regeneration of all species that are indi- genous, or that have thoroughly naturalized themselves in our climate ; whilst the formation of stoles or root-suckers is princi- pally confined to English Elm, and to exotic Poplars and Willows, which cannot be relied on to form seed of anything like average germinable capacity ; of indigenous trees, Aspen and Willow are the only species endowed with this quality to any great extent. The formation of shoots from the stool is not so much a regenerative measure as rather an effort at recuperation and replacement of the stem or bole when the ascending axis has been removed. It is solely due to the vital activity of the root-system, which, until late in life, remains active after the stem and crown have been removed, and which endeavours, by a new flush of shoots and foliage from the adventitious or dormant buds at the neck of the stump, to obtain the means of assimilating the food that it continues to absorb from the soil. This same tendency is seen in pollarding as well as in coppicing, but in another form and a more 'limited degree. CHAP, in.] * Characteristics of Trees 63 The formation of seed depends on the supplies of starchy and nitrogenous reserves stored up in the tree. These vary according to its age, the soil and situation the amount of exposure to light, and the warmth of the summer period of vegetation. In good seed-years Beech, Oak, Spruce, Pine, Birch, Hornbeam, Elm, Aspen, Alder, and Willow produce larger quantities of seed than Ash, Maple, Sycamore, Silver Fir, and Larch. But, classifying them as to the total quantities of seed produced during long periods, it may be said that Birch, Aspen, and Willow are most prolific ; next to them come the Pines, Spruces and Douglas Firs, Elm, Hornbeam, and Alder ; behind these again rank the Oak, Maple, Sycamore, Silver Fir, Larch, and Ash • whilst last of all in this respect comes the Beech. From this it cannot fail to be noted that in general the species with small seeds are more prolific than those with large and heavy fruits. As these light, and very often winged, seeds are more easily wafted and borne far away by winds, it must be admitted that species of trees like Birch, Aspen, Pine, and Spruce have better natural reproductive power than Oak, Beech, Silver Fir, and the like. It is worthy of note, too, that the former are species which make less demands on soil fertility than the latter, and are at the same time endowed with greater accommodative powers as to soil and situation ; for these are matters almost sure to be closely connected with the power of accumulating reserves of starchy and nitrogenous substances utilizable for the formation of flowering-buds. The different kinds of seeds vary, however, greatly in their germinative power. This is lowest in Birch, Alder, Elm, and Larch. It amounts to about 50 % in Ash, Hornbeam, Maple, Sycamore, Weymouth Pine and Silver Fir ; whilst it is some- what greater in Oak, Beech, Spruce, and Scots, Corsican, and Austrian Pines. The seed of most species of trees germinates in the spring after it has been shed ; but that of Birch, Elm, Aspen, and Willow sprouts during the spring in which it falls, and that of 64 Studies in Forestry ' [CHAP. in. Ash and Hornbeam germinates only in the second spring after its fall, if the seed has been stored before being sown. Seed-production is greatest when the main growth in height is completed, and the natural tendency to coronal development makes itself apparent in increased demand for light and grow- ing-space, i.e. when the vital energy is at its maximum. Warmth of situation, fertility of soil, and increase in growing-space, all stimulate to production of seed, owing to the larger supplies of nutrients, and the better assimilative opportunities then available for each individual tree. The formation of stool-shoots taking place in coppice-growth is essentially an expression of recuperative power. It is inherent in the broad-leaved species to a very much greater degree than in conifers, among which, indeed, with the exception of the Larch and the three-needled species of Pines, it is almost practically non-existent. This power of replacing the stem and crown is greatest during the younger stages of growth, but is always to a great degree dependent on the quality of the soil and the degree of exposure to light. Oak and Horn- beam retain their recuperative power in this respect longest (to about 85 years of age), whilst stools of Beech and Birch, after being coppiced several times, lose their reproductive vigour. The formation of stoles or suckers appears to be the only means of utilizing their surplus reserves of starchy materials with which exotic species of trees (English Elm, Lime, Chestnut, and most Poplars and Willows) are endowed, seeing that from climatic causes they are unable to utilize them in the same way as indigenous trees, or the other exotic species that are less exacting with regard to warmth, that is to say, in the normal production of seed of average germinative capacity. Stool-shoots are more often produced than suckers by Oak, Hornbeam, Beech, Elm, Alder, Ash, Maple, Sycamore, Willow, and Birch; whilst stoles are more frequent than stool-shoots from Aspen, non-indigenous Willows and Poplars, CHAP, in.] Characteristics of Trees 65 and White Alder. But Willow, Chestnut and Elm at the same time throw out a very fair proportion of stoles, which may be cut away and transplanted like seedling growth. VII. Differences as to Attainment of Maturity and normal Duration of healthy Growth. The ages to which the various kinds of forest trees may be grown in a healthy condition without showing visible signs of senile decay exhibit great differences. Thus we find Oak and Scots Elm attaining 500 years and more, English Elm, Silver Fir and Beech 300-400 years, Ash, Maple, Sycamore, Spruce, Larch, Scots Pine and Hornbeam about 200 years, whilst Aspen, Birch, Alder and Willow seldom attain over 100 years. Indeed, many historical trees are known to be very much older than any of these limits ; but even the above ages are far in excess of any rotations that could possibly be maintained in woodlands worked on sound economic sylvi- cultural and financial principles. For the attainment of healthy old age the essential con- ditions are (i) that the opportunities of growth must be such as to permit of the normal development of all the organs of nourishment, and (2) that the soil and situation must continue to supply all demands as to warmth, moisture, &c., made by the individual species. But very frequently the economic re- quirements of sylviculture are incompatible with the demands as to growing-space, &c., that are involved in the above. And the capacity of different genera for regaining normal vigour, after being first grown for a long time in close canopy and later on allowed a larger measure of light and air, varies con- siderably ; it is greatest in Oak, Lime, Willow, Elm and Silver Fir, and least in Alder, Aspen, Maple, Sycamore, Beech, Horn- beam, and Spruce. From the practical sylvicultural point of view, the following may be regarded as the ordinary average limits of age which F 66 Studies in Forestry [CHAP. III. it is advisable to allot to timber crops grown in high forest ; but so much depends in each case on the concrete conditions as to climate, soil, and situation, that the figures must be regarded as rough generalizations only : — Kind of Tree. On soils of good quality. On soils of inferior quality. I. Silver and Douglas Firs 2 Spruce . . Years. IOO-I2O 8o—IOO Years. 60-80 60- vo 3. Scots Pine and Larch 8O-IOO 50-70 i. Oak 120-150 ; 180—200 GO- I 2O 2. Beech. . . oo 1 20 8o—IOO 3. Hornbeam, Elm. Maple, Sycamore, Ash . . 4. Willow, Birch, Aspen . 60-80 50-60 40-50 40-50 From these approximate data it will be at once apparent that when mixed crops are formed of several genera, these may attain their technical and financial maturity at different ages ; hence it is the duty of the forester to utilize those which mature soonest, by extracting them at the time of their highest economic value. This is done not only with a view to obtain- ing the maximum monetary returns, but also for the purpose of protecting, to the greatest possible extent, the productive capacity of the soil. For the realization of both of these objects abundant opportunities are given during the process of tending the timber-crops throughout all stages of their development, to the consideration of which matter one of the succeeding chapters will be devoted (see Chap. IX). CHAPTER IV THE NUTRITION AND FOOD-SUPPLIES OF WOODLAND CROPS 'Concerning the growth of plants a large amount of informa- tion has been amassed, but we are far from possessing even an approach to a knowledge of the laws which regulate this important subject.'— RoscOE's Elementary Chemistry^ 1888, page 413. ALL plant life is governed by what is known in agricultural chemistry as the Law of the Minimum. According to this law the essential factor occurring in minima regulates the total extent of production ; whilst any given species of plant attains its finest growth and development in localities where all the essential factors are most favourably combined. These essential factors are partly of a physical, and partly of a chemical nature. To the former belong the action of warmth and of light, and to the latter carbonic acid, oxygen, and the water requisite for dissolving and holding in solution the mineral nutrients that can only be absorbed by the plant in the shape of soluble salts. Temperature makes itself felt, throughout both the soil and the atmosphere, in calling into activity the process of vegetation in spring, and in continuing it during the summer and the autumn. Most of the trees indigenous throughout central and northern Europe begin their period of active vegetation in spring when the temperature rises to 6° or 8° C, although with exotics from the warmer south a higher temperature is requisite in order to stimulate them to activity. F 2 68 Studies in Forestry [CHAP. iv. This is a subject which has hitherto been little studied, as the following extract from Willkomm 1 may show : — 'Despite a mean winter temperature of + 17-5° R. (71-4° Fahr.) the Beech in Madeira has a period of rest for 149 days, during which it remains leafless ! This strange phenomenon is to be noted also in the Elm, Silver Poplar, Willow, and other broad-leaved trees distributed through the whole of Europe, as well as in the Apple, the Pear, and other fruit-trees over all the most southern parts of Europe. They also lose their foliage in autumn, and only flush anew in spring, although during the whole of winter the temperature does not sink below + 5 to 7° R. (43^° to 47!° Fahr.). And whilst in central and northern Europe the buds of the above-named trees open early in spring after warm winters, this is not the case in the south. This phenomenon must be due to some law of nature which remains as yet unknown.' And in another place2 he remarks with regard to woodland trees that — ' The absolute minima during the period of vegetation are of far greater importance, with regard to the thriving of trees, than the minima of winter, and the average temperatures of the months and seasons.' Indeed he goes so far as to say that 3 — ' It may be stated as a general law that the polar or northern limit of any particular species of tree is determined by a certain definite isotherm of July, whilst its equatorial or southern limit is determined by a certain definite isotherm of January.' Seebohm's observations in Siberia agree with the first part of that statement. For he observed that 4 — * The limit of forest growth does not coincide with the isotherms of mean annual temperature, nor with the mean temperature for January nearly so closely as it does with the mean temperature for July.' When once active vegetation has been stimulated by increasing 1 Die Forstliche Flora von Deutschland und Oesterreich, 2nd edit., 1887, P- 452- 3 Op. «/., p. 364. 3 Op. cit., p. 39. 4 Presidential Address to Geographical Section of the British Association, 1893, in Royal Scot. Geog. Society's Magazine, October, 1893, p. 511. CHAP, iv.] The Food of Trees 69 warmth in spring, the energy of the vital process is enhanced as the temperature rises, until it may reach a point at which the plant is unable to carry out the vital operations in a normal manner. In Britain, hot southern slopes with light sandy soil may often prove too warm for woodland trees like Spruce and Silver Fir, whilst cold land with a northern exposure may not supply the amount of warmth requisite for the best develop- ment of Oak. In forestry, no measures can be taken to regulate the atmospheric temperature. But by maintaining a close canopy of foliage, or by the underplanting of standards, much can be done to regulate the soil-temperature, and to retard the commencement of active vegetation. This may even be delayed for about a fortnight or more, and may thus be made to com- mence only at a time when, the atmospheric temperature and the intensity of the light being greater, the process of assimila- tion may be more thorough as well as more energetic. Light, which is closely allied to heat, is essential in order that, with the aid of the chlorophyll contained in the leaves, the decomposition of water and of carbonic acid may take place in the elaboration of substances to be used for structural purposes; whilst at the same time various other processes, such as transpiration, the deposition of matter on the cell-walls, and, in fact, the whole nutrition, are all likewise more or less dependent on the action of light. The intensity of light necessary for the different species of trees, before they can carry out the process of assimilation, varies considerably, as may be seen from the different densities of their foliage; whilst the amount and intensity of light required by one and the same species of tree also varies according to the other factors of the soil and situation. Thus, for example, under unfavourable circumstances of soil the foliage is less dense, and the leaves are in every way smaller, than if the same species of tree be growing on more favourable localities. Leaves growing in full exposure to light are thicker, contain more chlorophyll in their parenchym, and have a much larger number of stomata than 70 Studies in Forestry [CHAP. iv. those growing in shade. The latter are sometimes only about one-third of the thickness of the former, and great differences in size may even be noticed in the buds throughout the winter. If young growth, that has hitherto stood in shade, be suddenly exposed to the full action of light, these thinner leaves are not always capable of carrying out the new and more energetic work thrust upon them ; hence they often fall into a sickly condition, which predisposes them to disease, and may even induce the death of the plant. Thus, in areas regenerated naturally, the clearance of the parent standards should be made gradually, although the period over which it must be extended varies considerably according to the kind of tree, and, for one and the same species, according to the concrete conditions of the soil and of the plants concerned. Broad-leaved deciduous trees can in general accommodate themselves comparatively easily to rapid transition from shade to light, owing to their leaves only lasting for one season • but in conifers this accommodative power is necessarily more gradual, and is least in those genera that retain their foliage for a long period, like Spruces and Silver Firs. The poorer the soil of any locality, and more particularly the nearer it approaches the minimum with respect to the water-supply requisite for the normal transpiration of any species of woodland tree, the greater is the necessity for a free supply of light in order to carry out in as thorough a manner as possible the assimila- tive process with the limited amount of sap and of nutriment yielded by the soil. But the quantity of foliage decreases along with these latter supplies. Hence it becomes of all the more importance that the limited amount of nutriment should be elaborated in a most thorough manner ; and this is only possible with the comparatively free exposure of each individual leaf to light and air. Or, in other words, this naturally leads to the formation of a loose crown of foliage, instead of a dense leafy canopy being maintained. Carbonic Acid or Carbon Dioxide (CO2) becomes de- composed under the action of light by the chlorophyll con- CHAP, iv.] The Food of Trees 71 tained in the parenchym of the leaves, and is assimilated, or prepared for being made of use for structural purposes, in different combinations of carbon 1. As on the average 0-03 % by volume, and 0-05 % by weight, of the atmosphere consists of carbonic acid, there is never any want of this essential factor to the due thriving of any kind of woodland tree in any given locality. Whilst there is no reason to deny to ordinary plants, with foliage containing chlorophyll, a certain capacity for absorbing nutriment directly from humus or organic matter in the soil, as is done by those which are not provided with chlorophyll, yet the thriving of woodland growth on soils poor in humus is of itself a proof that any direct absorption of carbon compounds by the root-system cannot be of essential importance to their existence. The discovery, by Sadebeck and Frank about nine or ten years ago, of the mantle of fungoid tissue around the extreme points of the rootlets of cupuliferous trees (Oak, Beech, and Chestnut), and since also proved in the case of other woodland trees, coniferous as well as deciduous, has given rise to a theory that the introduction of organic matter is often carried on by means of the symbiosis of a fungus or Mycorhiza at the points of the suction-roots. This Mycorhiza is supposed by Frank to act as a go-between, absorbing water, and nitrogenous and non-nitrogenous organic matter from the soil, and giving these to the rootlets, from which again the fungus receives other nourishment in exchange. According to Ramann 2, however, the appearance of the Mycorhiza must be considered as already the indication of an abnormal or diseased condition, rather than 1 The chemical process is probably as follows (see R. Hartig's Anatomic d Physiologic der Pftanzen, 1891, pp. 172 and 229): C2O + H2O = CH2O + 2O set free ; 6(CH2O) = C6Hi2O6 dextrin, glucose, or grape und Physiologic der Pftanzen, 1891, pp. 172 and 229): C2O + H2O = CH2O + 2O set free ; 6(CH2O) = C6Hi2O6 dextrin, glucose, or grape sugar, in which form the assimilated product is capable of being translated from the leaves to other parts of the organism. When formed quicker than it can be transported, this loses one molecule of H2O, and becomes C6H10O5 or starch, which is secreted temporarily in the solid form and transformed again into grape sugar, when required, by resuming the molecule of H2O. 2 Ramann, Forstliche Bodenkunde und Standortslehre, 1893, p. 302. 72 Studies in Forestry [CHAP. iv. a genuine symbiosis bringing mutual advantages both to the fungus and the tree. Oxygen (O), requisite for the process of respiration, is, like carbonic acid, always present in sufficient quantity in the atmosphere, which is composed of 20-93 % oxygen and 79-04 % hydrogen by volume, or 23-28 % oxygen and 76-67 % hydrogen by weight. Unless, however, the aeration of the soil is also favourable, it may happen that the root-system has difficulty in finding a sufficiency of oxygen for the supply of its requirements. Ebermayer found that under Beech the soil was always much poorer in carbonic acid than under crops of Spruce and on fallow land, a fact which he ascribed to the better aeration of the soil by the numerous and deep-going roots of the Beech. Ramann agrees with this view and adds * : — 'The "soil-improving" action of the Beech is probably mainly ascrib- able to its thorough aeration of the soil. As a large percentage of carbonic acid in soils rich in humus indicates a considerable reduction in the amount of oxygen in the air circulating throughout the soil, there is no reason why the former should be advantageous to plant life — on the contrary, the greater amount of carbonic acid may rather be taken to be a sign of deficient aeration and of deterioration in the soil/ Prof. Ebermayer's own most recent utterance with regard to the soil-improving qualities of the Beech — an opinion that must be accepted as of the highest authority — is by no means so direct and unconditional as the above. It is as follows 2 : — ' The shallow surface-roots of the Beech mostly ramify throughout the loose upper layers of soil that are rich in humus. Under normal circumstances the suction-roots are not here provided with hairs, but are covered with a fungus (Mycorhiza^, which acts in the capacity of a go-between with respect to water and food-supplies, and by means of which the trees derive much better nutriment from the layers of soil rich in humus, than is obtainable through the root-hairs from the mineral soil (B. Frank). A very valuable attribute of the Beech is that, judging from my numerous investigations as to the influence of woodland growth on the percolation of soil-moisture and on the chemical compo- 1 Op. cit., p. 266. . 2 Forstlich-naturwissenschaftliche Zeitschrift, 1893, p. 237. CHAP, iv.] The Food of Trees 73 sition of the air contained within the soil, in consequence of the ramification of its roots it keeps the soil more open or porous than the Spruce does. To this property, combined with the circumstance that it is a shade-bearing species of tree, which yields a more nutritious and more easily decomposible humus than the conifers, it owes its soil -improving capacity and its great importance for mixed forests.' Where aeration is insufficient, the same practical effects take place as in the case of inundations. The plants consume the available supplies of oxygen within reach of their root-systems, and then sicken and die off ultimately, although of course different kinds of plants show great specific differences with regard to their accommodative power in this respect. Nitrogen (N) is essential to the formation of the albuminoid substances which play so important a part in relation to the growth of plants. When organic matter decomposes, the nitrogen becomes sooner or later transformed into ammonia (NH3), which again in turn becomes transformed with the aid of a fungus (as Winogradski has proved) into nitric acid or hydrogen nitrate (HNO3). For the development of this fungus (Bacillus), or main intermediate agency, a certain amount of oxygen is requisite ; but when there is a deficiency of oxygen in the air contained within the soil, nitrous oxide or nitrogen monoxide (N2O) and free nitrogen are produced. This nitrifica- tion is confined to soil within about 18 inches of the surface. Other sources open to plants for obtaining the requisite supplies of nitrogen are the ammonia contained in the atmospheric precipitations, and also, but under special circumstances only, the free nitrogen of the air. Observations have shown that the summer showers contain a higher proportion of nitro- genous combinations than those that fall in autumn or winter. Although the older agricultural chemists, led by Boussingault, and strongly supported in 1861 by the Rothamstead experiments of Lawes and Gilbert, denied that plants could directly utilize the free nitrogen contained in the air1, yet this was strenuously com- 1 Compare Prince Kropotkin's article On Recent Science in the Nineteenth Century for August 1893, pp. 205 et seq. 74 Studies in Forestry [CHAP. iv. bated by Ville all along, and since 1888 it has been abundantly proved by Hellriegel, B. Frank, Wilfarth, and others, that this can and does take place indirectly, more particularly in the case of Leguminosae (e.g. in the Acacia among our common trees). So long, however, as a supply of nitrogenous food is available in the soil, this capacity, for which the symbiotic aid of a Bacillus (Bacillus Radicicola or Rhizobium leguminosarum} is requisite, is not called into play *. The researches of these last-named scien- tists during the last decade have shown that all leguminous plants possess, by means of their root-nodules or tubercules, which contain these bacteria, the power of withdrawing from the air a sufficient supply of nitrogen for the requisite formation of essential albuminoid substances when these are not other- wise easily obtainable. According to Frank's researches also 2, the Alder is endowed with similar capacity to the Leguminosae for the formation of nitrogenous and albuminoid substances ; for the tubercules on its roots are found to contain an albu- minoid protoplasma filled with the germs of a bacteroid fungus. Through a symbiotic process quantities of albumen are pro- duced within these root-nodules, which become gradually absorbed into the tree and utilized for general requirements. Alders therefore thus appear, like the Acacia, able to derive supplies of nitrogen from the air, when requisite, through this symbiotic aid. So far, however, as woodland crops are con- cerned, though any abnormal increase in the ordinary supply of nitrogen obtained from the soil might probably exert great influence on the extent of seed-production and the frequency of mast-years, it certainly would not stimulate the increment in timber3. The precise manner in which woodland trees obtain the supplies of nitrogen requisite for their development has not yet been satisfactorily determined. But as woodland soils contain at best very small amounts of nitric acid, and are 1 Ramann, op. cit., p. 306. 2 Report of the Deutsche Botanische Geselhchaft for 1891, p. 250. 3 R. Hartig, op cit., p. 221. CHAP, iv.] The Food of Trees 75 often totally deficient in it, their wants must be met by the nitrogenous compounds set free on the decomposition of organic matter within the soil ; and, even from this alone, one important function of the invaluable humus or leaf-mould can easily be seen. The warmer a soil, the more thorough its aeration, and the more its supply of moisture is removed from either of the extremes of dryness or wetness, so much the more rapidly and successfully will the nitric acid (so essential for agricultural crops especially) be evolved from decomposing organic remains. But as nitric acid is apt to be easily washed out of porous soils, this partially explains why loose sandy soil is less fertile than loams and other soils of a more retentive nature. Water (H2O) is also one of the essentials to the support of plant life. It not only forms a very direct source of nutriment, but it is also requisite for the solution of inorganic substances (nutrient salts\ which can only be absorbed by the root-hairs when held in solution. By far the greatest portion of the water that is imbibed is transpired through the foliage. A certain quantity, however, is utilized in the formation of the organic tissue, the requisite hydrogen being exclusively obtained from this source; whilst, during the process of assimilation, the organic substances are formed from water and carbonic acid by the elimination or setting free of oxygen (when CO2 + H2O becomes CH2O + O2 &c. : see note i to page 71). The requirements of woodland crops as to water vary greatly according to the species of tree, and for one and the same species according to the nature of the soil, the climate, and the exposure of any given locality. The finer the particles of soil, and the richer the admixture of humus, the more moisture can a soil contain. In situations with humid atmosphere the spiracles of the leaves open much wider than in dry air ; for the leaves have a certain power of accommodating themselves to the temporary conditions of the atmosphere so as to stimu- late transpiration during a humid, and to retard it during a dry, state of the air. They are thus endowed with a certain Studies in Forestry [CHAP. IV. capacity for regulating and maintaining as steady a rate of transpiration as possible. For all kinds of woodland crops, however, there is on the one hand a minimum supply of water requisite for thriving and for healthy development, and on the other a maximum normal limit beyond which any surplus of soil-moisture is prejudicial to their well-being. Although, with decreased transpiration, the process of assimi- lation may not be essentially interfered with, yet the imbi- bition of soluble salts is considerably decreased, and the amount of ashes or mineral constituents contained in the wood is less than in timber produced in a drier atmosphere. Observations relative to the amount of "water transpired by woodland crops were made by von Honel in experiments made in 1879-1881. He found that, with the exception of the deciduous Larch, conifers transpire on the average only about one-sixth to one-tenth of the quantity of water that is evaporated by broad-leaved trees l. Taking the average of these three years, his experiments led to the result that the average transpiration of water per 100 grammes (0-22 Ibs.) of dry leaf-substance amounted during the active period of vegetation annually to the following number of Kilogrammes (2-204 Ibs.) : — Broad-leaved Trees. Conifers. Aspen Kilogrammes. - QtvQ7O Kilogrammes. Larch 120-234 Alder Q3.3OO Spruce ... . 13-501 Lime . 88-3.4.0 Scots Pine 9-426 Ash . . . . . . 85-615 Silver Fir 7>J79 Birch 81.4.33 Black Pines 6-735 "Rpprh Hornbeam Elm 74 °59 73-107 66-170 Mean average for all trees . .... 69-800 Sycamore . e;8-<;o6 Mean average for broad- leaved trees . . . 82-520 Mean average for conifers 1 1-307 Oak . . . Maple c 3.-o6^ He also found that, whilst in conifers transpiration is greatest from foliage fully exposed to insolation, in broad-leaved trees it was greatest from foliage growing in shade, as the following table shows : — 1 See Ramann, op. cit., pp. 309-312. CHAP. VI.] The Food of Trees 77 • Kilogrammes per 100 grammes of dry leaves. In the sun. In the shade. Beech 76-180 81-300 61-690 19.150 13.910 8760 107-800 98.900 76-190 5-020 4-850 5-250 Hornbeam Sycamore . Scots Pine .... Silver Fir Black Pines .... As, however, the normal density of foliage, natural to the different kinds of woodland trees, varies greatly with each species, and also for one and the same species of tree according to the nature of the soil, the age and the method of treatment of the crop, and various other factors of sylvicultural importance, these data, which are by no means complete or intended to be advanced as finally authoritative, are rather of theo- retical interest than of practical sylvicultural value. When investigating the actual quantity of water required by the Beech for normal transpira- tion annually, von HOnel estimated that — A Beech tree 35 years of age consumed per diem i kilo.= 2-204 Ibs. = 0-220 gals, of water. A Beech tree 50-60 years of age consumed per diem ... 10 kilos. = 22-040 Ibs. = 2-204 gals, of water. A Beech tree 115 years of age consumed per diem 50 kilos. = i 10-200 Ibs. = n.O2Ogals. of water. Computing the average number of trees per acre, he arrived at the following results : — Age of pure crops of Beech. No. of trees per acre. Amount of Water consumed Annually. Years. 35 50-60 "5 1, 600 520 160-240 Kilogrammes. 280,000 920,000 1,400,000 to 2,l6o,000 Gallons. 61,712 202,768 308,560 to 476,064 Hence a summer rainfall of 1 2 inches suffices to meet these requirements. But it should be remembered that the quantity of soil-moisture requisite for transpiration through the foliage must be very considerably 78 Studies in Forestry [CHAP. iv. less in our damp insular climate than in the inland tracts of the continent of Europe with their much drier climate and consequently enhanced activity of transpiration. There are many places along the east coast of England where even the total average annual rainfall is less than 12 inches, and where timber crops are still capable of thriving perfectly well. Of much more practical interest than von Honel's experi- ments must be considered the investigations that have more recently been made by Ebermayer with a view to determine the relative transpiration of the different kinds of forest trees, and the results of which correspond better than von Honel's with the facts of actual sylvicultural experience. Ebermayer analyzed foliage for the purpose of determining this by means of the percentage of water contained in the fresh leaves, and of *pure mineral ash obtained afterwards from the combustion of the dry leaf-tissue. The former table is now given, whilst that relating to the mineral ash will be referred to later on. It need only be remarked that, as the nutrient salts are imbibed in a weak solution, and as the water is mostly transpired through the foliage in the form of aqueous vapour, whilst the salts eliminated are to a great extent deposited within the leaf- tissue, a steady and normal degree of transpiration is essential for the due conduct of the nutritive processes and the well-being of the trees ; but during sunlight, and also in warm dry situa- tions, the rate of transpiration is of course greater than in shadow, or in cool, damp exposures, and at high localities where the relative humidity of the air is great. Hence, coeteris paribus, it seems justifiable to conclude that leaves, which show large accumulations of pure mineral ash within them, not only make larger demands for mineral nutrients per unit of weight of foliage, but also at the same time transpire more water through their leaves in order to concentrate these de- posits. For the solutions taken up by the rootlets of various kinds of trees do not appear to vary much as regards strength (except in localities like Alder swamps where the solutions are abnormally weak), although of course in fertile soils (or on CHAP. IV.] The Food of Trees 79 manured land) the solutions are richer than in land of inferior quality. Proceeding from this point of view, Ebermayer made the following classification of trees with regard to their relative power of transpiration or relative requirements as to soil- moisture, by tabulating them according to the percentage of water the fresh leaves contained as compared with their total weight. Broad-leaved Species of Trees. I. *7O II. Oak 61 Horse Chestnut . . . Ash . . • k , 6* White Alder . 6* Elm . . ^5 . 61 . 64 . . 6* Acacia (Robinia) , . 6\ III. Birch . 61 IV. Beech . 57 Mountain Ash 61 Hornbeam .... cy Sycamore . . 61 Willows (in general) . Maple . 60 CQ Aspen . CQ Coniferous Species of Trees. I. Cembran Pine . Black Pines . . Larch .... Weymouth Pine II. 64 Scots Pine - f 63 Spruce. . . . 62 Mountain Pine . 61 III. 59 Silver Fir . . . 55 59 57 Taken on the whole, these scientific conclusions correspond fairly accurately with the knowledge acquired by sylvicultural experience, although at the same time certain kinds of trees, like Acacia, Birch, and Pines, are better fitted than other trees to accommodate themselves to conditions not exactly satisfying their normal requirements with regard to moisture. It cannot 8o Studies in Forestry [CHAP. iv. fail to be noted from the above that long-needled Pines transpire more freely than the true Firs having short foliage. But in the conifers (which, as has been previously remarked, require only about J- to y1^ as much water as broad-leaved trees) the rate of transpiration is limited very considerably by their thick, strongly-cuticularized epidermis impregnated with resin and wax. Hence, not only the rate of transpiration, but also the movement of the sap upwards within conifers is much more sluggish than in deciduous trees like the Oak, Ash, Elm, &c. And whilst the needles, with their weaker transpiratory capacity, contain as much water as the leaves of many kinds of deciduous trees, the woody tissue of conifers contains more water than that of the latter. The Indispensable Mineral Ingredients in the food- supplies of plants comprise Potash, Lime, Magnesia, Iron, Sulphur, and Phosphorus as well as Nitrogen. And at the same time Silica (often in large quantities), Chlorine, Soda, Manganese, and occasionally Alumina, are also to be found in the ashes of timber, after Carbon, Hydrogen, Oxygen, and Nitrogen have been eliminated by combustion ; but the former can hardly be considered indispensable constituents. The different uses to which these mineral substances are put in the vegetable economy have not yet been quite satisfactorily determined. Potash (K2O) is found chiefly in the foliage and the parts of more recent growth, which are concerned with the active processes of assimilation and of vital ac- tivity. Lime (CaO) is supposed to play a very important part in connexion with the formation and distribution of the carbo-hydrates, and in the formation of insoluble com- pounds with oxalic and similar injurious acids which are thus rendered harmless to the tender tissues of the plant. Whilst Beech and Black Pines show a decided preference for soils rich in lime, it has been proved by Fliche that even a slight percentage of carbonate of lime seems to act as a poison in the case of the Sweet Chestnut and the Maritime CHAP, iv.] The Food of Trees 81 Pine1. Magnesia (MgO) is utilized in the formation of albuminoid substances, and is supposed to have an important influence with regard to the production of seed. Iron (FeO and Fe2O3) is requisite, though only in small quantities, for the formation of the chlorophyll in the foliage, by means of which the work of assimilation is carried on with the aid of sunlight. Sulphur, taken up in the form of sulphates, i. e. salts containing sulphuric acid2, is, like magnesia, employed in the formation of albuminoid substances, for which also Phosphorus, in the active form of phosphoric acid (P2O5), is most essentially requisite. The presence of Chlorine (Cl) and of Soda (Na) is most pronounced in plants growing near the sea-coast and on brackish soil. The specific action of these minerals is not very clearly understood ; but they are supposed to assist in the movement of carbo-hydrates within the plant*. For the practical purposes of Forestry the most important soil- nutrients are water, then lime, potash, and phosphoric acid; and the chief nitrogenous compounds are nitrates and am- moniacal salts or certain nitrogenous organic constituents in humus. On soils which offer to woodland crops richer supplies of food than can be thoroughly assimilated by them, deposits of mineral substances take place within the plants in excess of their physiological requirements. Wherever this occurs in any excessive degree, it leads to a condition at once pre- disposing to disease and, at the same time, capable of offering least resistance to any attacks that may be made by fungoid parasites or by insect enemies. 1 Annales de la Station Agronomique de I'Est, 1878, pp. 3 et seq. 2 A common impurity to a slight extent in the atmosphere is sulphurous acid, which is carried by rainfall into the soil, and oxidizes into sulphuric acid (SO2fH2O becomes H2SO4). When present in the air in anything like excess, as in large towns and at all populous and manufacturing centres, where sulphurous acid is evolved on the combustion of mineral coal, it affects the thriving of trees. The sulphurous acid is imbibed by the foliage, and, on rain falling, becomes transformed into sulphuric acid ; this rapidly acts as an irritant poison with regard to the internal, soft, cellular tissue of foliage. G 82 Studies in Forestry [CHAP. iv. The demands of the different species of woodland trees vary greatly with regard to mineral nutriment, as can be proved easily by an analysis of the amount of mineral matter found in the ash yielded on combustion and elimination of the non-mineral portions of their tissue (formed by Carbon, Hy- drogen, Oxygen, and Nitrogen). The younger parts of the organism, and especially those actively engaged in the work of circulation, assimilation, and secretion (the foliage and the cambium), yield more ash because they are richer in salts of potash, phosphates, and nitrogenous compounds, than the older portions (the alburnum), and the lifeless tissue in the interior of the stem forming the hard heartwood (the duramen). The leaves are much richer in mineral matter than any other part of the plant ; whilst the bark contains more than the wood, and the younger portions of the tree contain more than the older portions. When parts of the tree are about to die off (as, for example, in the case of the foliage of deciduous trees in autumn), the more important classes of mineral nutrients — Potash, Phosphoric Acid, Magnesia, Lime — are transferred into the still active portions of the organism, to which they wander back together with albuminoid substances and soluble carbo-hydrates. The total proportion of mineral matter in the timber of broad-leaved genera of trees is seldom under J% or exceeding \% of the dry substance of the wood. It usually ranges between 0-3 and 0-45%; but, in the case of Birch and of conifers, it varies from about \ to \% (0-17 to 0-27). The heartwood of old sterns contains less ash than the sapwood. It is also comparatively devoid of albuminoid substances, and is therefore more durable, i.e. it is less exposed to the disinte- grating and decomposing influences of alternating damp and heat, or to the organic attacks of saprophytic fungoid growth and insects. According to the demands of the different kinds of trees for food- CHAP. IV.] The Food of Trees supplies, their wood shows the following- percentages of mineral matter per TOO parts of dry tissue, according to Ebermayer1 : — Class of Trees. Wood of the Percentage of Ash. Potash. Lime. Phosphoric Acid. Deciduous Stem Twigs and small! branches) 033-0.94 0-75-2.00 c-o6-o-i6 0-16-0.46 0-10-0-65 0-21-1.39 003-0-06 0-12-0-30 Coniferous Stem . Twigs j and small > branches J 0-31-0.45 LOI-2.30 0.04-0-15 0.11-0-40 0.06-0.14 0.25-0-44 0-OII-0-027 O-IO-O-22 In the majority of plants cultivated by the farmer the quantity of pure ash left after the combustion of the dry tissue varies from 6 to 8% of the total weight. And, according to the same high authority, the annual demands made by pure crops of forest trees, for the formation of wood only, are per hectare in kilogrammes, or approximately per acre in Ibs. avoirdupois, as under : — Species of Tree. Age of Crop. Total Quantity of Ash. Potash. Lime. Phosphoric Acid. years Ibs. Ibs. Ibs. Ibs. Scots Pine So-IOO 12-16 2—3 ^_H i t2 Spruce . . IOO-I2O 23-24 4-5? 9-11 2| Silver Fir . 9° 39 IO 4^ 3 Beech . . Hornbeam 4° 30-49 3° 6|-8J 15-20 20 a^4l Common Alder . . 70 18 2 13 i| Birch . -. 5° •*i 2i 4 4 And in investigations in which all previous thinnings were left out of calculation. Beech . . 50 23i 5 nf •I Oak (Q. ses- silt/lora) . • 27i 3 20| i 1 Forstlich-naturwissenschaftliche Zeitschrift, 1893, pp. 225, 226. G 2 84 Studies in Forestry [CHAP. iv. In trees on which the bark long remains thick and fleshy, larger quantities of mineral deposits are stored up in the rind than in those which tend to the early formation of a rough and rugged cortex. As the great bulk of the mineral matter is to be found in the foliage of trees, it therefore follows that woodland crops must make the greatest demands on mineral nutrients just at the time when they develop the greatest density of leaf-canopy — that is to say, about the twentieth to thirtieth year for Scots Pine, the thirtieth to fortieth year for Spruce, and the fortieth to fiftieth year for Oak and Beech, on the better classes of soil, or perhaps about a decade later on soils of poorer quality. On the inferior classes of land it is therefore just about these ages that crops of those particular kinds of trees will be most likely to show signs of the soil not being able to supply easily the normal demands made for fully adequate supplies of nutrient salts. But, at the same time, the absolute demands in this respect vary enormously in the different genera and species of trees. For the production of any given volume of wood, Weymouth Pine, Scots Pine, and Birch make relatively the smallest demands on mineral nutriment ; after these follow Alder, Spruce, Silver Fir, Hornbeam, Beech, and Oak ; whilst Ash and Acacia make the greatest demands. The quantities of the different kinds of mineral nutrients, required annually by the various species of woodland trees for their normal production of wood, range between wide limits for the different individual kinds of trees, as the above table shows. But mere analyses of the timber alone will give no useful key to the total annual requirements; for, as has already been stated, the most of the mineral salts absorbed from the soil are finally stored up or deposited in the foliage during the process of assimilation, and are returned again to the soil after the fall of the leaf. It may, however, in passing, be again briefly remarked that, for the production CHAP. IV.] The Food of Trees of wood only, the demands vary as follows in high-forest crops of various sorts : — With regard to Lime from 4 to 20 Ibs. per acre per annum. Potash „ 2 to 10 „ „ „ „ Phosphoric Acid „ | to 4^ „ „ „ In order to arrive at more definite estimates than these investigations alone could yield, Ebermayer made analyses for the purpose of determining the amount of mineral ash con- tained in the dried foliage of the more important kinds of forest trees, and obtained the following results as to the percentage of pure ash deposited in the dry leaf-tissue. A. DECIDUOUS, BROAD-LEAVED TREES. Ash 7.61 I. Exacting. Italian Poplar . 7-04 Elm 6-Q2 Lime . ... \j yt 6-Kc; II. Making considerable demands. Mountain Ash . . . Acacia (Robinia) . . Horse Chestnut . . 6-2O 6.16 6-03 Ill Making moderate de- Sycamore .... Maple Aspen . . 5-33 5.21 e.ic mands. Willow Oak 5-II 5-10 IV. Making slight demands. Silver Poplar . . . Hornbeam .... 4.69 4-20 4-02 White Alder . . . 3-92 3-9° Common Alder . . . 3.69 86 Studies in Forestry B. CONIFEROUS TREES. [CHAP. IV. I. Making greatest de- mands. Silver Fir . . t . Cembran Pine . . . Larch . . ~. . 2-93 2.78 2-K.A Spruce 2. 3Q II. Making moderate de- mands. Weymouth Pine . . Scots Pine . . v. . • oy 2.35 2-28 III. Making least demands. Black Pines .... Mountain Pine . I. 2 I-36 From these tables it appears that none of the conifers make anything like such large demands as the broad-leaved genera of trees per unit of foliage; for the most exacting of the former makes considerably less demand than the least exacting of the latter. But the amount of nutrients annually withdrawn depends on the total quantity of foliage and of timber formed annually; and, as yet, no exact data of this description have been collected and tabulated. As a matter of actual experience, however, we know that soil improves greatly under coniferous crops, so long as a good canopy of foliage is maintained ; hence there is good reason for believing that, in making very moderate annual demands, they enable the capital in nutrients to be increased within the soil year by year. But the very favourable physical influences exerted simultaneously on the soil by means of the canopy of ever- green foliage overhead must not be left out of the reckoning when this matter is being considered. It will be noted, by a comparison of the above table with that previously given for requirements as to water, that, in a general way, the trees transpiring most freely, also with- draw the largest mineral food-supplies from the soil. And these results correspond very fairly with actual sylvicultural experience. Where discrepancies seem apparent, a study of all the circumstances connected with the growth of the tree CHAP, iv.] The Food of Trees 87 in question will soon explain the paradox. Take the case of the Acacia (Robinia) for example. The analysis of its foliage distinctly shows it to belong to the exacting class of trees ; and yet it is to be seen in vigorous growth on soils of inferior quality. It must, however, be borne in mind that the total leaf-production of the Acacia is not heavy ; hence, even on poor classes of soil, it has less difficulty in supplying its higher requirements per unit of weight of dry leaf-sub- stance than other genera having more moderate requirements in this latter respect but endowed with a heavier total crop of foliage. And that, in the case of this particular tree, the symbiotic aid of the Bacteria — which are to be found in the nodules of all Leguminosae^ and which are capable of assimi- lating nitrogen from the free nitrogen of the air — may possibly be of assistance in supplying nitrogenous food, to be used for the easier assimilation of other mineral food, is not at all difficult of comprehension. In the case of the Ash, again, which makes the greatest demands of all the woodland trees as to mineral food-supplies per unit of weight of dry leaf-substance, this really withdraws only a moderate actual quantity of nutrient salts from the soil, as its total amount of dry leafy substance is slight compared with that of many other genera of trees, which require smaller quantities of nutrients per unit of dry leaf-tissue, but yet with- draw far larger total quantities from the soil annually. Subject, however, to the Law of the Minimum, referred to at the open- ing of this chapter, the productive capacity or fertility of any soil is dependent on the quantity of nutrients available within it in a form that can be absorbed by the rootlets, and on the extent to which their absorption is favoured by the combination of the various physical factors determining its tenacity, moisture, warmth, and depth. But every soil is not,, as one of the earlier sylvicultural chemists, Gustav Heyer, asserted \ adapted to the 1 Forstliche Bodenkunde tmd Klimatologie, 1856, p. 3. He assumed that almost any soil could produce any given kind of timber, if it only had the requisite amount of moisture. 88 Studies in Forestry [CHAP. iv. growth of every kind of forest tree ; for the supply of nutrients available in a soluble form varies with the chemical and the physical composition of the different classes of rocks, the degree to which disintegration and decomposition have ad- vanced, the depth of the soil permeable by the root-systems, the amount of organic matter contained in the soil, and the physical properties with which this is endowed. And the want of any one food-material, or perhaps even an unfavourable condition of one physical factor (more especially one of those relating to moisture or depth), may render a soil unsuitable for the normal development of any given kind of tree. But, undoubtedly, the inferiority of many woodland soils may also be due to poverty in one or other of the essential soluble nutrients, though this is generally combined at the same time with unfavourable physical conditions. The object of scientific sylviculture is, therefore, to plant only such trees as are most likely to attain normal development, and to yield the best monetary returns, without exhausting the soil or allowing its physical properties to become prejudiced or impaired by want of protection from sun and wind. From this it follows, theoretically, that the cultivation of coppice- woods, in which the crop is formed entirely of small branches containing relatively larger quantities of mineral sub- stances than are to be found in mature wood, must tend to exhaust the easily available supplies of lime, potash, and phos- phoric acid sooner than crops grown under high-forest. And this theoretical deduction coincides exactly with the results of practical experience; for it is well known that Oak-coppice for tanning-bark, or Osier-holts for withes, should only be made on good land, and that if inferior soil be cleared of Oak- coppice every twelve to sixteen years, it runs great risk of deteriorating. The treatment of timber-crops in high-forest is, as long sylvicultural experience has clearly shown, the most conservative manner of utilizing the soil; whilst copse or coppice tinder standards stands about midway between the CHAP, iv.] The Food of Trees 89 two other systems, as being less exhausting than coppice, though more exacting than high-forest. High-forests of timber can never lead to exhaustion or deterioration of the soil, so long as this remains protected by a sufficient leaf-canopy, and is not robbed by wind, or other- wise, of the natural manure obtainable through the decom- position of the dead foliage. On the contrary, and more especially in the case of trees like Scots Pine and Spruce, which make lower demands for potash and lime than other species, it is almost always the case that the nutrient salts contained in an available form within the soil at the end of the period of rotation, i. e. on the fall of the mature timber, are considerably in excess of the quantity that was present at the time of such crop being formed — provided always that the fertility or productive capacity of the soil has been duly safeguarded by the maintenance of a good, unbroken canopy of foliage throughout all the life-periods of the crop. For this reason, woods formed of trees like Pines, Spruces, and Firs, recommend themselves for the recuperation of the productive energy of soils that have been allowed to deteriorate by being kept long under lightly-foliaged kinds of trees, like Oak, Ash, Elm, or Larch ; because the broken canopy formed by these light-demanding species is unable, without the aid of under- growth, to protect the surface-soil from the exhausting influ- ences of sun and wind, and from having the accumulated supplies of humus consumed unprofitably by a more or less rank and unremunerative growth of weeds. CHAPTER V iV \ I SOIL AND SITUATION IN RELATION TO WOODLAND GROWTH 7 I. Soil in Relation to Woodland Growth. ,/ BY Soil is understood the product of the decomposition of the rocks forming the crust of the earth. Soil is formed mechanically and physically by rains, frosts, rivers, volcanoes, &c., or chemically and organically by oxidation, deokidation, and changes effected by carbonic acid. Through its permea- bility and its other physical factors, the soil enables trees to develop the root-systems necessary alike for their support mechanically and physiologically. By far the greatest portion \J of the food of all plants possessing chlorophyll is obtained from the carbonic acid of the atmosphere ; but certain neces- sary substances (nutrient salts) are only obtainable from the soil when held there in solution, so that they may be imbibed by the rootlets. A distinction is made between the soil or surface-soil and the subsoil. The former consists of the usually more thoroughly decomposed earth forming the upper layer permeated by the root-system ; whilst the latter may, or may not, be of similar composition to the superposed layer. Even when such patent signs of shallowness of soil as stony outcrops are not visible, the want of depth may easily be noted by the stunted appearance of the timber-crops, in which, owing to the deficiency in soil-moisture and food-supplies, an CHAP. V.] Soil and Situation 91 abnormal development of the root-system takes place relatively to the ascending axis, and to the crown of foliage charged with the duties of transpiration and assimilation. The chief signs of depth of soil are length of bole, fuller coronal develop- ment, and richer soil-covering of underwood, brushwood, and weeds. A tolerably correct estimate may, in fact, be obtained concerning the depth and the general quality of the soil from the mean average height of the timber crops on such soils as are usually to be found under woods. Thus Grebe gives the following averages for the Thiiringer Wald in the middle Saxon states J :— AGE OF FOREST IN YEARS, AND AVERAGE HEIGHT IN FEET. Kind of Forest. Quality of Soil. Yrs. 40 Yrs. So. Yrs. 60 Yrs. 70 Yrs. 80 Yrs. 90 Yrs. 100 Yrs. no Yrs. 120 ft. ft. ft. ft. tt. ft. ft. ft. ft. I. 43 55 69 81 90 97 103 107 I09 II. 37 48 60 69 84 88 91 93 Spruce . . III. 30 40 49 58 64 69 72 75 76 IV. 23 30 39 45 5° 54 57 58 V. 16 21 27 32 36 39 40 — — I. 39 52 65 75 84 90 95 98 96 II. 36 47 58 67 73 79 83 85 98 Scots Pine III. 41 49 57 62 66 68 70 IV 25 33 40 45 48 51 53 54 — V. 25 29 33 36 37 38 — I. 34 48 59 69 78 84 89 92 94 II. 29 41 5° 59 67 73 76 79 81 Beech III. 24 33 42 49 57 j 61 64 66 67 IV. 19 27 33 40 44 48 50 8* 52 V. (Not grown on such inferior soil.) How the general quality of the soil affects the outturn in timber from the different kinds of woodland crops may be seen 1 Die Betriebs- und Ertragsregelung der Forste, 2nd edit. 1879. These heights are of course only rough approximations so far as growth of these trees in Britain is concerned. But there is no climatic reason why they should not be equalled, or even excelled, in properly managed woods. 92 Studies in Forestry [CHAP. v. from a reference to the tables on pp. 43-45 of the author's British Forest Trees (1893). The Chemical Composition of any soil is in so far of im- portance to tree-growth that each of the necessary mineral constituents, always found forming part of the ash to which timber may be reduced by combustion, must be present in it in sufficient quantity in a soluble form. The adaptability of any given soil for the growth of any particular species of woodland crop is determinable by the Law of the Minimum, according to which the minimum amount of any one essential constituent of the necessary food-supply in the soil limits its total productive capacity for a given kind of timber. Thus, for example, Oak and Beech extract very much more potash and phosphoric acid from the soil for the production of their timber than Scots Pine or Spruce ; hence the latter may thrive well on soils where (according to the law of the minimum) the former are of exceedingly indifferent growth owing to the com- parative scarcity of these ingredients. As a matter of fact most soils contain the essential con- stituents of tree-food in sufficient quantities to maintain tree- growth of any kind. But as they are not always held in solution, they are not continuously available for imbibation by i/ the root-system ; for it is only when occurring in the form of soluble salts, that the nutrients can be absorbed by the suction-rootlets. It was from this point of view that Gustav Heyer asserted that almost any soil could produce any given kind of timber, provided that it contained the requisite degree of moisture — an assertion which, as has previously been shown, is only approximately, but not scientifically correct. Sylviculture varies essentially from Agriculture in being less J directly dependent on the fertility or inorganic richness of the soil. Though it is quite certain that rich soils, yielding toa copious supplies of food-material to be assimilated thoroughly, would produce large quantities of timber, yet it would be of a soft spongy nature, little able to withstand either the attacks CHAP. V.] Soil and Situation 93 of fungoid diseases whilst growing, or of red and white rot after conversion. According to Weber1, the analyses of different woods show that the composition of timber consists, on a rough average, of 50 % Carbon, 42 % Oxygen, 6 % Hydrogen, i % Nitrogen, and i % Ash only, for a great many of the mineral constituents abstracted from the soil are deposited in the foliage during the process of preparing the food- supplies for assimilation, and are returned again to the soil when defoliation occurs, and the dead foliage decomposes into humus or mould. But the whole demand for mineral food made by woodland growth is, roughly speaking, only about one-half of what it amounts to in the case of agricultural crops, according to the investigations made by Ebermayer2, which may thus be tabulated : — Average of 1-s jo |q |d 4 • lf° •H.I "a^O ther ituents. 3° wm £ 3o ^ «•«* >2^:c« 0| £ u Mixed agricultural crops .... 235 37 78 43 17 28 II 21 Woodland growth — timber & leaves 126 29 II 62 10 8 3 3 Woodland growth — timber only . 19 1.6 4 9 2 1.4 0-4 0-6 Approximate ratio of sylvicultural demands to agri- cultural needs . . * 3 * 1 if f * 7 As, in sylviculture, the greatest demands are for lime and silica, constituents abundant in every soil, and, as by the fall of the leaf, most of the mineral food is returned to the soil again, it will be at once apparent that woodland growth does not 1 DieAufgaben der Forstwirthschaft (Lorey's HandbucK}, p. 62. 2 Physiologische Chemie der Pflanzen, 1882, vol. i. p. 761. 94 Studies in Forestry [CHAP. v. exhaust the land to anything like the same extent as agricultural crops, which require manuring in order to supply deficiencies, and to stimulate the upper soil to increased decomposition. And when the dead foliage is retained on the ground and decomposes to form humus, this in turn exerts a very beneficial hygroscopic influence, stimulates the soil to more rapid decomposition, renders the mineral food-materials more easily soluble, and, in short, improves the productive capacity of the land, instead of exhausting it. This shows the importance of maintaining a close leaf-canopy, and of adopting all practical measures in order to obviate insolation of the soil, and prevent the free play of winds that may remove the foliage and exhaust the surface-moisture. But the mineral constitution of the soil is not the only factor determining its productive capacity sylviculturally ; for various physical factors are of equal, and often greater, importance — e.g. depth, porosity (aeration), consistency, &c. So far, however, we may be guided by practical experience as to assert that Elm, Maple, Sycamore, and Ash can only be grown satisfac- torily on fertile soils ; whilst Birch and Pines are least exacting as to mineral richness. Between these extremes, Oak, Beech, Lime, and Silver Fir make somewhat greater demands than Sweet Chestnut, Larch, Hornbeam, Spruce, Alder, Aspen, and Willow. When planted out on soils not naturally favourable to their growth and development, Scots Pine and Birch show a decidedly greater capability of accommodating themselves to any given conditions than Oak, Beech, Spruce, and Silver Fir; whilst Ash, Oak, Elm, Maple, and Sycamore — those genera whose demands on fertility are greatest — possess the least power of accommodation. Soils are largely made up of Salts, with Oxides and some- times Chlorides. The Salts are mostly Silicates (often com- bined with water), Carbonates, and Sulphates; whilst the Phosphates, so important for plant-life, only occur occasion- ally. In the formation of these Salts, the most important of the Acids are Silica (Si O2), Carbonic acid (CO2), Sulphuric CHAP, v.] Soil and Situation 95 Anhydride or Sulphur Trioxide(SO3) and Phosphoric Anhydride or Phosphorus Pentoxide (P.2 O5) ; whilst the chief Bases are Potash (K2O), Soda (Na2O), Lime or Calcium Oxide (CaO), Magnesia or Magnesium Oxide (MgO), Ferrous Oxide (Fe O), Sesquioxide of Iron or Ferric Oxide (Fe2 O8), Alumina (A12 O3), and Manganese Dioxide (Mn O2). The Silicates comprise quartz, serpentine, talc, felspars, mica, hornblende, augite, and chlorite; the Carbonates include carbonate of lime, chalk, and dolomite ; to the Sulphates belong anhydrite and gypsum or calcium sulphate. When the water of crystallization in many salts composing rocks becomes heated and driven off, the salt crumbles into powder ; and, at the same time, all rocks, being porous, are pervious to water, which not only dissolves certain salts, and holds them in solution ready for absorption by the roots of plants, but also effects transformations in many chemical compounds. Thus water impregnated with carbonic acid dissolves silicates con- taining alkaline earths and ferrous oxide, as also carbonate of lime (Ca CO3) and ferrous carbonate (Fe CO3) which are easily soluble in it, whilst magnesium carbonate (Mg CO3) is much less so. The products of the decomposition of rocks are mostly alkalies in combination with silica and carbonic acid, together with carbonate of lime, magnesia, and ferrous oxide, whilst soluble sulphate of lime is also found in most soils ; but as these salts act and re-act on each other, many various com- pounds are formed. Rocks of complicated structure decompose most rapidly, as, for instance, those rich in felspars, or in compounds of iron, in contrast with silicious slate or quartz-rock ; pure limestone de- composes slowly, but this difficulty diminishes with any increase of alumina and iron. Sandstones and conglomerates decompose in proportion to the cementing matter they contain, and to the degree in which this is affected by moisture. Fine-grained and massive rocks are less apt to fissure and crumble than coarse-grained stones or slaty beds, as they afford fewer points 9 6 Studies in Forestry [CHAP. v. of attack to water, mosses, herbage, and other disintegrating influences. Vegetation plays no unimportant part in the formation of earth, not only by helping to fissure and cleave the soil and subsoil, so as to enable water to effect an entrance, but also by reason of the decomposition of the organic debris of foliage, dead wood, &c., and the formation of humus or mould, which takes place under the combined action of oxygen, moisture, and a minimum warmth of 52° Fahr. When the humifica- tion takes place only under partial exposure to the atmosphere, humic and similar acids are formed, and saprophytic fungi aid in the work of decomposition, by attacking the albuminoid substances first of all. These acids (humic, ulmic, geic, &c.) have a strong affinity for ammonia (NH3), which is itself essential to the nourishment of trees, and which cannot be assimilated by the foliage from the free nitrogen of the air, although, as Hellriegel, Frank and others have shown, it can be obtained by the Leguminosae from the air circulating within the soil by means of symbiosis with a fungus (Bacillus radicicola) found in the nodules on the roots (see page 74). Humus condenses gases and atmospheric moisture, and possesses a certain amount of warmth, partly owing to reten- tion of atmospheric warmth received from sunshine, and partly to the generation of heat by the chemical process of decomposi- tion. Thus, whilst mechanically making clayey soils less stiff, and sandy soils more binding, it also warms the former, and makes the latter less liable to be affected by the changes in the atmospheric temperature. II. The Classification of Soils. Any classification of soils according to their geognostic or geological origin would be very misleading, for (i) the same kmd of rock does not always yield 'similar soil, (2) the quali- ties of the soil depend on the extent to which decomposition CHAP, v.] Soil and Situation 97 has taken place, and (3) some of the lighter products of decomposition (clay) are more easily washed away than others that are heavier (sand). Hence, for practical sylvicultural purposes, no better classification of soils can be adopted than that made by Grebe, which is now generally adopted at the experimental stations on the continent : — Sandy Soils, containing 75 % or more of disintegrated sand. They occur as sand-drifts, or are the product of the decomposition of sand- stones. Sand consists of abput 90 % of sand, and not more than 10 % of clay and other constituents. Loamy sand consists of about 75 to 85 % of sand, and from 15 to 25 % of clay and other constituents. Loamy Soils, always tinged with iron, containing 60 to 70 % of fine sand and silicious dust, the rest being chiefly made up of clay with less than 5 % of lime, and an almost constant quantity (5 %) of hydrated ferric oxide. Loam consists of about 60 % of sand and 40 % of clay. Sandy loam consists of about 70 % of sand and 30 % of clay. Clayey Soils, containing 50 % or more of clay. They are mostly formed from rocks rich in feldspars, augite, and hornblende, of sand- stones and conglomerates cemented with clayey cohesive substance, and of the clayey layers and bands throughout sandstones and lime forma- tions. Clay consists of about 60 to 70 % of clay, the rest being chiefly sand, and also other constituents. Loamy clay consists of about 50 % of clay, and 50 % of sand. Limy Soils, containing not less than 10% of carbonate of lime. They are produced chiefly by limestones, but also by other rocks containing lime felspar (labradorite). It often happens that limestone rocks produce a loamy rather than a limy soil on decomposition. Lime consists of at least 50 % of carbonate of lime, the rest being chiefly clay. Clayey lime consists of about 40 % of lime and 60 % of clay. Loamy lime consists of about 30 % of lime and 70 % of loam . When rich in carbonate of magnesia it is called dolomitic lime or dolomite. Marl consists of 10 to 20 % of carbonate of lime, with 80 to 90 % of clayey and sandy ingredients. Sandy soils have a coarse gritty feeling when slightly mois- tened. When there is any considerable admixture of loam, H 98 Studies in Forestry [CHAP. v. marl, iron, or humus, sandy soils are said to be loamy, marly, ferrugineous, or humose. Sands become easily heated or cooled, and have a poor capacity for retaining moisture and nutrient salts in solution j hence they form the inferior quali- ties of soil, on which trees require a considerable growing-space in order to obtain the requisite supply of food, fail to maintain good leaf-canopy, become deficient in increment, produce little seed, and are otherwise deficient in reproductive capacity. Owing to their becoming easily warmed by day, they stimulate to the early germination of seed, and movement of sap, and flush- ing of foliage in spring ; but, as they cool rapidly at night, this exposes the young vegetation to danger from late frosts. Earthy ingredients, and humus in particular, improve the quality of sandy soils. When forests approaching maturity show good development on such soils, their natural regeneration is safe and simple ; but where the tree-growth is indifferent, it is advis- able to resort to planting, as the young growth of seedlings is often too intolerant of shade to make natural regeneration under parent standards a success. In the planting up of such soils for the first time, Scots Pine is the best crop, mixed with whatever other species of trees may seem likely to thrive at all well, as, for example, Douglas Fir, Black Pines, Spruce, Menzies Spruce, &c. Clayey soils stick if brought in contact with the tongue, and smell of ammonia if breathed upon ; rubbed between thumb and forefinger they feel fatty to the touch, and take a polish or burnish if rubbed with the thumb-nail. They may be grey, yellow, or brownish-red in colour, and are usually tinged with iron. Their leading characteristics are tenacity, weak hygroscopic power, and impermeability to moisture ; but they are strongly retentive of moisture when once saturated. Such soils are cold, and are apt to become water-logged. Any con- siderable admixture of sand, iron, lime, or marl — forming sandy, ferrugineous, limy or marly clays — tends to modify these char- acteristics. As the soluble nutrient salts are not apt to be CHAP, v.] Soil and Situation 99 washed out of the soil, clays offer comparatively large supplies of ^ tree-food within a small space ; hence the crops have a greater density of leaf-canopy at all stages of their development than similar woods growing on sandy soils. Unless the subsoil be permeable, however, there is a danger of such tracts becoming marshy. Owing to their low conductivity of heat, woodland growth on clayey soils seems backward in spring. In the natural regeneration of mature crops a good deal of soil-pre- paration is usually required on clays in order to assist in the decomposition of the dead foliage, which often forms a thick layer on the soil in consequence of the density of the canopy overhead. Not only is more foliage thrown down, but this also retards the formation of humus by keeping the soil at a low temperature. On such soils natural regeneration is very easy; for the preliminary clearances stimulate to increased production of seed, and the young seedling growth bears shade better than on poorer sandy soils. The reproductive capacity of copse and coppice is also greater on clays than on sands. Limy soils effervesce when tested with drops of nitric acid. Marls and true limes are both comprised within this group; but in the former the limy constituent is equally admixed throughout each particle of the soil, whilst in the latter it is not. These also become by admixture sandy, loamy, clayey, or stony limes or marls. Limy soils are apt to be wanting in . depth ; but with careful treatment they often show fine growth of timber. Their consistency favours the equable distribution of soil-moisture, even on steep hill-sides ; hence the root-system easily attains normal development, and has few difficulties to overcome in satisfying its requirements in the way of food- supplies. But, when such soils have deteriorated through in- solation following on bad management, the soil-moisture is not f :' retained ; the finer particles of earth get washed away rapidly ; the soil rapidly becomes shallow, dry, and hot ; and timber production diminishes considerably. The re-wooding of dry, limy hill-sides is one of the most difficult of sylvicultural tasks. H 2 ioo Studies in Forestry [CHAP. v. Some very good results have occasionally been attained by sowing out lucerne (Medicago sativd] and beech-nuts at the time of planting out Austrian Pine (Pinus Laricio var. austriaca Endl.), the lucerne being left to form humus in place of being utilized as fodder. A soil-covering of dead foliage and humus on limy tracts is essential for the maintenance of a productive capacity anything like commensurate with their mineral strength ; hence natural regeneration is advisable when removing the mature crop. As the dead foliage rapidly decomposes, and seed-production is usually good on limy soils, little or no preparatory clearance is necessary previous to the seed- felling ; whilst, as the seed is generally of good quality and high germinative power, and the seedlings are not apt to wilt or droop under the shade of the parent standards, the regenera- tive process is comparatively easy. But, when limy soils are sandy or stony, greater care must be taken not only in making the regenerative fellings, but also in all the operations of tending throughout the whole life-period of the crop. Limy soils that are properly protected against insolation -are in every way well endowed with reproductive capacity as coppice. Loamy soils have greater resemblance to clay than to sand, but neither feel fatty when rubbed between finger and thumb, nor take any definite polish when rubbed with the finger-nail. A general mildness is their leading characteristic; but they approach more to the one or other of the three main groups according to the amount of sandy, clayey, or limy admixture ; contained in them. Though their capacity for absorbing and *.jT retaining soil-moisture is determined to a great extent by the nature of the subsoil upon which they rest, yet they are in general favourable to sylvicultural crops ; and the species of trees selected for growth are usually chosen for financial reasons, or for reasons connected rather with the physical properties than with the mineral composition of the soil. At high elevations with humid atmosphere the Spruce or the Douglas Fir is recom- mendable as the ruling species on loamy soils ; whilst at lower CHAP, v.] Soil and Situation ' ,', ; ; levels the Oak is one of the species thriving best in mixed forests of broad-leaved trees. Natural regeneration is easy on loamy soils when a good seed year comes round ; but, as good seeding or mast-years can not be depended on in crops on loam, it is best to sow seed procured from elsewhere rather* .XT than to risk deterioration of the soil from insolation after * once the preliminary fellings have been made. As the fertility or productive capacity of soils is neither dependent on, nor mainly proportional to, the mineral richness I ,r of the rocks from whose decomposition they are formed, no \^f hard and fast classification as to their mineral strength is possible. It can only be said that, in general, clayey soils are slow in forming humus and giving nutrients to tree-life, whereas . limy soils decompose organic matter rapidly and stimulate tree-growth, and that intermediate positions between these two groups are occupied by sandy and loamy soils, except when the sands are deficient in soil-moisture. All soils are improved by an admixture of humus to a mode- rate extent. It not only adds depth to the land, but, being .^f" of a strongly hygroscopic nature, also condenses and retains atmospheric moisture ; whilst, owing to its low conductivity, it protects the soil against evaporation. It is also directly active in aiding the continuous decomposition of the soil by means of the carbonic acid set free during the process of decomposi- tion. It modifies all extremes of physical properties in soils ; ' and though not an absolute necessity for the production of woodland crops, yet it is of inestimable value in stimulating the action of soils, no matter of what geognostic origin. Indeed, as Gayer remarks1, there can be little doubt that ' hu mus forms the most important factor relative to tree-growth, and -^ < E? is a priceless treasure as regards the production of woodland crops' And the beneficial influence it exerts on the aeration of soils is by no means its least important quality. When soils contain 20 % or more of humus they are termed humose ; fertile silt left 1 Waldbau, 1889, p. 27. Studies in Forestry [CHAP. v. after inundations is often of this character. Sometimes, as in the case of marshes, moors, and peat bogs, the accumulations of humose soil is so great that the roots of trees are unable to reach the mineral soil below it ; such formations usually take place on sandy soil resting upon clay. Ferruginous soils are coloured brownish-red, and contain at least 10 to 15% of ferric oxide or hydrated ferric oxide. But even by 2 to 5% of ferric oxide the general character of sandy soils may become affected, although considerably larger quan- tities may fail to effect any noticeable alterations in clayey or loamy soils. Thus moorpan, sometimes containing only about 2% of ferric oxide, is just as impenetrable to the roots of trees as iron-band or limonite with its 60 to 70%. In both cases tree growth is hindered until the impenetrable layer has been broken through, so as to allow of the roots reaching the sub- soil, and of the moisture circulating normally. III. The Physical Properties of Soils. To these, in a far greater degree than to the mineral com- position of any soil, is due its capacity to sustain timber crops, and to yield to them in due proportion the various forms of nutriment requisite for their growth, development, and reproduction. All the physical properties act and react on each other in determining the quality of any given land. Cohesiveness or Tenacity is the resistance offered by a soil to instruments used in separating its particles, or to force employed in disintegrating them. This property is not alone of importance in relation to air, moisture, and warmth, but also indicates the resistance to be overcome by the root- systems in penetrating into, and ramifying throughout, the soil. Clay soils have the greatest cohesiveness, sand the least ; lime approaches more to the clay, while loam resembles rather the sand. An admixture of humus tends to level all classes, making clays and limes less tenacious, and loams and sands CHAP, v.] Soil and Situation 103 more binding. The tendency of soils to expand with mois- ture, and to shrink on parting with it again, is practically proportional to its tenacity. Soils may be classified in this respect as — Heavy, stiff, or tenacious soils, which fissure and crack deeply when dried up. Clays and clayey loams, limes and marls belong to this class. Mild soils, exhibiting superficial cracks when suddenly dried up, but which when nearly dry have the power of retaining the form of clods. They are usually composed of favourable admixtures of clay, sand, and lime, as in loams, sandy loams, and loamy limes. Light soils, capable of forming clods when moist, but when dry show- ing a strong tendency to disintegrate, as in the case of loamy sands and sandy marls. Loose soils, which even when moist have little tendency to form clods. To this class belong the poorer sandy soils. Shifting soil, liable in a dry condition to be carried away by the wind, as in the case of sand-drifts and dunes. In a light soil, which is not deficient in moisture, humus, and ^ / mineral nutrients, a maximum of rootlets can be developed, and through these the maximum of timber. Hence one finds the greatest increase in cubic contents, and in particular the greatest average annual increment in height, on alluvial deposits having finely pulverized particles. But when loose soils are wanting in soil-moisture, planting operations are ,.- apt to be unsuccessful; for the plants have great difficulty in establishing themselves so as to send down their roots to lower levels and thus obtain an assured supply of the water requisite for transpiration through the foliage. Thus, on the sandy soils in some parts of Sussex, for example, seedling Oaks are only found to thrive when planted out among weeds, such as brambles, which keep patches of soil here and there cool and moist. The degree of moisture contained in any soil is one of the most important factors concerning woodland growth. No plant can grow without imbibing supplies of water; it is requisite for germination ; without it, the nutrient salts could IO4 Studies in Forestry [CHAP. V. not be made soluble for imbibition by the suction-roots, nor could transpiration through the foliage and assimilation possibly - ^ take place; it assists likewise in regulating the ^temperature-^' '' of the soil, by making stiff soils milder and loose soils more binding. But excess of soil-moisture interferes with the normal processes of decomposition, both of the soil and of the humus ; it leads to the development of injurious acids and acid solutions, and tends to the formation of marshes ; seed and roots also suffer from want of oxygen or insufficient aeration of the soil, and hence become easily infected with fungoid diseases; whilst, in consequence of its poor con- ductivity, and of the amount of heat necessary for raising the temperature of water, it both retards the natural activity of the soil, and increases danger from frost. Fineness of the soil- particles favours hygroscopicity, or absorption and retention of moisture ; whilst permeability, or diffusive capacity relative to moisture, is proportional to their coarseness. Soils are in these respects classifiable as follows : — Absorptive Power as to Power of retaining Moisture. Power of diffusing Moisture. (Permeability.) Rain Aqueous Vapour. I 2 Lime Clay Loam Clay Lime Loam Clay Lime Loam Sand Loam Lime 4 Sand Sand Sand Clay The addition of humus tends, however, to modify the various characteristic differences exhibited in these respects. With regard to the degree of moisture they contain, the following classification of soils has been adopted at all the sylvicultural experimental stations in Germany : — Wet, when water flows out, without pressure being applied, on a clod being lifted up. CHAP, v.] Soil and Situation 105 Moist, when water falls in drops from a clod on pressure being applied. Fresh, when only traces of moisture are left on the hand, after pressure being applied to a handful of soil. Dry, when the soil does not resolve itself into dust on being rubbed. Such soils lose their moisture within a few days after rainfall, and their colour is not much deepened by the moisture retained. Arid, when, on being rubbed, the soil resolves itself into dust that is carried away by the wind. Traces of rainfall rapidly disappear from such soil, and the slight quantity of moisture it is able to retain does not much affect its colour. Most of our forest trees — Oak, Beech, Maple, Spruce, Scots Pine, Larch, Silver Fir — thrive best on a fresh soil ; Willows, Poplars, Ash, Elm, and Hornbeam prefer a moist soil, and the Alder even a wet one ; but stagnating moisture is favour- able to no kind of tree-growth. Dryness of soil is not an essential for any of our forest trees ; but Birch, Rowan, Aspen, Black Pine, and Scots Pine in general, and Beech on a limy soil, appear to be able to accommodate themselves to less soil-moisture than other species. The sylvicultural qualities of a soil are frequently, to a very great extent, indicated by the nature of the forest weeds that grow upon it. Thus the following characteristic species of plants may be recognized : i. On wet or boggy soil: — Bog moss (Sphagnum^, hair moss (Polytri- chum), cranberry (Vaccinium Oxycoccos\ bog bilberry ( Vaccinium uligi- nosum\ heath or bell-heather (Erica Tetralix), marsh cistus or marsh rosemary (Ledum palustre), cotton grass (Eriophorum), sedges (Carex\ bulrushes (Sdrpus), rushes (Juncus), — the last three genera in many different species. a. On fresh fertile land, or soil rich in hu mus:— Raspberry (Rubus idceus}, bramble (Rubus fruticosus*) , red foxglove (Digitalis purpured), willow herb (Epilobium angustifolium) , deadly nightshade (Atropa Belladonna), balsam (Impatiens Noli-we-tangere], stinging nettle (Urtica dioicd), hemp nettle (Galeopsis Tetrahif), vetches (Viad), and species of clover (Trifolium), as well as ferns and broad-leaved grasses of different sorts. 3. On drier and more sandy soils :— HeatheY or ling (Calluna vulgaris), bilberry or whortleberry (Vaccinium Myrtillus\ red whortleberry or cowberry (Vaccinium Vitis idea), whin, gorse, or furze (Ulex}, broom (Cytisus scoparius), greenweed (Genista), groundsel and ragwort (Senecio], io6 Studies in Forestry [CHAP. v. mullein (Verbascum), hawkweed (Hieracium), spurge (Euphorbia] , — these last-named genera occurring in various species, — and the narrow-leaved meadow grasses. The shrubs which occur most frequently on hills and valleys, especially when the soil is fresh, include the following : alder buckthorn (Rhamnus Frangula), blackthorn or sloe (Prunus sptnosa), hawthorn (Cratcegus oxyacantha), spindlewood (Euonymus europ&us), dogwood (Comus sanguined), barberry (Berberis vulgaris), holly (Ilex Aquifolium), honey- suckle (Lonicera Periclymenuwi), elderberry (Sambucus) ; on drier soil, juniper (Juniperus vulgaris}, and on sandy soil, sea-buckthorn (Hippophae rhamnoides). Relation to warmth is exhibited in changes of soil-tempera- ture in accordance with changes in the atmospheric tempera- ture. It is determined to a far greater extent by the quantity of moisture in the soil, and by its colour, than by its specific warmth. Retentive soils, like clay, are cold and inactive ; but, when once heated, they only cool down again gradually. Sandy and gravelly soils become easily warmed and stimulated ; but they cool down again rapidly, and hence, in damp localities, increase the danger from frost. In Britain diurnal variations of temperature are obliterated at a depth of about 20 inches from the surface, weekly differences at about 40 inches, and monthly variations at about 6J feet. Depth expresses the extent to which decomposition of the soil has taken place below the surface. The finest earth is to be found near the top-level, where the soil has been most exposed to the disintegrating effects of 'weathering'; the deeper one digs below the surface the larger will the stones and breccia be found, until at last a layer of subsoil is struck which is practically beyond the reach of the decomposing agents, and which may, or may not, be of different geological origin from the soil resting upon it. When decomposition has proceeded so far that the ground is easily penetrable by the root-system for a considerable distance below the surface, a soil is termed deep ; but when the decomposed and aerated layer of earth is only slight it is said to be shallow. CHAP. V.] Soil and Situation For trees forming a decided tap-root — like the Oak, Scots Pine, and Larch — depth of soil is of very great importance ; for, unless the root-systems can develop normally, the growth in height of the trees becomes prejudicially affected. But trees with only moderately deep root-systems, like Beech, Horn- beam, Silver and Douglas Firs, or even rather shallow-rooting kinds like Birch, Aspen, and Spruce, also thrive better on deep than on shallow soils, as these latter generally contain more equable supplies of soil-moisture, and larger stores of food- material in an easily available, soluble form. Deep soils are much less apt to dry up or to become too moist than shallow soils ; and the disadvantages of the latter are intensified when the subsoil happens to consist of horizontal layers of stiff clay or other impermeable strata, or of ferruginous deposits like moorpan or limonite. The following is the classification of soils as to depth adopted at the sylvicultural experimental stations throughout Germany : — Description of Soil. Depth. Nature of Wocdland Crops for which such Depth suffices. Very shallow . up to 6 in. only . Not really sufficient for any species ; but often found under mixed coppice. Shallow . . from 6 in. to I ft. Spruce, Aspen, Rowan, Birch, Mountain Pine. Medium . . „ i to 2 ft. . Austrian, Corsican, and Wey- mouth Pines, Beech, Horn- beam, Alder. Deep . . . „ 2 to 4 ft. . Elm, Maple, Sycamore, Ash, Lime, Sweet Chestnut, Silver and Douglas Firs, Scots Pine. Very deep . . over 4 ft. ... Oak and Larch. But in Britain, as a matter of fact, woodland soils will seldom be found of great depth : for, when deep, they can generally be used to better economic and financial advantage as arable or pasture land. io8 Studies in Forestry [CHAP. v. IV. Situation in Relation to Woodland Growth. The growth and the regeneration of the different kinds of forest trees are dependent on combinations of various con- ditions regarding temperature and moisture, which are united under the term climate. Some demand for their normal development an amount of warmth which is absolutely fatal to others ; an4 these again can bear, and often even prefer, a low temperature during winter, which causes the vital energy of the former to cease, never to re-awaken. Some transpire so freely through the foliage (e.g. Spruce) as to need rather a damp soil and atmosphere, whilst others (e. g. Scots Pine) prefer a drier condition. Without light and warmth the action of chlorophyll in absorbing carbonic acid from the air, and consequently assimilation, would be impossible. Warmth is in general dependent on, and inversely propor- tional to, the distance of any locality from the equatorial line, although practically the nature of modifying circumstances connected with the distribution of land and water, high moun- tain-chains, &c., is always of more or less influence. Thus, in Britain, owing to our insular climate, and to the humid and essentially equalizing tendency of the Gulf-stream, we have no such extremes of summer heat and wintry cold as annually occur in the continental areas lying along the same degrees of latitude in Europe, Asia, or America. Owing to these local modifying influences, there are nowhere hard and fast zones of woodland crops. With ascent above the sea-level, and conse- quently above the densest and heaviest layers of atmosphere capable of acquiring most warmth in summer, temperature falls at about the rate of i° Fahr. for every 300 ft., and Angot has estimated that for every 333 ft. in vertical ascent woodland growth is retarded for about fourteen days in the awakening of vegetative activity during the spring. Recent investigations made in the Bavarian Alps (Brenner Pass, 4,500 to 5,000 feet above sea- level) have led to the following conclusions CHAP, v.] Soil and Situation 109 with regard to the effect of vertical elevation on the increment and the shape of forest trees * : — A. For individual Trees. 1. Growth in height diminishes regularly and noticeably. 2. Growth in basal area, or sectional area of the stem at breast- height, does not diminish so rapidly as growth in height. 3. Total increment diminishes gradually. 4. The period of development is prolonged in all of the above three directions (i. e. the attainment of maturity is slower). 5. The bole or stem deviates more and more from the shape of the cylinder and approximates towards that of the neiloid. 6. The distribution of the increment over the various portions of the tree increases relatively from above downwards. 7. The form-factor at breast-height (i. e. the proportion which the actual volume of the stem bears to a cylinder having the same base) becomes smaller. 8. The coronal development gradually comes lower down, nearer to the ground (i. e. the stems become short and stunted). 9. The proportion of branches and brushwood increases (i. e. as the stems grow stunted, the coronal development increases rela- tively). B. For whole Crops. 1. The number of stems per acre increases, but the proportion of those which form the larger girth-classes diminishes. 2. The mean average height of the crops diminishes. 3. The total basal area at breast-height does not diminish so perceptibly as the average height of the crops, but it is made up mostly by units belonging to the smaller classes of stems. 4. The total quantity of wood available as timber or fuel decreases perceptibly ; hence the total average annual increment of the mature crop becomes considerably less. 5. The quantity of small branches and brushwood increases. 6. There is a decided tendency towards growth of the trees in groups instead of being equally distributed over the whole area. Near the polar regions, or at very high elevations, there is no woodland growth. This may not be solely due to the actual 1 S. Honda, Ueber den Einfluss der Hbhenlage der Gebirge auf die Verdnderung des Zuivachses der Waldbaume, 1892, p. 27. no Studies in Forestry [CHAP. v. amount of cold in winter. It may, as Hartig has shown \ be caused by transpiration being excited through the leaves of the evergreen conifers (which reach to the highest latitudes and elevations) on bright, sunny days, whilst the soil still remains frost-bound and unable to allow of imbibition of fresh supplies of moisture by the root-system in order to replace what is being evaporated. Wilting and death are then the inevitable results if the winters are long and dry, and if the sunny days have been frequent. But, although woody plants suffer comparatively little from the effects of winter cold, yet late frosts in spring are apt to injure the young leaves and shoots, and also early frosts in autumn before the shoots have hardened. These dangers are greater in low-lying and confined localities than where aerial currents have free play. Ash, Acacia, sweet Chestnut, and Beech are most sensitive to frost ; Lime, Hornbeam, Elm, Birch, Larch, Aspen, Austrian, Corsican, and Scots Pines are decidedly hardy ; whilst Oak, Silver and Douglas Firs, Maple, Sycamore, Spruce and Alder occupy an intermediate position, in which the influence of other factors than atmospheric tem- perature merely (e.g. humidity of soil and air) determine whether they are likely to incur danger or not. The absolute equivalent of heat necessary for the normal development of any given species of tree is as yet unknown. But experience shows 2 that Elm, sweet Chestnut, pedunculate Oak, and Black Pines require the greatest amount of warmth, and that Larch, Cembran, and Mountain Pines can do with least ; whilst, between these extremes, Silver and Douglas Firs, Beech, sessile Oak, Scots and Weymouth Pines require de- cidedly more than Maple, Sycamore, Ash, Alder, Birch, and Spruce. Although their general requirements as to warmth limit the different species to more or less normal zones of 1 Lehrbuch der Baumkrankheiten, 2nd edit. 1889, pp. 104, 261. But compare the remarks already made on p. 68. a Gayer, op. cit., p. 20. CHAP, v.] Soil and Situation 1 1 1 elevation, yet quality of the soil, aspect, and local climatic conditions modify these demands in the most marked degree. It is more particularly the amount of warmth during the period of active vegetation which determines whether or not the different species of trees can thrive and regenerate themselves naturally in any given locality. If, between the time of their flowering and the natural term of their ripening the fruit, there has not been a sufficient development of warmth, accompanied by an absence of destructive frost, to enable the seed to attain maturity and germinative capacity, then the natural conditions for thriving and regeneration are not offered to any given kind of tree. The further northwards deciduous broad-leaved trees occur, the later is usually the time at which they break into leaf, as the amount of warmth requisite for stimulating active vegetation is only obtainable later in spring than at similar elevations situated further southwards. Light is also a factor which is undoubtedly of immense importance with regard to the thriving of woodland crops. A careful study of their demands with respect to light, and their capacity for enduring shade, will quite logically explain many of the concrete conditions in which woodland growth exhibits itself, as was first pointed out by Gustav Heyer1 (see also P- 54)- The Relative Humidity of the atmosphere is governed by the atmospheric temperature ; for, as regards any given quantity of moisture, the saturation-point will be much sooner reached when the air has only a low temperature, than when its temperature is high2. But, whilst the absolute humidity of the air varies inversely to the latitude above the equator, no such rule obtains regarding its relative humidity, as local circumstances determine the supplies of moisture available for evaporation. Thus, in Britain, the soft, mild, westerly winds which reach this island only after sweeping over the Atlantic 1 Das Verhalten der Waldbaume gegen Licht und Schatten, 1852. 2 See Roscoe's Elementary Text-book of Chemistry, 1888, pp. 55, 56. ii2 Studies in Forestry [CHAP. v. in the track of the Gulf-stream, have a high relative humidity ; whilst those from the east, which come from about the central area of Asia and Europe, are comparatively dry, although (in consequence of the moisture acquired in passing over the North Sea) not so dry as on the continent, where the relative humidity of the air decreases with longitudinal progress east- wards. As aqueous precipitations must occur whenever the air is reduced so far in temperature that the corresponding saturation- point renders it impossible for all the moisture to be retained, rainfall is more frequent at higher elevations than at lower levels, whilst at the same time aerial disturbances of various kinds are also more frequent and violent. For the maintenance of normal transpiration through the foliage of woodland crops enormous supplies of moisture are requisite in the soil. When a period of drought occasionally sets in during summer for about a fortnight to three weeks, this often forces vegetation to close its activity for the year in the case of broad-leaved trees, or can even be fatal to species like the Spruce, which transpire freely1. Though the actual amounts of soil-moisture requisite for the various species of trees of woodland growth are -not accurately known, yet observation and experience show that Spruce, Black Pines, Alder, Maple, Sycamore, and Ash thrive best in a humid atmosphere, whilst Beech, Birch, and Silver Fir grow better in damp than in dry localities. If, therefore, the former species be planted out in situations where the air is usually dry, they make considerably greater demands as to soil-moisture than when growing in localities where, owing to a higher relative humidity of the atmosphere, the transpiration of water through the foliage is not so much stimulated 2. The Aspect, or Exposure towards one or other of the cardinal points of the compass, exerts great influence on the 1 Compare Chapter VIII, Section i. 2 See British Forest Trees > 1893, pp. 27, 28. CHAP, v.] Soil and Situation 113 temperature of soils, and on the amount of moisture retained in them. Southern and south-western aspects, owing to their greater warmth and to the stimulation of evaporation, both " through the foliage and direct from the surface-soil, are usually much drier and more apt to get heated than northern and north-eastern exposures, which are cooler and damper, and whose soil is usually less active both in awakening vegetation in spring, in stimulating to assimilative processes, and in decomposing the dead foliage on the ground so as to form humus. On high ranges of mountains, however, trees will still be found on the warmer aspects at levels above those limiting their growth on the northern slopes. Eastern exposures are most liable to danger from late frosts; whilst western and south-western aspects are most exposed to damage from wind- fall and breakage, as the heavy storms coming from these directions are usually accompanied by rain, and often occur at times when the soil is still sodden from recent downpours. The Slope or Gradient of any soil is necessarily of influ- ence; for the opportunities which rainwater has of percolating / down to the lower layers decreases as the angle formed with the horizontal by the surface of the soil increases. According to Grebe, soils with a slope of from 5 to 30° form the true home of woodland growth; hence much land which is too steep for agricultural cultivation is well adapted for sylvi- cultural occupation. Grebe's classification of gradients, now adopted at the experimental stations throughout Germany, is as follows: — gentle 5-10° steep 21-30° medium 11-20° very steep 3I~450 precipitous over 45° ; this is, however, incapable of sustaining tree- growth. The Configuration of the Soil and of the surrounding Country exerts a considerable amount of influence on the woodlands. The soil near the base of hills is generally deeper, / richer, and more productive than on the slopes or ridges ; but i 1 14 Studies in Forestry [CHAP. v. the danger from frosts is greater in hollows and throughout low-lying tracts than where currents of air have free play. Mountain masses have greater uniformity of soil and situation than ranges of hills. On these the well-being of the woodland growth depends to a great extent on the amount of protection that can be given to it from winds ; for the bad effects of want of protection may only too clearly be seen in exposed planta- tions or woods near the sea-coast or on bleak hill-sides. In the assessment of the quality of soil the best standard is that which makes five distinctions, thus : — I. Very good ; II. good; III. average or moderate; IV. inferior; V. poor. In Germany the decimal system is often adopted. But practical men will have less difficulty in making up their minds as to whether any given soil is average or inferior in quality, than they will find in estimating it at 0*3, or 0*4, or 0*5 of the first-class soil classed as equivalent to i 'o. Such assessments are very useful, but are in each case only relative ; for a soil that might only be regarded as inferior so far as the cultivation of mixed crops of Oak, Maple, Sycamore, Larch, Douglas Fir, and Beech are concerned, might perhaps be considered a moderately good, or even a good soil if considered with regard to woods in which Pines, Spruces, and Firs were to be the ruling kinds of trees. CHAPTER VI ON THE ADVANTAGES OF MIXED TIMBER-CROPS OVER PURE WOODS AT p. 33 of the Nineteenth Century for July, 1 891, Sir Herbert Maxwell, Bart., in his article on Woodlands, in endeavouring to assist landowners towards a better system of Forestry than at present exists throughout Britain, makes a statement that the general bad growth of our forest trees as timber trees is attribut- able to the fact that — 'Mixed planting is generally practised, in sharp contrast to what Continental foresters call " pure forest " — that is, a woodland composed of one species of tree. This is in itself a hindrance to profitable manage- ment, because pure forest is much more easily tended than mixed planta- tion, and the timber is more readily marketable.' In England we are not accustomed to look upon the French as a particularly practical nation ; but, in regard to the treatment of their great forests, with which 17-7 % of the total area of France is clothed, it must be admitted that, although the methods adopted are not quite so scientific as in Germany, they are generally of a very high standard and thoroughly practical. Now in France, where sylviculture is well understood and practised, mixed forests form the great bulk of the woodlands, as, according to the last statistics available (Mathieu's, for I 2 n6 Studies in Forestry [CHAP. vi. 1876) these formed more than 70 % of the total wooded area, as exhibited in the following data ] : — Mixed forests of — Broad-leaved trees 50-3 % of total wooded area. Broad-leaved trees and Conifers 17-6 % ,, ,, Conifers 2-5% „ „ Pure forests of — Various species of Trees 26-7 % „ „ Data for Germany are not available. The imperial statistics for 1884 only showed 65 % of the total forest area (which aggre- gates 26 % of the empire) as covered by coniferous crops, whilst 34'5 % were clothed with broad-leaved species ; but the area of mixed forests was not computed. In sharp contrast to Sir Herbert Maxwell's dictum, is the following matured opinion of the most celebrated of living sylviculturists, Prof. Gayer of Munich 2 : — * We may say, in general, that the leading principle in the rational and economic treatment of woods must be less in the direction of pure than of mixed crops, and that the degree to which, and manner in which, mixed Woods occur throughout any system of management must be considered as the best test and standard by which one can estimate the knowledge and the capacity of those to whom are entrusted the duties of obtaining the best possible results from any given conditions as to soil and situation.' And, to prove that this is no mere new nostrum of these latest days, it may be permitted to quote the late Prof. Grebe of Eisenach, formerly Director of the Saxon forests in Thuringia, who wrote as follows in 1867 3 : — 'The more recent tendency of forestry is — and with full justification — towards the formation of high timber forests containing a suitable mixture of different species of trees, thereby duly acknowledging the manifold advantages to be gained with respect to increased outturn, more valuable assortments of timber, greater general security, and greater power of resisting inimical influences.' 1 Gayer, Der gemischte Wald, 1886, p. 9. 2 Der Waldbau, 3rd edit., 1889, p. 178. 3 Die Betriebs- und Ertragsregelung der Forste, 1867, p. 151 (2nd edit., 1879). See also Preface to the author's British Forest Trees, 1893. CHAP, vi.] Advantages of Mixed Woods 1 1 7 As arboriculturists we have nothing to learn from con- tinental nations ; but as sylviculturists we may learn a very great deal indeed. There is a need for the dissemination of sound knowledge, in the first instance regarding the proper density at which sowings and plantations should be made, and in the second instance as to that which should be maintained afterwards at all the various stages of their development. Sir Herbert Maxwell attributes the formation of mixed woods in great measure to neglect in cutting out the nurses originally planted for the purpose of stimulating the crops to quicker growth and of keeping down weeds. He says — and the statement is undoubtedly a true indictment of neglect and incapacity in those charged with the supervision of woodlands : — ' Want of system leads to irregularity in thinning out the nurses, which often remain to compete with what was intended to be the per- manent wood, and the result is a mixed plantation.' As will be pointed out in another chapter (see p. 183), such nurses should be removed during the weedings and clearings of the young woods ; whilst, if for any reason they have been allowed to stand till thinnings commence, an opportunity is then still given to remove them gradually. It would, however, hardly be rational to set up these mis- managed woods — admittedly the outcome of neglected tending operations, and not at all in conformity with the intentions or wishes of the proprietor — on anything like the same platform as mixed woods formed after deliberate consideration as to the best kinds of trees suited for each portion of the soil to be utilized under woodland crops. But, where mixed woods, are formed by capable foresters, they have, in comparison with pure forests, the great advantages of denser growth, larger and finer production of timber both as regards quantity and technical quality, comparative immunity from throwing or breakage by wind, snow, or ice, as well as from dangers arising from insects, fungoid diseases, and fire ; whilst against all these very solid advantages only one drawback can be named, — that the u8 Studies in Forestry [CHAP. vi. tending of such mixed woods is much more difficult, and that their proper formation and management require considerably greater knowledge of sylviculture than is requisite for the treatment of pure forests. In comparing the advantages and disadvantages of mixed woods, relative to pure crops, the following matters are worthy of consideration : — Advantages — 1. A greater density of crop is obtainable. 2. The soil is maintained in better condition as to pro- ductive capacity than under many pure crops. 3. A larger percentage of the outturn is available as timber for the higher technical purposes, at any rate in mixed crops of broad-leaved species of trees. 4. Demands of varying nature for timber can more easily be supplied. 5. It is easier to modify or transform the crop at any one time so as to meet the present or the probable future require- ments of the market. 6. Experience has shown that mixed crops are much less exposed than pure forests to dangers from external causes whether of organic or inorganic origin. 7. Natural regeneration of mixed woods is on the whole easier than with pure crops. 8. By concentration of various species in one series of crops the operations of tending, harvesting, &c., can be carried out most economically. Disadvantages are summed up by Gayer in the following words * : — 'It is easy to understand that mixed crops make higher demands on the capacity of the sylviculturist, as it is much more troublesome and difficult to give proper care and attention to each of several species in 1 Waldbau, p. 216. CHAP, vi.] Advantages of Mixed Woods 119 a mixed crop than to look after one species only; but when weighed against the many solid advantages offered by mixed crops, this drawback can surely seldom be seriously taken into account.' Mixed woods are such as are formed by two or more species, of which the matrix or ruling species should be one that is capable of safeguarding and retaining the productive capacity of the soil against insolation and the exhausting action of winds. The subordinate or dependent species of trees may be admixed with the ruling species either in clumps or hursts \ in groups or clusters, in patches or knots, in rows or fines, or merely scattered about singly as individuals. In mixed woods, wherever natural regeneration is permitted to the fullest extent, there will be a tendency for genera of trees with heavy seeds (Oak, Beech, and among Conifers the Silver Fir) to reproduce themselves in clumps on the patches of soil best suited to them ; whilst trees with lighter and often winged seeds (like Birch, Aspen, and Willow) will have a much greater repro- ductive power of asserting themselves individually and in small knots at some distance from the parent trees. i. A greater Density of Crop is obtainable. — Wherever the area under woodlands is of any considerable extent there are almost certain to be many variations of soil and situation with regard to the nature and the depth of the earth, its degree of moisture, its aspect, &c. ; and the best, most complete, and most economical utilization of the soil can only be expected when each such varying portion is stocked with the species of tree best suited for growing there. For, when thus growing in admixture on the patches of soil most suitable to their natural requirements, it will be found that the various species of trees do not thin themselves so soon as they otherwise must on soils less favourable to their natural development and requirements. And, by thus maintaining close canopy for the longest possible period, they not only avail themselves more fully of the pro- 1 The older term Bosc, often referred to by Manwood (History of the Forest Laws), is now obsolete. I2o Studies in Forestry [CHAP. vi. ductive capacity of the soil, but also conserve this in a higher degree than could otherwise be the case ; whilst, at the same time, they are able to utilize to the utmost possible extent the chemical power of the light requisite for the due performance of the assimilative functions by the foliage. This closer canopy and greater density of crop generally become of all the more importance as the crops advance in age, and begin to approach maturity ; hence in this prolonged maintenance of canopy lies the principal value of many kinds of mixed crops. 2. The Soil is maintained in better Condition and Productive Capacity than is the case under many kinds of Pure Crops. Pure woods of thinly-foliaged and light-demanding genera of trees, like Oak, Ash, Maple, Larch, and Pine, when once they have completed their chief growth in height and have begun to exhibit their natural specific tendencies with regard to increase of growing-space, are unable to conserve for themselves the general quality and productive capacity of the soil in conse- quence of the interruption of canopy, the decrease in the number of stems forming the crop, and the subsequent bad effects to the surface-soil wrought by insolation and exhausting winds. Hence the expenses of underplanting are usually un- avoidable. But as, during the earlier periods of development, these light-demanding genera are at the same time of more rapid growth than the shade-bearing kinds, Beech, Spruces, Silver Firs, and Hornbeam, in mixed crops they can, with now and again a little assistance in the way of tending wherever necessary, usually assert themselves as the predominating poles and trees, thereby acquiring just the position naturally best suited for their present growth and good future development. At the same time the shade-bearing genera, forming the dominant and more or less dominated classes of the crop, mechanically protect the soil against the exhausting and deteriorating in- fluences of sun and wind ; whilst, by their richer fall of leaves, they contribute valuable material for the formation of humus or mould, that natural manure of woodlands, which exerts very CHAP, vi.] Advantages of Mixed Woods 121 beneficial influence in enhancing the productive capacity of most classes of woodland soil. Pure forests make constant demands of one unvarying sort ^ on the land, so that on soils of merely average quality there is far greater risk of one particular class of nutrients being rapidly diminished and being less readily available than when a variety of species of trees induces a more general demand for the various different kinds of mineral food-substances. Thus, whilst in general the chemical composition of dry woody- substance of the different kinds of timber is, in round figures, approximately constant as follows l : — 50 % Carbon, 42 % Oxygen, 6 % Hydrogen, i % Nitrogen, and i % Ash (or mineral residuum), yet the nature of the substances found in the ash varies greatly in the different species of trees. Thus, with regard to lime, the principal constituent in the ash, there are 3-5 times as much found in Oak, and 2-3 times as much in Beech, as in the Scots Pine, which, however, exhibits more than Birch. Taking the quantity contained in Scots Pine as unity, then the amount of potash requisite is about 5 times greater in Beech, 3! times greater in Oak, 2\ times greater in Silver Fir, twice as much in Larch and Birch, and about if times as much in Spruce. And again, with regard to Phosphoric Acid, the wood of Beech contains in its ash about 2j times as much as Scots Pine, Oak 3 times as much, Birch twice as much, Larch and Silver Fir i^ times as much, whilst Spruce contains considerably less. There can be little doubt that the theory enunciated by Georg Ludwig Hartig, the father of Dr. Theodor Hartig, and grandfather of Prof. Robert Hartig (of Munich), that the soil can be most thoroughly utilized by an admixture of shallow- \/ rooting species with deep-rooting, in order that each may draw 1 Weber, Die Aufgaben der Forstwirthschaft (Lorey's Handbuch, &c.), 1886, vol. i. pp. 72 and 62. More accurate details have already been given in Chapter IV. pp. 82-85. 12,2 Studies in Forestry [CHAP. vi. its main supplies of nutriment from a different layer of soil — although long scoffed at by a certain class of sylviculturists (headed by Hundeshagen), who saw the advisability of admix- ture explained solely by the relation of the various species towards light and shade — is based on a principle equally sound from the theoretical and the practical points of view ; for it is a fact that, in the majority of mixtures acknowledged to be good, the root-systems of the different species vary considerably in depth. That, in addition to greater density of growth, which has already been referred to in the previous section, the productive capacity of the soil is at the same time more thoroughly utilized can be proved, if requisite, by actual crop measurements made in Silesia in 1880. These showed that, on soil similar as to conditions and quality, the average annual increment in eighty-year-old crops was : — Cubic ft. per acre. Pure forest of Scots Pine 18-3 Pure forest of Spruce 19-9 Mixed forest of Scots Pine, Spruce, and Silver Fir . 23-5 But, beneficial though the influence of the overshadowing of the soil by the leaf-canopy undoubtedly be, there are occasions on which even it may perhaps be carried farther than is de- sirable or advantageous ; as, for example, in dense woods of pure Spruce or Silver Fir, where the close, thickly-foliaged canopy overhead, and the deep sponge-like growth of moss covering the soil, intercept and retain a very much larger pro- portion of the atmospheric precipitations, both in winter and in summer, than deciduous trees or other coniferous species (Pines) with somewhat thinner growth. For whilst, of all the precipitations in the course of the year, on the average about 25 % are intercepted by the foliage and branches, and 75 % reach the soil in woodlands, these data vary considerably according to the kind of tree forming the crop. The averages CHAP, vi.] ^Advantages of Mixed Woods 123 of long-continued observations in Switzerland, Prussia and Bavaria gave the following results l : — Species of Tree. Percentage of total Atmospheric Precipitations reaching the soil. intercepted by, and evaporated from, the foliage and branches. Deciduous Larch . . Beech . . 85 81 '5 19 Evergreen Spruce . . Scots Pine 76 70 24 3° And of the moisture reaching the soil, Weber calculated that — leaving out of account the transpiration of the foliage for which the supplies of moisture are withdrawn by the roots from deeper layers of soil — its disposal was as follows : — Woods. Amount evaporated. Remained in the soil. Beech .... Spruce .... Scots Pine . . . per cent. 40-4 45-3 41.8 per cent. 59-6 54-7 58.2 Owing to the smaller percentage of precipitations reaching the ground, to the larger evaporation from the soil-covering, and to the strongly hygroscopic nature of the moss, we can easily understand the dried-up appearance that soils under pure Spruce woods sometimes assume in early summer, just at the time when transpiration is becoming most active, and when the greatest necessity exists for a free supply of moisture from the soil so as to permit of the assimilative and productive processes going on to their fullest possible extent. In former times, when the work of nature was comparatively uninterfered with, mixed woods almost everywhere formed the 1 Compiled from data given by Weber, op. cit., pp. 47-49- 124 Studies in Forestry [CHAP. vi. covering of the uplands, and the hilly tracts, and stretches not yet required for arable land or pasturage. Rain and snow were then more equably precipitated over the soil itself, and were not so apt to be sucked up and retained by a strongly hygro- scopic surface-growth of weeds and mosses, which likewise is exceedingly active in afterwards utilizing and exhausting the supplies of moisture contained in the upper layer of the soil. The aqueous precipitations were, on the other hand, preserved by a good layer of dead foliage and of the humus or mould resulting from their decomposition, and could thus percolate normally into the soil downwards towards the subsoil, so as to maintain a tolerably equable distribution throughout the whole, owing to the effects of gravity being counterbalanced by capillarity. Whilst Boussingault has shown in France that, with increase in the area stocked with conifers, a gradual local sinking of the water-level below the soil has taken place, practical sylvi- cultural experience in Germany has also shown that— except at high elevations with humid climate — extensive plantations of pure Spruce rapidly lead to a marked decrease in the quantity of soil-moisture. And Runnebaum's comparative investigations in 1885 showed that in mixed woods of Scots Pine with Beech the conditions relative to soil-moisture were more favourable for tree-growth than in pure forests of Pine. It is, however, only right to point out that this must to a certain degree be ascribed to the influence exerted on the soil by the good humus or mould formed by the dead foliage of the Beech. 3. A larger percentage of Timber is available for the higher technical purposes^ at any rate in mixed crops of broad-leaved genera of trees. Many of our more valuable kinds of timber trees are, when once they have passed through the initial stage of pole-forest, so light-demanding, and so dependent on increase of growing-space for the continuation of vigorous growth and further normal development, that they are unable to maintain CHAP, vi.] Advantages of Mixed Woods 1 25 for themselves such degree of density of canopy as is requisite for the due conservation of the productive capacity of the soil, and for the prevention of its gradual, but inevitable, deterioration. Even on the better classes of soil, pure crops or mixed woods of valuable light-demanding species only — Oak, Ash, Maple, Larch, Pine, &c. — grown without admixture of any shade- bearing species, are apt to thin themselves out naturally at so rapid a rate as to favour branch and coronal development to an extent inconsistent with a studiously economical utilization of the woodland soil. This, too, is a drawback not in any way obviated by underplanting. But an admixture of one or other of the shade-bearing species (Beech, Hornbeam, Spruces, Silver Firs), according to the nature of the soil and situation, not only protects and stimulates the productive capacity of the soil, but at the same time acts mechanically in stimulating to growth in height, and in preventing the formation of short boles and of stout branches that would prejudice the technical utility and the market value of the timber produced. It is a matter of practical experience, needing no discussion, that Larch and Scots Pine form more valuable boles, and contain a larger percentage of heart-wood, when grown in admixture with Spruce or Silver Fir than as pure crops. And all the more valuable species of deciduous trees gain in shape, increment, and age up to which they may be advan- tageously grown from technical and financial points of view, when the Beech, or on moister descriptions of soil, the Horn-beam, forms a part of the crop. But these beneficial effects are even more distinctly noticeable when mixed crops are formed, on suitable soils, of conifers and broad-leaved trees — even when all are shade-bearing, as in the case of Spruce and Silver Fir forming crops along with Beech. In consequence of the greater increase in the total quantity of timber produced in mixed crops as compared with pure woods, and of the more favourable circumstances affecting the forma- 126 Studies in Forestry [CHAP. vi. tion of long, full-wooded, clean stems with comparative freedom from knots and branches, the timber produced attains its highest possible technical and financial value. And owing to the tendency towards confinement of the crown to the upper part of the tree only, to which these favourable results are practically due, a considerable portion of the upper wood is comprised within the bole that must otherwise have been dissipated in the formation of branches of comparatively little technical or monetary value. By concentrating the energy of growth in good bole-formation, the actual cubic content of the stem is not only increased, but also its value per cubic foot, as this rises with the length, straightness, and freedom from flaws occasioned by knots and branches. 4. Demands of varying nature for Timber can more easily be satisfied. This statement may almost be said to be of an axiomatic nature. It plainly stands to reason that, where several species of trees are grown together on the same area, the classes of material periodically yielded during the necessary operations of tending, thinning, and removal of diseased or already mature individual stems, must offer a considerably greater variety to the different classes of local consumers than is possible in the case of pure forests. And the same holds good when the period comes for the harvesting of the mature crop. At the same time that variations in the local demands can be more easily satisfied, the wider, more general, and more important requirements of timber marts at some distance can also be better met by mixed than by pure forests ; whilst there is less danger of the over-production of any one kind or assortment of timber to any such extent as might possibly glut the market and cause a sudden fall in the prices obtainable. 5. // is easier to modify or transform the Crop at any. time so as to meet the present or the probable future requirements of the market. Of the necessity for such considerations no better example can be given than is shown in the Crown Oak woods of the New Forest, Alice Holt, Parkhurst, and the Forest of CHAP, vi.] Advantages of Mixed Woods 1 27 Dean, which were planted up for the purpose of supplying Oak timber for the use of our navy. But now all our ships of war, and the best classes of liners, are constructed almost entirely of iron or steel and of Teak timber from Burma. Teak — in place of corroding iron with which it comes in contact, as Oak does owing to its tannic acid — is, through an essential oil contained in it, preservative of the steel screws, bolts, &c. But notwithstanding the present extensive and ever-increasing use of substitutes like iron in place of timber, and the vast improvements in communication — by means of which the forest produce of far-distant countries can be brought to build the navies of Europe, and even to pave the streets of London — timber is, along with gold, almost the only com- modity which has not during the past half century depreciated in relative exchangeable value with most other articles of com- merce. All classes of timber do not, however, command equally favourable market quotations. But the sagacious sylviculturist will easily know from a study of selling prices, of the stocks of timber held at the chief marts, and of the reports as to the probable quantity and the quality of imports from abroad, what kinds and classes of timber are most likely to be re- munerative in the immediate future. And it is self-apparent that he will be in a far better position to tend and foster those species which hold out the fairest financial promise, when several kinds of trees are growing together in mixed woods, than when each species forms a pure forest worked quite independently of the other crops. Mention has above been made of the Oak woods planted by the Crown for the future supply of navy timber, which is not now required. As crooks were formerly an essential before the framework of hulls was made of iron or steel, the most economical method of producing them was to grow the Oaks as standards enjoying as full supplies of light and air as possible. But, under ordinary circumstances, the most economical manner of growing Oak timber for general technical purposes (requiring 128 Studies in Forestry [CHAP. vi. length and full-woodedness of bole, straightness, and freedom from knots or twists), and for the highest possible financial returns, is undoubtedly to confine the individual stems within the least growing-space sufficing for their actual requirements as to light, warmth, and the normal activity of their assimilative organs, until the main growth in height has been completed, and until natural demands for freer exposure to light and air, and greater lateral expansion of the crown of foliage, can no longer profitably remain unheeded. Crops, however, which have been originally formed and treated with the express view of yielding crooked stems, cannot be forced later on to form fine, straight, clean boles showing a minimum of tendency to tapering growth near the top-end. Such existing crops must first be cleared and regenerated before others can be formed and produced with the express intention of utilizing the productive capacity of the soil in the fullest and most economical manner. And, on the other hand, whenever present market rates offer inducements for the speedy clearance and sale of certain classes of timber, advantage can much more easily and con- veniently be taken of the favourable opportunities of disposal without at the same time threatening the well-being of the woodlands by departing to a greater or less extent from the normal methods of treatment that may have been forecast by the provisions of the Working Plan. And a Working Plan must be the basis of all operations in any well-managed forests. In short, when the growing-stock consists of one series of falls of mixed woods, varying in age from zero to maturity, in place of having a similar series for each of the species of trees grown by themselves in pure crops, the Working Plan is capable of much greater elasticity of treatment. It affords larger scope for the somewhat premature utilization of portions of crops, whenever the market may be exceptionally favourable for that particular kind or assortment of timber, without necessarily exposing the soil to deteriorating influences likely to weaken CHAP, vi.] Advantages of Mixed Woods 129 its productive capacity. By removing or diminishing the number of individuals of other species during the ordinary operations of thinning and tending, or, if necessary, even in special revisions for this purpose, the probable immediate future requirements of the timber marts within reach can be more economically, conveniently, and speedily arranged for than when one has to deal with pure forests only. As an example of this the safety-match industry throughout Norway, Sweden, and Germany, may be instanced. The woods best suited for the requirements of this industry are Willows, Aspen, and Poplars ; and it very frequently occurs that the match-factories have to be removed from one district to another solely on account of the supplies of suitable timber falling off. The heavy expenses thus involved mean that if steps were taken to provide better supplies of these softwoods, the factory proprietors could well afford to pay higher rates to secure them. The full advantage of such favourable markets can only be derived when patches of moist soil have been utilized for the growth of these softwoods in mixed deciduous forests. 6. Experience has shown that Mixed Woods are much less exposed than Pure Forests to dangers from external causes, whether of organic or inorganic origin. Shallow-rooting species, like the Spruce in particular, when mixed with deeper-rooting kinds of trees, like Pine, Larch, and Silver Fir, are much less exposed to be damaged or thrown by storms than when grown in pure crops ; whilst conifers of all kinds suffer less damage from wind, fire, snow, ice, insects, or fungoid diseases, when grown in admixture with broad-leaved trees than if forming pure woods, or even mixed woods consisting of conifers only. If associated along with broad-leaved trees, conifers usually attain a better development than under any other circum- stances. This alone would partly account for the decreased liability to attacks from insect enemies ; whilst, at the same time, a much better check is kept on any tendency to increase K 130 Studies in Forestry [CHAP. vi. in the number of insects, as insectivorous birds are much more frequent where broad-leaved trees exist than in purely coniferous woods. But even where attacks of noxious insects take place in such mixed woods, they seldom become wide- spread over all species, and never necessitate the clearance of whole crops, as unfortunately sometimes happens in the case of Spruce and Scots Pine. Trees like the Oak, which are somewhat sensitive to late frosts in spring during the early period of their growth, are apt to suffer less damage whilst growing under the protection of hardier kinds of quicker development, like Birch and Scots Pine. And again, in mature mixed woods of conifers and broad-leaved species, the technical value of the boles is less likely to be diminished by frost-shakes than when these latter are grown by themselves. The woodland proprietors, of Scotland especially, know what ravages can be committed in pure Larch forests by the fungoid disease, due to Peziza Willkommii^ which causes a cankerous outbreak on the stems, and induces crooked growth. And in pure woods of Spruce, Silver Fir, and Scots Pine, red-rot and other fungoid diseases of the stem and the root-system, occasioned by Trametes radiriperda, T. pini, Aetidium elatinum, Peridermium pini, Agaricus melleus, &c., are often productive of very serious sylvicultural and financial results. Speaking of ' leaf-shedding] a disorder to which Scots Pine is liable at an early age — an infant ailment, due some- times to frost, or to the drying-up of the needles when stimulated to transpiration by bright sunshine in winter or early spring, whilst the soil is still frost-bound and unable to yield fresh supplies of moisture to replace that evaporated, but in many other cases undoubtedly occasioned by a fungus, Hysterium pinastri, — Gayer says * : — ' About thirty years ago the sporadic occurrence of " leaf-shedding " in Scots Pine was merely " an interesting observation" whereas now it is 1 Der gemischte Wald, 1885, p. 24. CHAP, vi.] Advantages of Mixed Woods 131 nothing short of a wide-spread calamity all over Germany. At first, two to four-year-old seedling growth was chiefly attacked, but nowadays sowings and plantations are both liable to be affected, and it is even be- ginning to attack young thickets. And wherewith shall we replace the Scots Pine, if even it refuse to serve our purposes ? R. Hartig says, at page 40 of his book on the Diseases of Trees l : — " the best prophylactic measure against the occurrence and spread of epidemics is the cultivation of mixed forest crops.1' ' A direct and fuller quotation may, however, also be per- mitted from Professor R. Hartig's celebrated work, in which the opening words of the Introduction are : — ' The transformation in the natural woods of Germany, the formation of pure, equal-aged crops of the same species of trees, instead of the composite mixed forests and copses made up of all sorts of trees of all ages, and especially the restriction of the broad-leaved species by the formation of pure crops of conifers, have during the present century, and most particularly in the last few decades, threatened the well-being of our woods to an extent which was formerly unknown. And it is chiefly the enemies belonging to the animal and vegetable kingdoms which find in the recent developments of our woodland economy the conditions favourable to their increase in enormous strength, so that the complaints made concerning larger and ever larger devastations, appear in no wise unfounded.' But it is perhaps more with regard to damage caused by injurious insects, than in any other way, that the beneficial effects of the formation of mixed crops may be judged of, so far as Spruce and Scots Pine are concerned. Simultaneously with the disappearance of the natural mixed crops, which can be proved to have formed the chief portion of the wooded areas throughout Germany during the first quarter of the present century, and with the formation of extensive pure forests of coniferous species, the damage done by insect enemies has increased enormously, and has on several occa- sions during the past half-century attained the dimensions of actual calamities, sometimes of national importance. Thus, referring to the ravages of the Black Arches, * Nun/ 1 Lehrbuch der Baumkrankheiten, 1882 (2nd edit. 1889, p. 55). K 2 132 Studies in Forestry [CHAP. vr. or Spruce moth (Liparis monacha) which — together with the bark-beetles (Bostrychini and ffylesinini) that followed it and attacked the stems left in a sickly condition of growth — between 1853-1862 devastated the coniferous forests of eastern Prussia and western Russia over about 7,000 geographical square miles, and necessitated the felling of over 420,000,000 cubic feet of timber, Hess recommends *, as the first measure of prevention, ' avoidance of the formation of pure forests of Spruce or Scots Pine ; formation of mixed crops of suitable species.1 This same insect has quite recently, in southern Bavaria and western Austria (1889-1891), necessitated the clearance of 40,000 acres, mostly of pure Spruce; and during 1892 an outlay of £75,000 was incurred solely in order to combat its further attacks in the State Forests of Bavaria alone 2. That the calamitous extent to which attacks by moths (Bombycidae\ bark-beetles (Scolytidae), and weevils (Curcu- lionidae] occur every now and again in Germany, arises from the want of natural admixture of different species is a fact which receives practical recognition in the endeavours now everywhere being made in order to effect a re-transformation to the former mixed state of the woodlands. As Gayer says 3 : — * Endeavours are in general being made to prepare the way for a return to mixed forests in all suitable localities. And that, face to face with the late fearful devastations (by insects) in the Spruce forests of southern Bavaria, these principles should be even more strongly insisted on, can easily be understood.' It is a well-known matter of experience that forests of broad- leaved species are not exposed in anything like the same degree to serious damage from insects. Even after crops may have been stripped of their spring flush of leaves — as sometimes 1 Der Forstschutz, vol. i., 1887, p. 355. a A detailed account of this moth and its ravages will be found in the Transactions of the Highland and Agricultural Society of Scotland, 1893, pp. 176-207. 3 Zeitschrift fur Forst- und Jagdwesen, 1892, p. 386. CHAP, vi.] Advantages of Mixed Woods 133 happens when swarms of caterpillars of the Processionary Moth ( Gastropacha processionea) defoliate the Oak, for instance — the injury is not of a permanent nature, owing to the much larger reserves of starchy matter accumulated by the broad-leaved kinds of trees, and the stronger reproductive and recuperative capacity with which they are consequently endowed. By admixture of broad-leaved genera, therefore, and parti- cularly of Beech or Hornbeam, along with conifers, the danger of attacks from insects can be greatly diminished without prejudicing the other advantages derivable from the formation of mixed crops. Thus Danckelmann states 1 that woods which consisted of four-fifths Scots Pine and one-fifth Beech or Hornbeam practically did not suffer at all in Prussia from any of the insect calamities caused by moths between 1860- 1880, whilst the pure woods of Pine suffered severely. The beneficial effect of mixed crops in obviating extensive injuries from insect enemies is perhaps almost the only point concerning which German sylviculturists are absolutely unani- mous. That such calamities as have from time to time occurred in different parts of Germany have not taken place similarly, though on a smaller scale, in any part of Britain is, most probably, solely due to the happy chance or the prudent sagacity of woodland proprietors imitating nature by the forma- tion of mixed woods rather than pure forest over areas of considerable extent. Experience on a large scale in Germany has shown that the number of dangerous insects is not only less in mixed than in pure crops, but also that at the same time the number of insectivorous birds is greater. Should Sir Herbert Maxwell's advice be extensively adopted, however, the days of such comparative immunity will almost to a cer- tainty be numbered. What is true about dangers from injurious insects, may also be repeated as to windfall and breakage from storms, and to damage wrought by accumulations of snow or ice on the 1 Zeitschrift fur Forst- und Jagdwesen, 1881, p. I. J 134 Studies in Forestry [CHAP. vi. crowns of trees. In these respects again, conifers suffer to a far greater extent than broad-leaved genera, among which Beech suffers more than Oak, Ash, Maples, or Elms. Of all forest trees Spruce is, owing to the shallowness of its root- system, most apt to become windfall ; whilst Scots Pine is, owing to the brittleness or low degree of elasticity of its branches, more apt to have its crown injured by violent winds or heavy accumulations of snow or ice. A year seldom goes past without the necessity of registering damage from one or other of these causes ; though, fortunately, destructive storms like the N.E. gale of November 17, 1893, in Scotland are rare. To prevent, so far as possible, damage from storms, Hess1 recommends the admixture of. deep-rooting species along with those which have shallow root-systems, and adds that — ' The injuries caused by storms during the last decades should be a warning to those sylviculturists who are over-eager to transform forests of broad-leaved trees into coniferous woods ; such transforma- tions should only take place when justified by extreme necessity,' as, for instance, when soils have become greatly deteriorated by faulty treatment. Accumulations of snow on the crowns of trees become diminished in mixed crops, especially when the conifers are inter- spersed with broad-leaved trees. Besides allowing the snow to reach the ground, the bare crowns of the latter afford some slight support to the snow-laden crowns of the former. Even when breakage results, it is then more of an individual nature, and does not extend throughout large patches, or over the whole of the crop as sometimes happens in Spruce and Pine woods. Here again Hess lays down 2, as the first sylvicultural measure to be taken for the prevention of damage from snow and ice : — 1 The avoidance of the formation of pure forests of species liable to suffer. Scots Pine is entirely out of place in such localities. So far as 1 Op. cit.t vol. ii., 1890, p. 287. 2 Op. cit., vol. ii. p. 315. CHAP, vi.] Advantages of Mixed Woods 135 possible, broad-leaved species of trees should be scattered, in sufficient quantity and at convenient distances, throughout Spruce woods.' That similar drawbacks are also incidental to the formation of too extensive pure crops of either cereals or roots in agricultural utilization of the soil, may be seen by a reference to Fream's Agriculture \ from which the following short extract may here be given : — ' In other words, side by side with the excessive, or exclusive, cultiva- tion of one kind of plant, the pests — whether insects or fungi — which prey upon that plant may be expected to become more abundant, for they find their victims literally crowded together, and therefore ex- tremely accessible.' 7. Natural Regeneration of Mixed Woods is on the whole easier than in the case of Pure Crops. This is but of minor importance compared with many of the other more substantial advantages offered by mixed crops. It is due to the special treatment and tending which must be bestowed on the crops in order that, so far as possible, each species may be placed in the natural conditions most favourable to its growth and further development. With some attention given towards securing for each kind of tree the soil and situation best adapted for it, a healthier growth, and a richer production of seed are natural results, owing to larger secretions of starchy reserves of surplus nourishment. Hence regeneration from seed in small groups and patches is comparatively easy, and is more likely to be successful than when one single species predominates over the whole woodland area notwithstanding the usually frequent changes with regard to the depth of soil and the quantity of soil- moisture. The species of tree which gains most in this way is again the Spruce, which cannot usually be regenerated under parent standards owing to danger of windfall ; but, when treated thus in mixed crops, it can be reproduced without the danger otherwise threatened to young seedling crops by weevils (Cur- culionidae\ The natural regeneration of the other great shade- 1 Elements of Agriculture, 4th edit. 1892, p. 333. 136 Studies in Forestry [CHAP. vr. bearing species, Beech, Hornbeam, and Silver Fir, offer in general but slight difficulty. In mixed crops these trees would usually be reproduced naturally and cleared away as soon as possible, thus leaving the young seedling crop to grow up as underwood under the light-demanding standards of other kinds of trees left to thicken into stems of fine marketable dimensions. In the regeneration of mixed woods it will be almost in- variably found advisable to plant out large transplants of the more valuable species of timber trees ; for their disposal through- out the soil-protecting, ruling species, and the advantage in age and development which it is desired to give them over it, are much better ensured by this than by any other means. But, at the same time, wherever special conditions of soil render the natural regeneration of the light-demanding species desir- able, this can also be effected : and any blanks that remain afterwards can easily be filled up with one or other of the shade-bearing and soil-protecting kinds of trees. 8. By Admixture of Various Kinds of trees in one series of Crops, the operations of tending, harvesting, &°, ioo „ 282 „ ii » I2° » 238 „ 4 1 Die Bctriebs- und Ertragsregelung der Forste, 1879, p. 300. 2 Gayer, Waldbau, 3rd edit. 1889, p. 15. 3 This only refers to natural reproduction and sowing ; it would of course be much less in the case of plantations. But compare with the above the remarks made on page 57. might be advantage- ously removed by thinning. i88 Studies in Forestry [CHAP. IX. In mixed forests the practice of thinning must, of course, be conducted on quite a different principle from that obtaining with regard to pure woods. Thus in order to save a valuable species of tree, it may very often be found necessary to cut out other kinds of more energetic growth, which may threaten to prejudice its development, or even to endanger its existence. As regards the influence which the species of tree has on the extent to which thinnings are necessary, Schuberg3 found in the Black Forest that in forty to eighty-year-old crops, which had been regularly thinned, the following were the results on soils of average quality : — Kind of Crop. Scots Pine. Spruce. Beech. Silver Fir. Average number of stems per acre 545 619 686 864 Absolute individual growing - space in square feet 80 70 63 5° Relative individual growing-space 100 87 ' 79 63 If the chief light-demanding genera (Pine, Larch, Oak, Ash, Maple, Birch, &c.) be grouped together, and be compared with the various shade-bearing kinds of trees, it will be found that on the whole these, latter only require on the average from 50 to 75 %, or one-half to three-quarters, of the growing-space demanded by the former for their proper development as a woodland crop. The quality of the soil is also a very important factor in deter- mining the number of stems per acre. Owing to the more 1 Gayer, op. tit., p. 550. CHAP, ix.] Tending of Woods 189 equal strength with which the individual struggle for supremacy is waged on soils of indifferent quality, the growing-space per stem is, up to the sixtieth to eightieth year, often considerably less than on better soils, although in the case of the Scots Pine this difference is less marked than in any other species. The practical lesson thereby conveyed is that, on soils just of or below the average in quality, both financial and purely sylvi- cultural considerations point to the advisability of stimulating, by means of early, oft-repeated, and moderate thinnings, the development of all individuals which it is desired to retain. Thin early, often, and moderately is the golden rule of tending woodlands. Anything approaching interruption of the canopy during the period of most active growth in height must of necessity lead to a further development of the crown at the expense of the length and cleanness of the bole ; and this will consequently tend towards a diminished technical and monetary value of the timber produced. Between the two extremes of overcrowding and of free individual growing-space there must be in every kind of crop a happy medial point or a normal density of canopy, at which the quantity and the quality of the crop attain their com- bined maximum. To show the practical effect which thinning has on the increment of the basal area of the individual stems left forming the crop, the following example may be given. In two different parts of an extensive forest three areas were selected on soil of similar nature and quality, and thinnings were carried out on equal areas in the following degrees : — I. Slight, only dead and dying poles being removed. II. Moderate, all suppressed poles being removed. III. Heavy, all dominated poles being removed. The conditions as to soil and situation were in each locality as similar as possible, the soil being a fresh, loamy sand throughout. The results of the experiment were tested five years after the thinnings took place. 190 Studies in Forestry [CHAP. IX, I. — In the first instance, that of a thirty-seven-year-old crop of Spruce, raised by planting, the data 1 were : — Previous to thinning: Area No. Nature of thinning. No. of stems per acre. Total Basal area, sq. ft. I. Slight .... 2,126 242 II. Moderate . . . 2,IOO 25J III. Heavy .... 2,044 234 During the thinning there were removed — Area No. Stems per acre. Basal area removed, sq. ft. Percentage of Basal area removed. I. 502 9 About 3f II. 822 28 „ XI III. 971 37 „ 16 In consequence of the thinning, the arithmetical mean diameter at breast-height (4^ ft.) of the stems that were left was found to be — On area I, 5-12 inches ; On area II, 5-68 inches; On area III, 5-84 inches; whilst five years later , just before another thinning was to take place, it was found to have increased — On area I to 5-48 inches, or an average diametral increment of 0-36 inches per stem. 1 These and the following data are, by permission, excerpted from Dr. M. Behringer's prize thesis Ueber den Einfluss wirthschafflicher Massregeln auf Zuwachsverhaltnisse ^lnd Rentabilitdt der Waldwirthschaft, 1891, pp. 19 et seq. CHAP. IX.] Tending of Woods 191 On area II to 6-16 inches, or an average diametral increment of 0-48 inches per stem. On area III to 6-40 inches, or an average diametral increment of 0-56 inches per stem. II. — In the other locality, a thirty-six-year-old Spruce wood, raised by sowing, the data were : — Previous to thinning: Area No. Nature of thinning. No of steins per acre. Total Basal area, sq. ft. I. Slight .... 7,707 2I9 II. Moderate . . . 7,725 235 III. Heavy .... 7,497 22O The operation of thinning removed — Area No. Stems per acre. Basal area removed, sq. ft. Percentage of Basal area removed. I. 4736 29 About 1 3 II. 5,6l9 53 „ 22 III. 5,9*5 71 32 when the arithmetical mean diameter at breast-height of the remaining stems was found to be — On area I, 3-44 inches ; On area II, 4-00 inches ; On area III, 4-20 inches ; and, just previous to another thinning five years later ^ it had risen — On area I to 3-88 inches, or an average diametral increment of 0-44 inches. 192 Studies in Forestry [CHAP. IX. On area II to 4-48 inches, or an average diametral increment of 0-48 inches. On area III to 4-72 inches, or an average diametral increment of 0-52 inches. The actual average increment in basal area was found to be per annum per acre — I. In the Plantation. II. In the Sowing. Area I. sq. ft. 6-6 Area. I. sq. ft. 8-9 » II. 7-7 >» II. 8-7 » III. 8-2 >? III. 8-2 Comparing the average annual increment with the total basal area at the middle of the period of five years, the percentage of annual basal increment was found to be — In the Plantation. In the Sowing. Area. I. per cent. 2-68 Area. I. per cent. 4-27 r» II. 3-22 >» II. 4-39 5> III. 3-85 >> III. 5.02 The obvious conclusions from these data seem to be that in plantations, in which from the very outset each individual plant has a fixed amount of growing-space, the natural process of selection proceeds so much more rapidly than otherwise that— I. There is less risk of any overcrowding of the leaf-canopy. II. Despite the smaller number of stems per acre, the total CHAP, ix.] Tending of Woods 193 basal area (i. e. the sum-total of all the stem-superficies at breast- height) is certainly not less than in dense crops raised from seed or by natural regeneration. III. A far less percentage of the total number of stems belongs to the dominated and suppressed classes. IV. The stimulation of the increment in basal area takes place in accordance with (though it is not necessarily propor- tional to) the degree to which the thinning takes place. So long, therefore, as thinning is not carried to such an extent as to prejudice the energy of growth in young crops that have not yet nearly completed their activity, i. e. which have not yet culminated in average annual increment, a free thinning stimulates to the earlier maturity of the crop, and is there- fore decidedly advantageous from a financial point of view. Thinnings are, generally speaking, said to be slight when only dead or dying poles are removed, moderate when all suppressed poles, and also a portion of the dominated poles, are cut out, and heavy when at the same time all the dominated poles are eliminated l. It may be noted here that, in tree-forest, a slight thinning removes about 5 % of the basal area of the stems at breast- height in crops of normal density of leaf-canopy, a moderate thinning about 10 %, and a heavy thinning about 15 %. Where it goes beyond this last degree, it becomes in reality a partial clearance, and must be regarded as such. The average percentage of basal increment has been given above ; but it must be observed that these figures are subject to modification. For the actual percentage of basal increment is 1 In the special case referred to on p. 64 the moderate thinning was particularly stated not to include any of the dominated stems, as these were all included in the heavy thinning. But it must be borne carefully in mind that the thinnings were carried out in dense crops of Spruce, which is one of the most shade-bearing kinds of trees. For crops of light- demanding trees, like Oak, Larch, Pines, Ash, Maple, Sycamore, Elm, Birch, Willow, and Poplar, even a moderate thinning would certainly remove a portion of the dominated individuals ; but the extent to which these should be cut out would, in each concrete case, depend on the kind of trees forming the crop, the general vigour of the latter, and the nature of the soil and situation. O 194 Studies in Forestry [CHAP. ix. greatest just immediately after the thinning takes place ; and it gradually decreases as the crowns close up again towards the termination of the period at which another thinning becomes necessary. The physiological explanation of this decrease is to be found in the fact that the assimilative functions of the lower foliage again become weakened through the gradual exclusion of the light, air, and warmth requisite for assimilation. Experience has shown that the height of timber crops, as well as being practically proportional to the quality of the soil for the species of tree in question, is, in all regular crops grow- ing on soils and situations of similar quality, and under similar conditions as to their development, as a rule proportional to their basal area until they have completed their chief growth in height. But when the conditions of development vary, as must be the case when, ceteris paribus, certain woods are only slightly thinned, and others moderately, or perhaps even heavily thinned, then the natural proportions between height and girth become to a greater or less extent interfered with. The fuller the leaf-canopy remains, the more, does the form of the bole approximate to the cylindrical (i. e. the higher does the form- factor become) ; and the freer the growing-space, the greater is the tendency to conical growth of bole (i. e. the lower does the form-factor become) with simultaneous increase of branch de- velopment. Experiments carried out in Beech and Scots Pine woods by Dr. Behringer, under the direction of the experi- mental section of the Forest Branch of Munich University, went to prove l that — ' When thinnings were carried out freely, the development in height was relatively much greater than the diametral increment : and that at any rate during a certain period in the growth of crops, the heaviest degree of thinning produced the loftiest and the cleanest boles.' Of course, the correctness of this statement, or of any other dictum with regard to most of the operations of practical sylviculture, depends in each case on the nature and condition 1 Op. cit., p. 28. CHAP, ix.] Tending of Woods 195 of the crop in question as to species of tree, age and mode of formation of crop, condition previous to, and at time of, thin- ning, nature of soil and situation, &c. But Weise1 seems perfectly correct in making the broad generalization that— ' When a crop is too thick, increment in height and in girth both suffer to an extent not compensated by the outturn jnelded from the greater number of stems ; when it is too thin, however, the crop remains back- ward in growth in height.' Experiments made in order to endeavour to formulate a natural law regarding the effect of slight, of moderate, and of heavy thinnings on increment in height, girth, form-factor, and total yield of timber per unit of area, have hitherto failed to yield any practical result. On the whole they simply lead one in a general way back to appreciate the wisdom and the prac- tical value of the rule, founded on experience, that * thinnings should be begun early^ carried out moderately, and repeated frequently' This does not militate against the correctness of the theory and the practice of partial clearance, after once the chief growth in height is completed, for the purpose of stimu- lating the trees to rapid increment in girth and to improvement in the shape of the bole. And, practically, the same conclusion must be come to when the matter is viewed from the financial standpoint. Although increased returns from material thinned out and profitably disposed of — regarding them not only as items reducing the capital represented by the growing stock, but also as sums which, for correct reckoning, must be taken as growing in value at compound interest till the whole mature crop is harvested — would point to the desirability of heavy thinnings, and would perhaps yield fair results where the market for small timber is favourable, yet the future well-being of the ultimate crop is undoubtedly the main object to be kept in view. And here, again, experience has shown that considerations affecting both the productive capacity of the soil, and the normal development 1 See Chronik, 1881, p. 25. O 2 196 Studies in Forestry [CHAP. ix. of the crop, are most favourably kept in view when the degree to which thinning is carried out, at each time of repeating the operation, is only moderate — although on soils of better than a merely average quality it may well be somewhat freer than on those of a poorer nature. 3. Partial Clearances in Tree-forest. Partial clearances are made in tree-forest when over 15 % of the basal area is removed for the express purpose of affording freer supplies of light and air, so as to stimulate the rate of increment, and thus enhance the technical and the financial value of the timber. This sylvicultural operation, which is merely a more vigorous and emphasized expression of the theory of thinning, may be carried out after once the timber crop has passed through the most active period of growth in height ; for then the advantages, offered by increment in girth and in full-woodedness towards the top-end of the bole, are not, to anything like the same degree as during any earlier stage of development, prejudiced by such increment being perhaps stimulated at the expense of the rate of growth in height. The removal of up to 15 % of the total basal area, when the crop stands in full canopy, is still a thinning; whereas the removal of 18 or 20 % is already a partial clearance. But the latter operation is practi- cally merely a continuation of the former ; only it is carried out with a freer hand. Whilst, in thinnings, the conservation of the productive capacity of the soil is one of the most important objects to receive consideration, in a partial clearance its maintenance, by means of the tree-crop alone, is seldom attainable except on soils of the very best quality ; hence underplanting is usually necessary, simultaneously with the partial clearance being made \ Throughout the whole of the operations of tending — 1 A fuller consideration will be given to this subject in Chapter XI, On Underplanting. CHAP, ix.] Tending of Woods 197 the weedings and clearings, the thinnings, and the partial clear- ances— the same object is definitely kept in view, viz. the best possible ultimate development of the individual stems forming the chief financial factors in the mature crop. During all these tending operations the more valuable kinds of trees are not only protected against other species threatening their existence, but efforts are also consistently made to procure for them, at all the various stages of their development, such conditions relative to growing-space, &c., as may produce the greatest outturn of long-stemmed, large-girthed, and full- wooded timber in the shortest space of time — or, in other words, as may produce the most valuable timber, technically and financially, at the least cost of production. In practical forestry this method of partial clearance is to a great extent naturally confined to Oak, Scots Pine, and Larch ; for the other light-demanding species of trees, Maples, Elm, Ash, Birch, &c., which are in request for ornamental work chiefly, are generally utilized during the later thinnings. When forests, in which the ruling species is Silver Fir or Beech, are to be naturally reproduced, the same stimulation to increment in girth, and to improvement in the shape of the bole, is prac- tically obtained during the clearances made preparatory to, and following after, the seed- felling. In sheltered localities the effects of partial clearance are also very profitable in the case of Spruce crops, which, owing to the great danger to which this shallow- rooting species is exposed from windfall, are not generally regenerated naturally, except under very favourable circum- stances as regards protection from winds. When the first partial clearance is made — in Oak woods about the fiftieth to sixtieth year, in Scots Pine between the thirtieth to fiftieth year, and in Larch about the thirtieth to thirty-fifth year — the fall is confined to all stems of inferior development, or to such as do not give promise of ultimately producing timber of the better class. Later on, in about five, or ten, or fifteen years, when the standard trees gradually begin 198 Studies in Forestry [CHAP. ix. to approach each other in an endeavour to form canopy, the clearance has of course to be repeated, in order that the foliage on the lower branches, and within the interior of the crowns, may not be hindered in its assimilative functions, owing to the decreased measure of exposure to light and air to which they must be reduced in anything like close canopy. As in regard to thinnings, there can be no hard and fast rules for the conduct of partial clearances ; for so much depends on the quality of the soil and situation. But, practically, they should be repeated at intervals of about five to ten years at first, and about ten to fifteen years later on. Oak woods treated in this manner about the fiftieth to sixtieth year should, according to Gayer1, yield a quantitative annual increment of from 3 to 3^ % up to their looth year, and 2 to z\ % after that, without taking into consideration the qualitative, technical, and financial increment simultaneously rising more rapidly. At 120 years of age the Oak woods treated thus should show about thirty-six to forty-eight stems per acre. Larch crops partially cleared from the thirtieth to thirty-fifth year onwards should, on situations naturally adapted for their growth, at sixty to seventy years of age show about sixty to seventy trees per acre with an annual increment of from 3 to 4 %. In Scots Pine woods a repetition of the process is only advisable on the better classes of soil, as, otherwise, experience has shown that better results can generally be achieved by letting the whole of the standard trees come together to form the light canopy which is their characteristic on inferior soils and situations, and beneath which a crop of underwood can usually thrive fairly well. In mixed woods of Spruce, Silver Fir, and Beech excellent results have been attained by beginning to thin rather heavily about the thirtieth year, repeating the thinnings every tenth year, and then making a partial clearance between the sixtieth to seventieth year, so as to leave per acre about 120 to 1 60 trees of sound, promising growth. In crops thus 1 Op. cit., pp. 574, 575. CHAP, ix.] Tending of Woods 199 treated, after the lapse of twenty years natural regeneration will generally be found to have been effected spontaneously, the standard trees will be of good marketable dimensions and excellent quality, and the seedling growth will vary from about 3 to 15 feet in height. Blanks left by the removal of the standards can easily be most advantageously filled up by planting with Pine, Oak. Larch, Ash, Maple, &c. Of course, an essential condition for the success of this measure is that the crops are still in active vitality and capable of being stimulated to quantitative and qualitative increments. The operation would be useless in the case of trees already entering, even prematurely from injudicious treatment or any other cause, into the stage of senile decay. With reference to the relative and the absolute increment on individual stems after partial clearance, Behringer l gives some interesting and instructive data, which are exhibited in tabular form on the two following pages. Measurements made at the same time showed that the rate of growth in height had been sensibly diminished in con- sequence of the greater amount of growing-space afforded after the partial clearance. But as the operation was not performed until after the most active period of growth in height had been completed, this diminution was of comparatively little technical or financial importance. So far as these experiments go they prove not only that, owing to the larger growing-space, each of the standards was stimulated to produce more than double the increment in cubic contents which it had before the partial clearance took place, but also that, whilst in regard to the Spruce the enhanced increment culminated within the first decade after this opera- tion, the culmination was delayed in the cases of the Scots Pine and the Silver Fir until the second decade had been entered on. This had also previously been found by Konig to be the case in Beech woods. 1 Op. tit., pp. 59, 60. A. 0 VO O i>. •«*• OS O N H- N Tf-00 VO vg i 1 £ 0? vo rt-n-^^ t^ Tf' i < op oo 1-1 O >o O COOO CO rj- uj O M o o 0 1 fa « *- G 2 55 i 3 £ earance f VO Tj- -i VO O O CO t>. CO »O I ci cs c^ -rj- O ' CO CO 1 13 13 1 o » *0 (O E I .2 1 i »0 t>. U5 O OO M CO »0 I 1 CO ^-J^iO 1 1 ?" S, 1 in | 0 oo vo ONVO o o O ^O »— i 10 O VO 1 •N 0) £ § S3 * £ S CO CO ^^- CO CO 1 CO B s s VO VO CO co O CO J^ C* M OO CO 0* 1 00 OJ oo vo rt ^3 S 1 i CO CO CO co •<*• *>• 9 CO 0 M 1 « S . Cv •'t1 i>. O ^ co •n J. S 1 C/3 § vi M VO Tt- ON Ui CO N • a\ o\ a^ co i -< M M « ir.oo o N ! E &* *"* V. s 1 .2 CO CO !>. HH U5J>, . 3 B & c 1 4, « co COVO 1-1 § 4> T 3 4J . . • • PH I 2 B fcJD & :J 3 tn (M 1 'a ^ s R a 0 & S g«S s c B bo > S .2 ^^ 5 s s = u V w be rt £ w S "w 1 ^ COVO O COVO ^ COVO 6 covO ? i *^«« Os^-^ ^ CO 1 | 1 oT in« « « 6 6 f* it "E ? f VO H- O fC « VO in ^t* co o ro in vo a v? n -^- I-H cooo « tc o ON ONOO in « A M ^ 6 6 1 0 CO 8 o ro 53 d o « ONt^co « KH Tf O M OO VO u CO oo 0 g; 5 t: c & AH rt _ O "- u ** I § 2 VO o 0 ON ON^t- N 5^ O"svO VO ^O *O i tg >» u s\ a >- M co N O ON O vo i^ rcoo « C^ M M » 6 6 § U o oo vo m CO 6 li CO ^ o> M 00 r-VO M O T.VO i u in §| CO C/3 j3 . <3 ci « « M « 6 6 c ro ^ (N O "*•* u rt ^ « > cS £ | 1 jy CO O -+0 vo O « O CO CO t^ J^ ro PH 6 6 6 6 6 crement T ? 43 a c 8 r4 J3 H W g 1 i m »n ONO O\t>. ON O ON O *>• M •^~ t^. 1 c 0 ? PL! i O M o M O 0 o 6 . ^ • . . . rt . • "3 'io O •E 3 " e C rt* c * •*-> 1 'a * s a a < • o g CO * *jy * H ro *^ 0 M *x ^ • c | ^ rt ts £ | o> bJD o ta .5 tJ 3 V ^^ t^ 3 C/3 *^< fCO O fOVO U *i rOVO 6 rCVO ^ w N T^ ino c 2O2 Studies in Forestry [CHAP. ix. That, at the same time, a qualitative enhancement takes place along with the quantitative increment of the timber is clear from the researches of R. Hartig, who asserts1 that in general, without variations according to the species of tree, the quality of the timber grown in the comparatively full exposure to light and air is better than that formed under other conditions. This is due to the fact that the extent to which transpiratiofi is carried on through the foliage does not increase pan passu with the enhanced rate of increment, as the conductive capacity of the vessels in the new zones of wood is relatively smaller, in consequence of the ligneous deposits within the cellular tissue being thicker and denser. And, further, when underplanting is simultaneously carried out, the undergrowth keeps the soil and the root-system cool, and thus retards, for at least a fortnight, the awakening of active vegetation in sprirlg; hence the latter is only entered upon when the weather has become somewhat warmer, and when the assimilative and constructive processes can consequently be performed more thoroughly and energetically, owing to their taking place under more favourable conditions as to warmth and sunshine. To determine whether or not a partial clearance is likely to be financially remunerative, practical figures, based on past average results for crops of similar kinds on soils of similar quality, are requisite. Where these are available, the reckon- ing is very simple by means of the following equation : — When C = the cubic contents that may be expected from the mature crops with ordinary treatment only, V = the value of same per load, or per cubic foot, at time of harvesting the mature crop, ta • • • • tq — outturn in cubic contents from ordinary thinnings from now till harvesting of the mature crop, va - • . . v q = the sale-price of same per load, or per cubic foot, capitalized until the clearance of the mature crop. 1 Centralblatt fiir das gesammte Forstwesen, 1888, pp. 8, 363. CHAP, ix.] Tending of Woods 203 And Q = the cubic contents expected from mature crop after treatment by partial clearances, Vx = the value of same per load, or per cubic foot, at time of final clearance, to. ---- t£ = outturn in cubic contents from partial clearances up till the harvesting of the crop, va . . . . v$ = the sale-price of same per load, or per cubic foot, capi- talized until clearance of the mature crop takes place. When x is a minus quantity, then the method of partial clearance is remunerative, and therefore advisable. „ x = o, then there is no financial advantage to be gained by partial clearances. „ x = a plus quantity, then the ordinary method of treatment by thinnings merely is the more advantageous. But when underwood, which should almost always be formed — even on the better classes of soil — can only be pro- duced after a certain amount of outlay, then the complete and correct formula for estimating the financial prospects of the operations must be : — CV + fava+ or, in another form similar to that originally given, — Where /* = the outlay for producing underwood, capitalized until final clearance of the mature crop, and r — the market value of the underwood at the time of clearance of the mature crop. Practical experience in Germany has shown that this method of partial clearance should, under ordinary circumstances, only be adopted on the better classes of soil, and when undergrowth can be formed either naturally or without any considerable outlay. Pruning or Removal of Branches. High-forest crops, which have been properly tended and thinned throughout the various stages of their growth, require, 204 Studies in Forestry [CHAP. ix. as a rule, no clearance of branches in order to improve the shape of the bole. The cutting and the lopping of branches are both merely measures adopted, often at considerable outlay, to cover the effects of faulty treatment of the crop during the past, and are, in general, not requisite where trees have gradually been accustomed to a fuller measure of individual growing- space. In the case of copse or standards over coppice some diminution in the amount of shade cast may be necessary for the well-being of the underwood; and, within certain limits, this can be effected by thinning the crowns of the standard trees forming the overwood. Under ordinary circumstances, the removal of living branches can only take place to a limited degree, and must in any case (for financial reasons) be confined to the more valuable species of trees. The manner in which the crown is set on the tree is of well-known influence in determining the shape of the bole, as stems with lofty crowns are more full-wooded at the top-end, and approximate more to the cylinder in shape, than such as have deep-seated crowns of foliage. In order that any benefit may be derived from the operation, it is necessary that pruning should be carried out when the trees are in their full energy of growth, and as early as possible before the period fixed for their mature fall. In many cases, too, where the crowns of the trees are very dense, a fillip may be given to their general energy in growth by thinning out some of the branches, so that the foliage re- maining may have a larger share of the nutrients extracted by the root-system from the soil. The stimulation thus given to the energy of assimilation is perhaps nowhere more notice- able than with regard to young Larch trees, the lower portions of whose foliage may have already been attacked by the Larch mining-moth (Coleophora laricelld). The removal of dead branches, when carefully conducted, so as to leave no ragged surface likely to offer a favourable germinating-bed to fungoid spores, interferes in no way with CHAP, ix.] Tending of Woods 205 the performance of the vital functions of the rest of the tree. On the contrary, when the operation is carried out smoothly and close to the stem, it prevents the formation of hard, horny knots in the wood ; and this consequently enhances the value of the timber, considerably diminishes the danger from fun- goid diseases, and favours an early and complete cicatrization of the wound-surface. It is therefore particularly to be recom- mended in the case of Oak, Pine, Larch, Spruce, and Silver Fir, whose dead branches are much more apt than in other genera to form hard, tough snags, which, becoming gradually embedded in the stem by the new growth of annual zones of wood, diminish the value of the timber for technical purposes, and thereby affect its market price. The removal of living branches is, however, a direct inter- ference with the vital condition of the growing tree, and can therefore only be ventured on to a limited extent. Under no circumstances should more than one-third of the total quantity of foliage be removed at one time ; practically, only about one- fifth of the foliage is generally the extent removed during such operations. Experience has shown l that, even in the case of quick-growing kinds of trees, the removal of living branches should ordinarily be confined to those that are not over 2\ inches in diameter for conifers, or not over 4 inches for broad-leaved species of trees, as, otherwise, the process of cica- trization cannot take place quickly enough to ensure hindrance of the germination of fungoid spores producing disease. As the broad-leaved species of trees are not so liable as conifers to fungous infection, they usually stand trimming better. With reference to this matter Professor R. Hartig remarks that 2 : — • When branches are removed from a tree, it thereby acquires a pre- disposition for a number of wound-diseases, of an infectious or non- 1 See Ney, Die Lehre vom Waldbau, 1885, p. 300; also Gayer, op. cit., p. 584. a Lehrbuch der Baumkrankheiten, 1889, p. 15. 206 Studies in Forestry [CHAP. ix. infectious nature, which may be obviated by timely and effective closure, i. e. by antiseptic treatment.' And at another place he adds * : — ' In broad-leaved trees, especially the Oak, to which my investigations have hitherto been confined, wounds over 4 to 4-8 inches in diameter, should not be made.' The species of trees which best stand the removal of green branches are the Oak, Silver Fir, Larch, and Pines, when they are in energetic growth on favourable soil and situation and have normally developed crowns. Ash, too, can well bear the operation ; but, as Ash and Alder both grow with naturally clean stems, pruning is hardly requisite in their case. Whenever the removal of branches takes place to any great extent from Oak, Maple, Sycamore, or Elm, the result is that the bole has a ten- dency to become covered with shoots from the dormant buds. This, of course, interferes very considerably with the technical and financial value of the stem, besides, particularly in the case of the Oak, exposing the tree to the danger of becoming ' stag- headed' or dead in the upper portion of the crown. The soft- woods— Birch, Willows, and Poplars — are not naturally adapted for this kind of treatment, owing to the comparatively slight resistance which their soft, porous wood is able to offer to the development of fungoid disease ; hence any wound-surfaces formed afford only too favourable a germinating-bed for the disease-producing spores. In order to diminish the danger from fungoid diseases, it is highly recommendable that the wounds should be coated over with some antiseptic substance impervious to moisture. In conifers this takes place naturally by the oozing out of resin ; but some coating must be provided artificially in the case of the broad-leaved genera. The tree-wax, formerly in general demand for the purpose, consisted of a mixture of 1-20 parts (by weight) of bees-wax, 2-70 parts of pure resin, 0-60 of tur- pentine, 0-15 of wood-oil, and 0-15 of suet, all dissolved in 1 Ibid. p. 228. CHAP, ix.] Tending of Woods 207 warm methylated spirits. Nowadays, however, the simpler method of coating over the surfaces with coal-tar, slightly thinned with oil of turpentine, finds general adoption owing to its cheapness. The coating of tar will only bite into the surface satisfactorily whilst the wood is relatively free from sap ; hence it should be administered either towards the end of October, immediately after the vital functions of the foliage have been completed, or at any rate some time during the first half of winter. Unless the removal of the branches takes place in autumn or early in winter, the experiments made by Professor R. Hartig of Munich tend to show that, in addition to the tar not obtaining a good hold on the wound-surface, the condition of the woody tissue is such as to make it less able to resist the penetration of fungoid, disease-producing spores. Practically, the same principle holds good here as in regard to, the thinning of young tree-forest ; for it is much better to thin out branches to a moderate extent only, and then repeat the operation subsequently if necessary, than to endeavour to effect the object in view by one coup de main. The cost involved by the operation varies, in each particular case, according to the local rate of wages and the handiness of the workmen, the species of trees, the height at, and the extent to, which the branches are to be removed, &c. ; but in Germany it has been found to vary generally in amount from about \d. to 2d. per stem for sawing off the branches and tarring the wound-surfaces. In Britain, it will, for various reasons, prob- ably cost quite the double of this amount ; but, even then, it may, under certain circumstances, prove a highly remunerative operation if judiciously conducted. With regard to the remunerativeness of the removal of branches, Alers, who invented the patent long-handled saws now usually employed in the operation, estimated that if begun in the thirtieth year of age of the crop (coniferous ?), and re- peated every five years till the fiftieth year, at a cost of about i\d. per stem, the net results at eighty years of age, after 208 Studies in Forestry [CHAP. ix. deducting the various outlays capitalized at compound interest up to that date, would show a profit of 12 %. It is impossible to criticize such a vague estimate without examining all the data closely, and ascertaining what the results would be for a fall of timber fixed at 100, 120, or 150 years; but, at any rate, it is worth remarking that the practical effect of Alers' agitation has been to induce the Prussian Government to undertake regularly the removal of all dead branches in forests grown for the production of valuable timber stems, and not intended merely to be utilized as fuel. From the national- economic point of view this may be advisable in State forests, though for private landowners it is a purely financial question, concerning which local experience will best guide the sylvicul- turist to a sound judgement about the matter. In accordance with the natural laws of tree-growth, as increment begins at the top and is gradually continued towards the base, the removal of a portion of the foliage diminishes the amount of elaborated nourishment available for structural purposes towards the butt-end of the trunk, and thus leads to improvement in the form-factor of the bole ; whilst at the same time, as R. Hartig has also shown, the quality of the timber produced improves the more, the less difference there is in the quantitative incre- ment proportionately to the surface of the foliage through which the process of transpiration is carried on. That, in consequence of this artificial thinning of the crown, the growth in height is stimulated, is a point about which experts have hitherto differed, and which has not yet been determined by any series of authoritative experiments. Thus, while special circumstances have most influence in- each particular case relative to the remunerativeness of such measures in private woodlands, the general statement can at any rate be made, that the removal of sickly, rotting branches — or of all those infected with parasitic growth of Loranthus or Mistletoe, or of such as exhibit deformities like twig-clusters (e. g. those caused by Aeddium elatinum on Silver Fir, and CHAP, ix.] Tending of Woods 209 called ' witches' brooms ' in Germany), or show any other forms of fungoid diseases — is certainly advisable, even at some consider- able outlay, in order to prevent the propagation of the disorders, and the penetration of diseases into the stem. But, at the same time, in coniferous forests it also diminishes the liability of the crops to be damaged by storms or by heavy accumula- tions of snow and ice. And, finally, not its least utility is to be found in the fact that, in mixed forests, the judicious removal of lower branches often enables a greater density of crop to be maintained for some years longer than can possibly be the case if tending is confined solely to the operations of thinning. For species like Ash, Maple, and Sycamore, which attain maturity at a comparatively early age, this last consideration is a matter of no little sylvicultural importance. CHAPTER X METHODS OF STIMULATING THE INCREMENT IN TIMBER-CROPS WHEN APPROACHING MATURITY IT is a well-known fact that, when trees growing in close canopy are thinned out, or when in the case of old crops approaching maturity a partial clearance is made, the annual increment on each individual stem naturally rises in con- sequence of the decrease in the number of stems drawing food-supplies and moisture from the soil, and engaging in the unavoidable struggle for light and air. In the system of selecting only the largest trees for ex- traction, in standards over coppice, and in standard trees retained in high forest for a second period of rotation, such increment in growth is certainly attained. In the following cases, however, the question to be considered is mainly con- nected with heavy thinnings, or a partial clearance made shortly before a crop falls to the axe, in order to stimulate the remain- ing trees to more energetic growth in girth before the date at which the fall should take place according to the Working-Plan. It is, in fact, but the continuation of the thinnings that have been made as measures of tending throughout the whole life- time of the crop, only it is carried out more freely on account of this being the last thinning that is to be made before the trees attain their full maturity. If less than one-fifth of the total amount of timber on the area be removed the operation may still be considered as a heavy thinning, whilst if one-fifth CHAP, x.] Stimulation of Increment 211 or more of the crop be thus prematurely utilized it must certainly be considered a partial clearance. That such measures undoubtedly do lead to a stimulation of the annual increment is a fact not only abundantly shown by practical experience, but also proved more than half a century ago by the more eminent sylviculturists of Germany, C. Heyer, Th. Hartig, Nordlinger, and others. These authors showed conclusively that a stimulation of the increment on individual stems took place, as the natural result of all such thinnings as exceeded in degree the natural process of that unavoidable struggle for existence in which the stronger first overtops and finally suppresses the weaker individual stems, whenever such free thinnings were made in forests growing in dose canopy, and at an age not exceeding to any considerable extent the normal periods of rotation under which the species of tree in question was usually grown as a timber crop. Every now and again, however, some champion steps forward to dispute what have long been accepted as facts; but the plausible deductions drawn from his observations are always, on closer investigation, found to have some flaw. Thus, for example, he may have confined his attention to the bole only, or have neglected to discriminate between the direct effects of the freer exposure to light and air, and the adventitious circumstances under which the latter may have taken place, although these concrete conditions are at times of such influence as to diminish, or even to counteract, the intended results of the thinning or partial clearance. There is generally some very easily determinable reason when this latter measure fails to produce more energetic increment. The thinning or partial clearance may, for example, have been carried so far as actually to have interfered with the normal functions of the root-systems and the crowns of foliage of the individual trees left forming the crop. These nouveaux riches may often require some little time to settle down and accustom themselves to their altered circumstances ; and the first form P 2 212 Studies in Forestry [CHAP. x. in which this makes itself apparent is very frequently rather in the energetic formation of new roots and of thicker foliage, which ultimately exert their due influence on the increment of the stem, than in the immediate thickening of the annual rings, or the immediate formation of woody-fibrous tissue. And, wherever the other main factors exerting influence on the pro- ductive capacity of the soil are not at the same time tended and well provided for, stimulated increment cannot always be expected as the natural result of diminishing the number of trees forming the crop. Thus, for example, care must be taken to prevent deterioration of the soil (where necessary, even by underplanting) in consequence of insolation, and of the drying and exhausting effects of winds, or with regard to the soil- moisture and to the soil-covering of dead foliage requisite for the formation of humus or vegetable mould. In one case, however, the current increment of the trees may be directly decreased at first in place of stimulated. This is, when the fuller exposure to light and air leads in the first instance to abnormal increase in the production of seed, in consequence of a tendency to the formation of albu- minoid substances in place of carbo-hydrates ', as is especially liable to take place in the case of trees that were already pre- dominating throughout the canopy at the time of the partial clearance being made. And, of course, if the partial clearance be carried too far, the increment on the remaining crop will probably be injuriously affected by the natural consequences resulting from over-exposure of the soil to insolation and the action of winds, and from exposure of the stems themselves to sunburn or scorching of the bole in smooth-barked species, to increased danger from windfall and insects, as well as to the greater damage apt to be done during the felling of the stems that are being removed, and the grubbing up of their stumps. 1 Rinicker, Der Zuivachsgang in Fichten- und B^uhenbestdnden, 1886, p. 30. CHAP, x.] Stimulation of Increment 213 Theodor Hartig was the first to assert l that, as the direct and immediate consequence of the freer exposure to light and air, without reference to the species of tree, stimulated incre- ment on each individual tree invariably took place, though subject to the influence of the other factors determining the rate of growth. When any apparent exceptions to this rule are met with, they are neither ascribable to differences in the species of trees, nor to differences in respect of soil and situa- tion, but are solely due to one or more of the above-indicated causes. Species of timber, soil, and situation certainly exert their influence as regards the extent to which increment may take place ; but they are not of themselves the direct or primary cause. There is, however, good reason for believing that deci- duous trees are enabled by nature to avail themselves of the direct and immediate increment to a somewhat greater extent than those coniferous trees which retain their foliage throughout the whole year. The enhanced increment need not assume the form of broader annual zones of woody-fibrous tissue along the bole. It may, and very often does, at first take the shape of con- siderable changes throughout the root-system and the crown of foliage, primarily and undoubtedly due to the freer ex- posure to light, air, and warmth. This paves the way for the succeeding form of enhanced increment, due to these changes in, and increment of, the assimilative organs, which makes itself more readily distinguishable throughout the stem and branches. The extent to which the annual increment thus becomes enhanced varies in any particular species of tree according to the individual stem, its age and reproductive capacity, the soil, situation, and exposure on which the crop grows, the density of the canopy throughout the crop, and the development of the crown of foliage borne by the individual stem. The younger and sturdier the tree, the better developed its crown, 1 LehrbuchfiirForsier% 1861, vol. i. p. 105. 214 Studies in Forestry [CHAP. x. the more favourable the soil and situation may be to the thriving of the particular species of tree, and the denser or more crowded the wood, so much the more likely is the influence of the thinning or partial clearance to be readily observable. That the extent to which it is perceptible varies in the different genera of our forest trees has been above indicated and really requires no explanation. Thus, for example, Oak, Pine, and Larch, that have been grown in pure forests, in which there is a strong tendency for the trees to thin themselves naturally to such an extent as to make the canopy loose, if not broken, and to allow of each individual stem forming a larger crown than is usual in the case of shade-bearing genera like Beech, Spruce, and Silver Fir, can hardly be expected to derive so much benefit as these latter from any artificial diminution of the number of stems per acre. In many such cases, indeed, this natural thinning, especially when the Oak, Larch, and Pine are approaching the time of maturity of the crop, may have pro- ceeded so far that any further artificial clearance might lead to diminution instead of enhancement of the increment of the remaining stems in consequence of deterioration of the soil, unless underplanting take place at the same time in order to improve, or at any rate protect, its productive capacity. As it is well expressed by Gayer l, the founder of the modern school of scientific sylviculture — ' Whenever the partial clearance is likely to lead to interruption of the canopy of the crop, it should only be carrried out when the productive capacity of the soil is such as promises, in all its essential factors, to supply continuously the increased demands made in consequence of greater energy in the crown of foliage (transpiration and assimilation), i. e. that the soil in question is fertile, or that care may be taken to stimulate the productive capacity of the soil in some suitable way at the proper time. This can only take place through the maintenance of a good layer of humus and the careful retention of soil-moisture, and consequently in many cases only by means of underplanting in order to protect the soil against sun and wind.' 1 Waldbau, 3rd edit. 1889, p. 571. CHAP, x.] Stimulation of Increment 215 But in the case of the shade-bearing genera, Beech, Spruce, and Silver Fir, which (except in cases of accident) remain in dense canopy throughout their whole period of growth, right up to their normal maturity, the effects of the freer exposure to light, air, and warmth procured for the individual stems by heavy thinning, or by partial clearance when they approach the prescribed time of fall, are often during the first year marked by a two-fold to ten-fold increase in the breadth of the annual zone of woody-fibrous tissue1. This stimulation of increment can also in the case of these trees be attained with a far less degree of clearance ; hence, with proper care, there need be small danger of the soil being in any way injuriously affected owing to the partial and temporary interruption of the canopy to a slight degree. This fact is easily explained by the smaller absolute measure of light and air available for these shade-bearing species when grown in canopy of normal density. Thus, whilst the laws regulating the increment in all species of forest trees are substantially constant, the extent to which the enhancement of increment may take place after partial clearance has, so far as observations have yet been recorded, been found to be practically in the inverse ratio to the require- ments of any particular species with regard to light and freedom of crown. The Causes of the Enhanced Increment explained. Various causes have been assigned to the effects produced in enhanced increment after partial clearance2. Th. Hartig considered it to be due rather to the utilization of reserves of productive matter collected and stored up in the stem whilst it stood in close canopy, than to any increased assimilation in direct consequence of the increase in foliage that takes place when the individual tree obtains a larger growing-space; 1 Grasmann, Beitrag zur Lthre vom Licktungszuwachs, 1890, p. 9. 3 Idem p. 4. 216 Studies in Forestry [CHAP. x. whilst Nordlinger, on the other hand, ascribed the enhance- ment in increment to the increase in the foliage, but laid particular stress upon what he considered the fact, that the enhancement was not so much the direct result of the increase in the mass of foliage as of the stimulated assimilative activity of the leaves and needles, with simultaneous temporary increase in the productive capacity of the soil. The correct explanation as to the enhanced increment is probably to be found in a combination of these views. It seems much more than probable that the utilization of the reserves of productive matter (principally starch in various forms) is most likely greatly favoured by the more active assimilation of nutrients whenever the increase in the foliage takes place; and there is no reason why this should not be directly con- nected with the formation of the fuller crown of foliage immediately after the partial clearance has been made. It is still an open question how such reserves of nutrients are formed, how they circulate throughout the tree, and how they are finally utilized, although their existence in the parenchym- cells of woody-fibrous plants is just as well known as that of similar reserves in orchids, perennial tuberous plants, &c. The recent destruction of forests in Bavaria by the Nun moth has given Professor R. Hartig of Munich special opportunities for studying a part of this subject, particularly with regard to the Spruce l ; and he has conclusively proved that this species of tree has much fewer reserve supplies of nutrients than the Scots Pine. In general, as is well known, such reserve supplies are far more plentiful in the broad-leaved deciduous species of trees than in conifers, and larger in the deciduous Larch than in the evergreen conifers. All the changes that take place in trees prior to the commencement of the assimilative activity in spring are ascribable to these nutrient reserves — the flowering 1 See Forstlich-naturwissenschaftliche Zeitschrift for January, February, and March 1892. CHAP, x.] Stimulation of Increment 217 of Hazel, Alder, and Willow, the swelling of the buds and the flushing of the young leaves, the formation of rootlets, &c. In fact, all the similar phenomena previous to the development of independent cambial activity must be ascribed to these reserve supplies of starchy and nitrogenous nutrients. The supply of reserves is usually sufficient to maintain vegetation for one complete year, and often for longer; indeed, in many cases it amounts to 7 or 8 % of the total weight of thirty-year-old timber crops. Diminution of light and foliage, consequent on limitation of growing-space, must interfere with the utilization of these reserve nutrients ; hence it is quite logical and reason- able to expect that with more growing-space, and a consequent increase of foliage, these reserves should be largely drawn upon and utilized. That any stimulation of the productive capacity of the soil takes place in consequence of the freer penetration of the atmosphere, and the stimulus given to the formation of humus or vegetable mould, is doubtful, or even more than doubtful ; for, unless the canopy still remains comparatively dense, the soil soon becomes covered with forest weeds, which often really consume the mould, and tend to exhaust the soil, in place of allowing the timber crop to have the full benefit of the humus. The true physiological cause of the enhancement in incre- ment, after heavy thinnings, or partial clearance of crops of trees approaching maturity, is to be found in the stimulus to the formation of starchy matter afforded by insolation ; for the degree of activity of the assimilative organs is dependent on the purity or brilliancy of the rays of light, as the decom- position of the carbonic acid in the atmosphere can only take place when the waves of light attain a certain length. Whilst a crop is growing in full canopy, the assimilative activity of the foliage forming the lower portion of the crown is extremely small, owing to the low quality of the diffused light which is alone available ; but, when the canopy is opened up to a suffi- 2i 8 Studies in Forestry [CHAP. x. cient extent, these portions of the lower foliage, which have been practically inactive, or may perhaps even have been existing on the work done by the upper leaves or needles, reassume their normal assimilative functions and help to enhance the general increment of the tree. And, besides this increased assimilative power of the foliage, the consequent increased formation of new leaves and needles is undoubtedly of enormous influence in maintaining and increasing the general enhancement of increment throughout the stem. As remarked by Konig1, the direct result of the freer exposure to light and warmth leads to the better and more energetic development of the leading-shoots, the strengthening of twigs, and the formation of twigs from buds that would otherwise most probably have remained dormant. The enhanced increment continues until the crop once more forms close canopy. But, if it be again stimulated by a repetition of the thinning out or partial clearance, this may — if not accompanied by underplanting — be carried so far as to involve deterioration of the soil to such an extent that the beneficial influence of light and warmth on the crown is cancelled by the diminished activity of the root-system, con- sequently involving decreased supplies of moisture and of mineral nutrients for conveyance to the assimilative organs. The simultaneous underplanting of crops subjected to this system of partial clearance, and especially of those of light- demanding kinds of trees — Oak, Ash, Maple, Larch, and Scots Pine — has an undoubtedly stimulating result in effecting and maintaining the enhancement of increment after partial clearance, and is of particular interest from the financial point of view. The influences exerted by the soil, the situation, and the age of the crop, exhibit themselves rather with regard to the extent of the enhancement in increment than to its production and continuance. Unless the individual trees are 1 Ueber Lichtungszuwachs, insbesondere der Buche, 1886, p. 7. CHAP, x.] Stimulation of Increment 2 1 9 already far past their normal maturity, and have begun to show signs of the loss of energy in growth due to a foreshadowing of the approach of senile decay, they must receive a fillip from admission to larger growing-space and freer exposure to light and warmth. When, however, the vital energies of the trees are weakened by age or disease, normal enhancement of increment need not be looked for. The circulation of the sap throughout the stem must already be to a greater or less extent interfered with; whilst the root-system is also unfitted to discharge the extra duties it is called upon to perform. Trees, that are not very far past the period at which their current annual increment has culminated, as well as such as have not yet attained the culminating point, are, however, unquestion- ably stimulated to livelier energy, which manifests itself in enhanced increment. But, in practice, this system of partial clearance, for the speedy formation of the more valuable assortments of timber, is seldom applicable to very young woods, or to crops that are already much older than the usual periods of rotation. It generally finds proper scope only in mature crops of high forest and in those approaching maturity. And in these cases the age of the crop has little influence on the length of time throughout which the enhancement of increment is maintained ; for this is determined rather by the length of time which it takes the crop to form close canopy once more. The nature of the development of the crown is, however, of greater importance than the age of the crop. If the previous thinnings have been neglected, and if the canopy has been allowed to remain so dense that the woods are crowded, it often happens that, on receiving increased growing- space, the trees with their weakly crowns are unable to avail themselves of the advantages thereby offered, and exhibit, as may so often be seen in the case of Oaks, a tendency to the development of dormant buds, which leads to * stag- headedness* or death of the crown, and malformation of the bole. 220 Studies in Forestry [CHAP. x. Practical Advantages of the Method of Partial Clearance. From the practical sylvicultural and the financial points of view such heavy thinnings or partial clearances should not be made until after the crop in question has completed its chief growth in height. Along with the other advantages of natural reproduction under parent standards, the rapid increment in timber, as well as in the technical and financial value of the latter, which takes place after partial clearances made for the purpose of regeneration, has drawn considerable attention to this method as a system of treatment of woods, even when their artificial reproduction — as in the case of Oak, Maple, Larch — may generally be considered more advisable than natural regenera- tion. The favourable returns received from the gradual clearance of parent standards in the case of natural repro- duction of Beech, and of Silver Fir in particular, as well as the financial advantages that accrue ultimately from the partial clearance and underplanting of indifferent crops of Oak, Larch, and Scots Pine when they approach maturity, have to a great extent dispelled the prejudices that existed against the system in the minds of some as being entirely inconsistent with the natural course of things, and have won for it recognition as a method of treatment worthy of adoption wherever circum- stances admit of its practice. There seems little doubt that in the near future it will be carried out to a much greater extent than at present, as it combines most of the advantages of standards over coppice with decided sylvicultural and financial advantages of its own. Thus, for example, by means of this method of partial clearance, the larger and more valuable assortment of stems can be produced in a shorter time, i. e. at a less cost ; whilst, instead of a high forest of normal density composed of nearly mature trees, with an average annual increment long past their point of culmination and gradually CHAP, x.] Stimulation of Increment 221 sinking, an equal and often a greater annual increment per acre is attainable after the partial clearance. This pays as well, and often better, than if the full crop had been allowed to attain maturity, besides yielding substantial returns from the timber prematurely utilized. When the gradual clearance of the parent standards is effected during natural reproduction, it is in no way inconsistent with what has been above said, if, before the formation of the young crop, the average annual increment of the standards is below that of normal high forest reproduced by total clearance and sowing or planting ; because, counting from the time the young crop may be considered formed, the enhanced increment on the more or less isolated standards is undoubtedly more favourable finan- cially than when a total clearance is immediately followed by artificial reproduction. That portion of the fixed capital which is represented by the growing crop is considerably reduced by means of the partial clearance ; and the money thus derived as intermediate returns can be otherwise utilized in order to yield interest for itself, whilst the material left standing increases in the per- centage it affords. Thus, if the partial clearance amounts to one-fifth, or one-third, or one-half of the total crop in close canopy, it has been satisfactorily proved by several authorities * that the enhanced increment on the area partially cleared at least equals, and often exceeds, the total previous current annual increment, notwithstanding the diminution in the number of trees thereafter forming the crop. The financial advantages derivable are thus summarized by Grasmann 2 : — i. The larger and more valuable assortments of timber can be produced in shorter time, and therefore more cheaply, by this method. 1 Wagener, Der Waldbau und seine Fortbildung, 1884, p. 208; Kraft, Beitrdge zurforstlichen Zuwachsrechnung, 1885, pp. 99 et seq.; and others. 2 Op. «'/., p. ii. 222 Studies in Forestry [CHAP. x. 2. Instead of the full crop, with small annual increment on a larger number of individual stems, three factors are favourably introduced and combined, viz. : — i. Good intermediate returns are available, capable of producing interest for themselves. ii. The enhanced annual increment on the remaining crop equals, and often exceeds, that produced by the full crop previous to its partial clearance. iii. The young crop produced naturally or artificially under the parent standards often practically equals in incre- ment a young crop formed artificially by sowing or planting. What Loudon says l of the Oak may be applied to all our forest trees grown as crops with a view to remunerative returns from the capital invested : — ' The age at which Oak timber ought to be felled, with a view to profit, must depend on the soil and climate in which the tree is grown, as well as on other circumstances. Whenever the tree has arrived at that period of its growth, that the annual increase does not amount in value to the marketable interest of the money which, at the time, the tree would produce if cut down, then it would appear more profitable to cut it down than to let it stand.' Whilst this is perfectly correct for each individual tree grown in the comparatively isolated positions that timber trees usually occupied in Britain at the time the above was written, it in no way precludes the possibility, which in fact we know from actual experience to be the case, that when the current annual increment per acre has sunk below the point up to which it is not unprofitable to allow a crop to remain in the full normal canopy of its species, it can be stimulated and rendered more profitable, often very considerably so, by the above-indicated method of partial clearance with a view to the earlier production of valuable stems of large girth. In regular high forest, with natural reproduction, the time of regeneration 1 Arboretum et Fruticetum Britannicum^ 1838, vol. iii. p. 1809. CHAP, x.] Stimulation of Increment 223 is often, in order to attain good boles of valuable dimensions, prolonged till after the period when energy for the formation of seed, or the natural reproductive capacity is already some- what weakened. By means of partial clearances, however, the regeneration can be favoured during the chief natural seed- producing period of growth ; whilst, at the same time, as good dimensions of timber may be obtainable as in the regular high forest, and in a more profitable manner. Thus, for example, in the reproduction of Spruce in sheltered localities — where windfall is not likely to occur, and where the period of reproduction may be taken to be usually about a hundred years — if partial clearance be made about the seventieth year, during the time of the most active production of seed, the financial position of soil plus crop during the succeeding thirty years will almost, beyond question or doubt, be much more favourable than if the crop had been allowed to stand as regular high forest till the full period of rotation originally fixed in the Working Plan had been attained ; for it is almost certain that the partially cleared crop will contain a relatively higher number of boles of valuable assortments than would have developed themselves under the system of regular high forest. And what is said here with regard to Spruce is still more applicable in respect to the other two great shade-bearing genera, the Silver Fir and the Beech. The whole system is, in fact, merely a modification of, and improvement on, the older system of natural reproduction under parent standards. But, whilst in the latter case the seed fellings (partial clearances) before and during the time of seeding, and the gradual clear- ances after the formation of , the young crop, took place mainly with the object of effecting natural regeneration, the partial clearances under the new method are made with the distinctly avowed intention of stimulating the standard crop to enhance- ment of the annual increment, and to the yield of more favourable returns from the capital represented by soil and growing crop. In the former case formation of a young crop 224 Studies in Forestry [CHAP. x. was the motive, and enhanced increment on the parent standards the effect; in the latter, enhancement of annual increment is the object, and simultaneous natural reproduc- tion of shade-bearing kinds of trees is the result of this sylvicultural operation. Rules for the Conduct of Partial Clearances. With the light-demanding species of trees, when they are not grown in mixed forests along with shade-bearing species, underplanting is almost a necessity after heavy thinnings or partial clearances, in order to maintain the productive capacity of the soil. The manner in which this method of treatment is applied to the various chief genera of our light-demanding forest trees — Oak, Pine, and Larch — is as follows : — Oak. — When pure forests of Oak have passed through the regular processes of thinning, and approach the time for a partial clearance taking place, their canopy is in general somewhat light and thin, although perhaps not broken ; and the under- growth is usually already beginning to form canopy for itself below the older crop. To avoid the formation of twigs and shoots from the dormant buds along the stem, often leading to ' stag-headedness V the partial clearance should not be made by one fall, but is better attained by one or two heavy thinnings conducted to the extent deemed advisable for each individual crop. The time at which it should take place is also dependent on the special circumstances of each crop, special regard being given to the time of underplanting and the development of the undergrowth, the energy of growth of the trees, and the nature of the soil and situation. As, however, the efficacy of this method of treatment is all the more apparent the earlier 1 In his Lehrbuch der Baumkrankheiten, 1889, p. 14, R. Hartig remarks that : — ' Oaks, which have grown up in close canopy along with Beech and have only a slightly-developed crown of foliage, acquire a predisposition towards a drying-up of the top of the crown (stag-headedness) when they become fully exposed to light and air ; whilst, under similar conditions, trees with well-developed crowns do not suffer from this disease.' CHAP, x.] Stimulation of Increment 225 it can be begun, the thinnings should, if possible, be com- menced about the fortieth to sixtieth year. They should at first be confined to the young stems of backward growth, and to such as are never likely to attain good marketable shape. The oftener the thinnings can be repeated at short intervals the better, as any sudden exposure of the boles should be carefully avoided. About ten or fifteen years after these preliminary operations have been begun, the main partial clearance will in most cases seem advisable ; for by that time the crop should be in a state of active increment, due to the favourable influences of the undergrowth and the previous thinnings. Here, again, as also whenever further partial clearances are considered necessary later on, the fall is in the first instance confined to trees that have been damaged by organic or inorganic agencies, or that do not continue to yield satisfactory increment ; and not until all such unremunerative material has been removed should any sound trees in energetic growth be cut out. When the main partial clearance has taken place about the seventieth year, and has been followed by minor gradual clearances at intervals of five years at first, then of ten, and later on of fifteen, the preliminary yield or intermediate returns thus obtained should amount, according to Kraft *, respectively to about 288 to 628 cubic feet, then to 720 to 1,080 cubic feet, and ultimately to 1,800 cubic ft. per acre, inclusive of branch- wood. Past experience seems, according to Gayer 2, to justify the hope that by this method of treatment the same dimen- sions of bole can be attained in about 120 years as are obtainable in pure forests worked with a rotation of 200 to 240 years, provided that up till about the hundredth year the rate of increment has been maintained at 3 to 3! %, and after that at 2 to 2\ %, conditions which are quite conformable with the actual results obtained on suitable soils. The crop of Oak 1 Aus dent Walde, vol ix., p. 80. 2 Op. fit., p. 574- 226 Studies in Forestry [CHAP. x. then ultimately harvested numbers about thirty-six to forty- eight stems per acre, which on good soil yield valuable and remunerative assortments of timber \ Where soil and situation are good enough to fulfil the demands made on them, there can be little doubt that this system of underplanting with a shade-bearing species, and partially clearing the main crop from time to time, is the method best calculated to produce timber of the highest value for technical purposes, and to yield the most favourable returns financially from the capital repre- sented by the soil, together with the growing crop. Scots Pine. — For the practice of this method a good deep soil is necessary, as it differs essentially from the custom, common on poorer qualities of soil, of thinning out crops during their twentieth to fiftieth year of age and underplanting them with Spruce or other suitable shade-bearing species. In the latter case they are often allowed to grow on to maturity without any further thinning or interruption of the canopy to speak of; but, though they continue to improve in growth and form, this is due to the beneficial influence of the undergrowth both on the soil and the standards. As a good formation of the crown is requisite for Scots Pine, in order to enable it to continue for a long time in active energetic increment, thinnings should be made towards the end of the pole-forest stage of growth, and afterwards repeated whenever there seems any danger of the crowns interfering with each other. Under- planting should also be here carried out as soon as the thinnings have taken place with a view to the formation of 1 The following passage from London's work already quoted (p. 1809) is interesting, although not quite intelligible as regards the largest scantlings being produced at 130 years of age — though if larger be read in place of the largest the statement readily becomes intelligible : — ' A writer in the Gardener s Magazine states that Mr. Larkin, an eminent purveyor of timber for ship-building, stated, when examined before the East India Shipping Committee, that, in situations the most favourable for ship timber (the Weald of Kent, for example^, the most profitable time to cut Oak was at ninety years old ; as, though the largest scantlings were produced at 130 years' growth, the increase in the forty additional years did not pay 2 per cent. (Card. Mag. vol. xi. p. 690.)' CHAP, x.] Stimulation of Increment 227 good individual crowns. By this means, in place of having a pure forest formed, according to Weise's Yield-Tables \ on soil of average quality at eighty years of age by 317 stems per acre (having a mean average girth of 29 inches at breast- height, which would only be attained by about 40% or 127 stems, with a form factor of 0-45 and a current annual increment of only 44 cubic ft. per acre), it can hardly be doubted that a smaller number of trees with enhanced incre- ment and the finer dimensions of stem effected by the com- paratively rapid thickening of the bole at the top end must yield more favourable financial returns on the capital invested in timber production. Reliable comparative data are, how- ever, unfortunately not yet available to illustrate this point. Larch. — In regard to general treatment by partial clearance with a view to the speedy production of large-girthed timber, the Larch has much in common with the Oak ; but the under- planting may sometimes take place more advantageously with the Silver Fir than the Beech. So far as experience goes, this method of treatment is well adapted to the cultivation of the Larch on good, deep soil ; and it is most satisfactory when the partial clearance and underplanting takes place as early as the twenty-fifth to thirtieth year. When the previous tending of the plantations has been good, and the thinnings have been regularly made, the main partial clearance can be heavier than in the case of the Oak, so that subsequent clearances are often almost unnecessary. On good soil from sixty to seventy trees per acre may remain to form the final yield of the standard crop ; and wherever soil and situation are at all suitable for the growth of Larch, sixty- or seventy-year-old crops can often yield an increment of 3 to 4 % up to that age, when they should already show very good marketable dimensions. As the Beech is not in favour or demand as a timber-tree of large dimensions, this method is only apt to find any practical 1 Yield-Tables for the Scotch Pine, translated by W. Schlich, Ph.D., 1888, pp. 18, 19. - Q 2 228 Studies in Forestry [CHAP. x. application with the Spruce and the Silver Fir among shade- bearing genera ; and as they show many points of similarity, these two trees may be considered together. Where, however, there is any likelihood of windfall or damage from storms, this method is totally unsuited for the Spruce. Spruce and Silver Fir. — The way towards partial clearance should be paved by preliminary operations carried out about the twenty-fifth to thirtieth year in such a manner as to let the predominating poles have a clear space of 2 or z\ ft. around the crowns. These favoured individuals should stand about 15 to 17 ft. apart, all the rest of the crop being thinned out in the ordinary manner customary in pure forests without inter- ruption of canopy. During the thirtieth to fiftieth year, when the influence of this measure has made itself apparent in the re-formation of close canopy, the main partial clearance takes place in a somewhat similar manner. The stems between the favoured individuals should be freely thinned so as to permit of the formation of an undergrowth either naturally, or where necessary artificially, wherever the minor portion of the crop is of itself insufficient to protect the productive capacity of the soil. When the favoured stems have at breast-height a girth of about 36 to 40 inches, which they should attain between the sixtieth to eightieth year, the marketable trees can then be gradually cleared away on the same principle. Another method, practised in the neighbourhood of Salzburg in Western Austria throughout mixed forests consisting of Spruce, Silver Fir, and Beech, consists in carrying out the thinnings once every ten years after the crop has attained thirty years of age, and in making them heavier each time the opera- tion is repeated, until the main partial clearance is made about the sixtieth or seventieth year, leaving 120 to 160 stems per acre, all of them conifers and in energetic growth. Under such a crop natural reproduction can easily be effected, so that about twenty years later the standard trees are of large market- able dimensions, whilst the young growth may vary from CHAP, x.] Stimulation of Increment 229 5 to 15 ft. in height. On the removal of the standards the blanks thus formed in the new crop can easily be filled up artificially, and may be advantageously utilized for the forma- tion of mixed forests by the introduction of other species. Actual measurements of crops thus treated are not yet available for comparison with the yield-tables published for pure forests ; but the approximate data already given may be contrasted favourably with the more accurate information con- tained in these latter. According to v. Baur, pure forests of Spruce of 120 years in age and growing on good soil have 288 stems per acre, the mean girth of which at breast-height is 39 inches, but this is only attained or exceeded by about 40 % or 1 1 5 stems ; the mean average stems have also been found to have a form-factor of 0-48, which is undoubtedly lower than that of stems treated by the method of partial clearance. Again, according to Lorey, the Silver Fir, when grown in pure forest on good soil, yields 200 stems per acre with a mean girth of about 52 inches at breast-height, which also is only attained by about 40 % or eighty stems per acre. As has already above been pointed out, this method of partial clearance with the distinct object of stimulating the remaining crop to the speedy development of the larger and more valuable assortments of timber cannot be successfully attempted with 'regard to any species of tree when once its natural energy of growth has practically abated to any con- siderable extent, or on the poorer classes of soil ; but wherever the trees are still capable of stimulation in respect to incre- ment, and the productive capacity of the soil can be easily safeguarded against deterioration, the method has decided practical advantages which should strongly recommend them- selves to the woodland proprietors of Britain, where sylvi- cultural operations on any extensive scale should only be conducted on strictly financial principles. CHAPTER XI THE PRACTICAL EFFECTS OF UNDERPLANTING THE conservation of the productive capacity of the soil is one of the first fundamental principles of Sylviculture ; for the sustained yield of the best classes of timber can only reasonably be expected when measures are taken to safeguard all factors determining the quantity or quality of the food-supplies avail- able for the root-systems. One of the first practical steps in this direction consists in the protection of the soil against insolation, and against loss of soil-moisture, by means of the maintenance of a good, close leaf- canopy and the consequent thicker layer of dead leaves. This both forms humus or mould for the benefit of the soil, and also acts mechanically to prevent evaporation from drying winds. Beech, Spruce, Douglas and Silver Firs, and Black Pines — species of trees that are densely foliaged and therefore naturally capable of bearing shade well — are endowed with good soil-protective qualities throughout the whole period of their development until they attain their technical and financial maturity ; but most of our other valu- able forest trees, Oak, Ash, Maple, Birch, Larch, and Scots Pine, lose their power of conserving the productive capacity of the soil long before they attain their maturity, owing to the natural demands they exhibit for increased growing-space and relatively greater coronal development when once they have nearly completed their main growth in height. These latter species, in fact, prove themselves light-demanding in place of CHAP, xi.] Effects of Underplanting 231 shade-bearing ; and, if measures are not taken to counteract the consequences of the gradual interruption which takes place in the leaf-canopy, the effects of insolation and of exposure to the freer action of wind and rain on the soil, tend to diminish its productive power, and must ultimately lead to its deterioration. To obviate the consequences of this natural tendency on the part of the lightly-foliaged species, which is not reconcil- able with the conservation of the productive energy of the soil, the best plan capable of adoption is to underplant them with shade-bearing species for the purpose of maintaining the soil cool and moist, and of improving it through the larger quantities of mould formed by their dead foliage. In most of the open forests of Oak, Larch, or Pine, for example, there will usually be some sort of natural undergrowth found under the comparatively light shade of these forest trees ; but the practical influence exerted by an underwood of brush- wood, scrub, or berries, is by no means so beneficial as that of undergrowth formed either naturally or artificially by Beech, Hornbeam, Sweet Chestnut, or Sycamore — or by evergreens like Spruce, and Silver, Douglas, or Nordmann's Firs l. The first occasion on which underplanting is known to have been carried out under Oak, with the express intention of 'giving a covering of dead foliage to a soil already overgrown with whortleberry, and thus strengthening its productive capacity, and stimu- lating the diminished increment of the Oaks,' took place in the Spessart forest in central Germany about 1 Under Firs are included only the genera Picea, Abies, Tsuga, and Pseudotsuga, including Spruce, Silver Fir, Hemlock, Nordmann's, Menzies, and Douglas Firs, but not the Pines (Pinus) incorrectly though perhaps more commonly called Firs, e. g. Scots Fir for Scots Pine. Etymologically, Fir is properly the name of the Scots Pine, from the old Anglo-Saxon/~z