J'^Oj/c Vo / X Tut?' i / y<%u£cxc h <^) \ fi. V. )h% . /Yew Qi\/?tz> . ON THE MAURITIUS, BY CAPTAIN J. R. MANN. To L. BOUTON Esq., Secretary Royal Society of Arts and Sciences. My dear Mr. Bouton, I send you the paper we were speaking about yesterday. I am afraid you will find it more bulky than valuable, but if you think that it is not likely to interest the members of the Society, pray destroy it or do what you please with it. Yours very truly, J. R. MANN. 7th February 1860. OBSERVATIONS ON THE WATER SUPPLY OF MAURITIUS. The subject of Wood and Water has been much written and spoken about, but the question does not seem to have been yet exhausted. No great variety of opinion has been elicited on the subject ; most of those who have the want of a better supply of water have made up their minds that the Forests must be in one way or other preserved, yet the public opinion is far from being decided upon the manner in which this should be done, or as to the extent to -which the princi- ple which has been so generally admitted, should be carried out. In this, as in other cases, there are two sides to the ques- tion, and besides those who are calling out for more water* there are many who are wishing for more sugar. On one side of the question are those who connect the destruction of Fc ests with the cessation of rain, and on the other side those (who perhaps happen to be proprietors of Forest lands fit for culti- vation), who are anxious to clear and plant canes, either dis- believing or disregarding the popular theory of the connexion between the existence of Forests and the fall of rain. The object of the following observations, is to bring toge- ther some of the considerations bearing upon the question of water supply ; in the hope that some help, however slight, may be thereby given to the determination of the principle which should be our guide. — 64 — The endeavour to follow out to precise mathematical results the phenomenon of rain, would be met by at least as many difficulties, as would a similar attempt, in the case of any other of the natural phenomena. The great number of agents at work in the production of rain, and the manner in which they act and re-act upon one other, each being at the same time influenced by local cir- cumstances in an infinite variety of ways, makes the pheno- mena of atmospheric condensation extremely complicated. For instance, suppose the process to have just commenced, by the influence of a cold mountain summit upon a warm and humid atmosphere, the first step is the transformation of the vapour into the watery vesicles of which clouds and fog are composed, simultaneously the latent heat of the condensed vapour becomes sensible, and is distributed around, tending to check the energy of the scarcely begun process. Then, the opaque clouds assumes a power which the transparent vapour had not ; — it becomes capable of losing heat by radiation, as well as of intercepting the radiant heat coming from the sun or earth, or neighbouring clouds. Again, the two component parts of the atmosphere, name- ly the aqueous and the dry, have different affinities for heat ; that is they are not equally affected by the same increment or decrement of temperatui*e, so that when a change of tempera- ture takes place a disturbance of their relations ensues, and each component part of the atmosphere acted upon, has to go and seek a new place of equilibrium in the vertical column. Besides all this, the act of condensation is accompanied by electrical action, which no doubt introduces new modifications into the result. Thus each step of the process causes the introduction of new agents to the work ; all acting upon one another and tending to modify the energy of action of each of the forces in play. Of course, there is nothing like chance, or accident in the ever changing action of these mingled forces ; they are all wonderfully adjusted so as to produce a result beneficial to man, namely, a well regulated supply of rain. Each of the agents mentioned, and perhaps many others of which we are ignorant, works in its appointed course, performing with un- erring certainty the precise amount of work allotted to it; all of them together contributing to a result so unfailing that it might be expressed by an algebraic formula, did we know perfectly the whole of the influences at work, and the laws by which their varying energies are regulated. But though we cannot hope to reach a mathematical deter- mination in so complicated a process, yet we may with toler- able certainty foretell, in general terms, the result of certain given conditions ; by considering one by one, the most active of the known causes of atmospheric condensation, and tracing the probable manner and amount of influence exercised upon each, by the conditions stated. The chief, if not the only way in which forests and vegeta- tion in general, can affect atmospheric condensation, in the formation of rain, must be through their influence upon the temperatui’e of the soil. . Close vegetation affects the temperature of the soil it covers in two ways. Firstly. — It causes the evaporation of moisture, and con- sequent cooling of the surface of the ground, to proceed slow- ly, and continuously ; instead of allowing the direct rays of the sun to first dry up such moisture suddenly, and then to raise the temperature of the ground to a high degree : so that in this respect the tendency of the vegetation is to keep the temperature of ground it shelters lower than that of ground exposed and bare. Secondly. — Vegetation acts precisely in the same - manner as a clothing of a bad conducting medium; preventing the communication or loss of heat ; so that it checks variation of temperature, and tends to keep the soil at a mean degree of heat. During the hot part of the day, ground so protected will be cooler than a naked surface of rock or earth, but at night it will in general be warmer. On the one hand, the foliage will prevent the full force of the sun’s rays reaching the earth ; the intercepted heat being returned into space, partly by re- flection from the surfaces of the leaves, which in tropical plants are often highly polished ; and partly by radiation from 66 those portions of the plants which have received any heat. On the other hand, whatever heat which finds its way to the soil, is there preserved by the vegetable covering from loss by radiation, a process by which exposed surfaces are reduced to very low temperatures, when the sun is below the horizon. We may therefore conclude, that as a general rule, the tem- perature of ground protected by forests, will be within the extremes of temperature reached by exposed surfaces ; and further that the mean temperature of the sheltered land will be rather below that of the other. Now, the following are the most important of the recognized causes of atmospheric condensation. First. — The mixing together of bodies of vapour having different temperatures. Second. — The rising of vapour from low to higher aud colder strata of the atmosphere. Third. — The increase of pressure. Fourth. — The cooling of clouds through the effect of radia- tion. The first mentioned of these causes, namely the mixing to- gether of vapours of different temperatures, is no doubt a very common cause of rain. The condensation in this case results from the law by which the capacity of the air, for holding moisture in suspension increases and decreases more rapidly than the temperature ; so that when two masses of air satur- ated with vapour, at different temperatures, have been mixed’ the total quantity of vapour is necessarily greater than the mean temperature can support, and the surplus is thrown down as rain. If the masses of air are not sufficiently satur- ated to cause rain, the effect of the mixing will be to increase the degree of humidity, and perhaps to form light clouds or mist. In this operation the different masses of air are brought to- gether by some of the numerous causes of disturbance always present in the atmosphere, such as the meeting of different winds; sometin es perhaps differences in the electric state of clouds; the action of rotatory storms; and the variations in temperature of mountain masses, caused by the change of po- sition of the sun. - 67 — We have frequent opportunities in Mauritius of observing the operation of some of these processes, and especially of the last mentioned. Daring the heat of the day, the Trade wind is often met, and partly overpowered by a sea breeze, drawn towards the island from the Westward, by the upward current of air, caused by the great heat of the mountain masses. The transparent air allows the sun’s rays to pass through it with- out intercepting much of their heat ; but the earth on which they fall is quickly raised in temperature ; and it then imparts heat, by actual contact, to the air brought near to it, which at once expands and rushes upwards. From this cause we may often see the phenomenon of a Westerly wind in the Harbour and neighbourhood of Port Louis, at the same time that the Trade is blowing over the flat and windward parts of the Island. At such times the mixing of the two winds is accom- panied by clouds and mist ; sometimes presenting the ap- pearance of heavy banks of clouds, driven back by the wind from the sea, and heaped up above the Island, until their ele- vation brings them again within the influence of the Trade wind. The clouds are more or less dense, according to the degree of humidity of the air, and in general they deposit rain ; the horizon to the Westward being all the time clear. In the evening the mountains cool, by radiation, the up- ward draught of air ceases, and the clouds disappear, or seem to be swept away by the trade. The exciting cause in this operation is evidently the variable temperature of the earth, in relation to the surrounding air. The transparent air cannot receive heat from the sun’s rays, nor part with it by radiation ; the air can only be affected by actual contact with bodies of a different temperature, whereas the earth is soon treated by the sun, and as readily cooled by radiation, when the sun is not in a position to act upon it. There is only one way in which forests can affect the cau- ses which bring together different bodies of air, that is through the influence they exercise upon the temperature of the soil ; but from what has been said upon this subject, it is clear that the forests will in no way assist the process, but will rather tend to impede it, by preventing those changes of tempera- ture which give rise to the opposing currents of air. t — 68 — The second cause of condensation which has been men- tioned, is the rising of vapour from low to higher and colder strata of the atmosphere. In Mauritius, the formation of the ground causes frequent illustration of this process also. The saturated winds which come to us along the surface of the sea, are pushed, as it were, up an inclined plane, until the masses of vapour have reached great heights, (1400 to 2000 ft.) in passing over the elevated lands in the central parts of the Island. The greatly increased cold, due to the elevation, condenses the moisture and produces rain in great abundance. By way of example, let us suppose the air at the sea level to be saturated ; with the Thermometer at 85 ° and Barometer at 30 in : and that on the high lands of the interior the Ther- mometer is at /5 ° and Barometer at 28.8 in: Under these conditions, each cubic yard of the atmosphere at the sea level would contain in the form of vapour, 1.34 cubic inches of water ; though when expanded by the diminution of pressure from 30 inches to 28.8 inches, at the high level, each cubic yard of the atmosphere would only contain 1.31 cub. in. of water ; but simultaneously with the diminution of pressure at the high level, the temperature will be there reduced to 75 ° at which temperature, each cubic yard could support in a state of vapour only 0.995 cub. in. of water, so that the dif- ference, namely 0.315, or nearly ^ of a cub. in. of water must be thrown down, in the form of rain, from each cubic yard of the atmosphere which passes over the high land. This is no doubt a favorable instance, for the air as the sea level was assumed to be saturated, which will not often be the case ; but the example nevertheless serves to shew the depen- dance which may be placed upon the source of rain under consideration. It will be seen that the quantity of rain will depend upon the degree of humidity of the wind, and upon the difference of the temperatures of the lower and higher levels, and that it is altogether independant of the action of forests. The rain drops due to the increased cold, have their origin at a great elevation above the ground, and altogether beyond the in- fluence of the trees the rain drops increase in size, gradually, — 69 — as they descend, partly on account of their originally low temperature, which enables them to condense additional moi- sture as they fall ; and also on account of their power of col- lecting by attraction the smaller watery particles amongst which they pass, in the same manner as a globule of mercury may be seen to attract to itself and agglomerate the smaller particles brought near to it. It is from these causes that a rain guage placed on the ground collects a much larger quan- tity of water than on top of a tower. Another way in which vapour is raised from low to higher strata, is by the ascending currents already spoken of, caused by the heating of mountain masses. An extensive conflagration, likewise, often causes such an upward draught, that masses of vapour, after having been heated and expanded, rise to great heights, where the tempo- rary accession of heat is lost, and much of the moisture con- densed. Those who have witnessed extensive fires may have noticed the irregular gusts of wind approaching from all quar- ters, often accompanied at intervals by light showers of scat- tered drops of rain. There can be little doubt that ascending currents take place during rotatory storms, and it is perhaps to this circumstance that the lowness of the Barometer in the vortex is due. The third cause of rain which has been referred to is in- crease of pressure. If the air be saturated, any increase of pressure, when un- accompanied by increase of temperature must cause conden- sation of moisture. Variation of pressure may result from atmospheric chan- ges, though in this case, within such small limits that it can be scarcely considered an active cause of rain, in itself ; though it may assist or retard the action of other causes. Increase of pressure may also take place when a strong wind, saturated with vapour, strikes with unbroken force against a mountain range, sufficiently abrupt and extensive to arrest the onward motion of the air. In such a case, increase of pressure will be caused, and maintained by the cons v/c motion of the wind, which continues to arrive faster than the - 70 - compressed air can escape, by rising and passing over the mountain. The great quantity of rain observed to fall on the Wind- ward side of mountain ranges, in many parts of the world, has been attributed to the cause described ; but it seems pro- bable that the actual increase of pressure has had less to do with the result than the circumstance that the vapour was forced to ascend to cold altitudes, before it could escape over the mountain ; also the air must frequently suffer a loss of heat, by contact with the mountain, which, by reason of the constant radiation will often be lower in temperature than the air. which latter maintains more nearly a mean temperature. ugh the idea is not without supporters, it seems to be naite out of the question that the slight impediment offered to the wind by a forest, or by a line of trees, can cause suffi- cient compression to produce rain ; the forest could only af- fect the motion of a thin stratum of air, allowing the chief mass of the wind and vapour to pass onward above, altoge- ther unimpeded, so that under the most favorable circum- stances, only a few drops of rain could be deposited, near the border of the forest. Neither could the amount of conden- sation resulting from the contact of the vapour with the trees, (supposing the trees to be colder than the air) be great, con- sidering how very slowly the air is changed in a forest, even when a strong breeze is blowing over the tops of the trees? and consequently how very small a portion of the vapour which supplies us with rain is ever brought into actual con- tact with the trees. The fourth cause of condensation and the last which it is necessary to consider, is the cooling of the clouds through the effects of radiation. When once an opaque cloud has been formed, their radia- tion commences, and the cloud is constantly parting with heat, and at the same time intercepting heat from other bo- dies ; the loss may often exceed the gain, and the consequent increase of condensation will cause the rain to fall. The general eff ect of forests being to impede radiation from the earth’s surface, the presence of the vegetation would be in most cases favorable to the cooling of the clouds ; but as the 7i — total supply of rain from this cause alone cannot be very great, the trifling increase of quantity clue to the action of the for- ests cannot be worth taking into account. It may be said that trees have some influence upon the electric condition of the atmosphere, but to what extent the quantity of rain may be modified in consequence, it is not easy to determine ; it is generally considered, however, that electric changes are more often the consequence than the cause of condensation. Now as there is no cause of rain which may not be traced ultimately to one, as to the combined action of several of the processes which have been mentioned, it seems sufficiently clear that the extent of the forests has very little to do with the actual quantity of rain. It will be seen, further, that the permanent physical condi- tions under which the Island of Mauritius is placed, render it positively certain that large quantities of rain must fall, whe- ther forests exist or not. We have huge masses of rugged mountains, supporting elevated table lands in the centre of the island, the whole surrounded, to a great distance in every direction, by an ocean, yielding a constant and enormous sup- ply of vapour, under the influence of a tropical sun ; it neces- sarily results from these conditions, that from which ever di- rection the wind arrives, it comes in a very humid state. ’ almost always at a high temperature, such winds must t > - sit rain when passing over the elevated and cold parts of the island. It would have been very interesting to have procured re- liable statistical evidence shewing the quantity of rain that hasffallen at different periods, during a long series of years but that has not been possible, and it would require many years of carefully conducted observations, made simultane- ously in different parts of the island, to enable any positive deductions to be made from that source, as to the relation be- tween the extent of forests, and the quantity of rain. As far as the evidence of former legislation may be taken, it would appear that a periodical scarcity of water has always, from the earliest times, seemed to be quite as imminent as it is now ; and at very distant periods measures have been taken - 72 - or recommended, for preventing the cutting of timber, for the sole purpose of ensuring a sufficient supply of rain ; but though these measures have been ineffectual, and an immense amount of clearing has been done within the last 60 or 70 years, there is not the slightest ground for supposing that any change has taken place in the quantity of rain which falls in the course of a year. So far back as the year 1771? it was found necessary to un- dertake the construction of the Bois Rouge Canal, a work of great magnitude, for the purpose of conveying water from the upper part of the Riviere du Rempart to the flat and North- ern parts of the Island ; and this great expense was incurred to supply the wants of a population probably less than one tenth of what it is at the present time. In the year 1810, the British troops suffered great hard- ships on account of the want of water, whilst penetrating the thick forests which then extended nearly the whole distance from Grand Bay to Port Louis ; and the expressions of Ge- neral Abercrombie’s Despatch imply that the deprivation of water was not a temporary or accidental occurrence, but that that part of the Island suffered from a permanent scantiness of supply. The formation of the ground moreover, proves that no streams, besides those now in existence, have ever traversed that part of the country. In comparing the quantity of water now in the rivers with what is stated or supposed of their condition at some distant period, allowance must be made for the enormous consump- tion of the present day caused by the great increase which has taken place in the population of the Island, and in the extent of cultivation. We must expect to find less water in the rivers when we consider the number of extensive planta- tions crowded along their banks, and remember the great num- ber of men and animals to be supplied, and the large quanti- ties of water made use of in carrying on the improved processes of manufacture and cultivation. The simple recollections, or general impressions of persons, on the subject of the effect s of clearing, upon the water supply, arc very likely to mislead. For instance, the assertion that a cer- tain stream had never before been dry, at that particular sea- ~ 73 son, does not prove the quantity of rain to have diminished; the average flow of water may be unaltered, although a diffe- rent distribution of the total quantity may have taken place, between the several seasons of the year ; and with respect to general impressions on the subject, they would no doubt be in general, founded on the circumstance of the two conditions of abundant moisture and luxuriant vegetation being com- monly found together; the effect being mistaken for the cause, and the plentiful rain being considered the consequence of the very vegetation which it has produced and nourished. Mauritius revels in all the conditions necessary to exube- rance of vegetation. With a fertile soil, a genial sun, and a humid and stimulating atmosphere, it is inconceivable that the conversion of the humidity into rain should be the only thing to continue wanting for the completion of one of the great works of Providence, namely the preservation and mul- tiplication of organic life, in the vegetable creation. We can- not suppose the laws of nature to have been so disposed that rain is forbidden to fall until some human hand shall have first planted and noui’ished trees to invite it. Such a theory would be altogether contradicted by the wonderful systems of self-regulation and compensation which may be observed in all the operations of nature. The foregoing considerations seem to shew conclusively that trees have little or nothing to do with the quantity of rain, and that Mauritius will always receive a fair and suffi- cient supply, whether forest exist or whether they be swept away altogether. The real value of trees, in connexion with the water supply, consists in their power of preserving and husbanding the rain water after it has fallen. When rain falls upon land not sheltered by forests, it rush- es down the slopes of the ground, at once, without opposition, to the water courses ; they are suddenly swelled into torrents, but will soon be left dry, as before. The very small quantity of moisture which has time to pe- netrate into the parched ground, or which remains upon the surface, is quickly dried up by the sun, and the water courses - 74 - will receive no further contribution until the fall of another shower. Where forests abound, the case is different. The rain is received by a soft and spongy soil, chiefly composed of de- cayed leaves, mosses etc. ; it is there preserved from evapora- tion hv the shade of the trees, and as it cannot rush down the surface of the slope with great velocity, time is given to the water to soak well into the ground, which it penetrates to a greater of less depth, according to the nature of the soil. The water is then collected and drained away gradually, according to the arrangement of the subjacent strata, or the formation of the rocky bed upon which the vegetable covering and po- rous strata lie, and the water ultimately contributes a well re- gulated supply to the rivers, often shewing itself as a spring at the side of a mountain slope, or even on a plain, at a con- siderable distance from its origin, and wherever the course of the hidden natural drains may lead it. Sometimes the gradual soakage from the higher levels is stopped by hollow or flat formations of the ground, where the water accumulates and forms marshes or lakes, which serve as reservoirs, for the regular supply of constantly flowing- streams. Mauritius abounds in examples of these processes. On the shoulder of the Pouce mountain is a constantly run- ning spring, which is due to the gradual draining oft’ of the large quantity of moisture received from the atmosphere, by the cool summit of the mountain, all the year round. Were all the vegetation stripped from the mountain top, it would ne- vertheless continue to receive from the atmosphere as much moi- sture as hefoi'e ; hut the spring instead of producing a nearly regular and a constant flow, would become intermittent, and would be sometimes dry and at other times overflowing. The Table lands of Yacoas and Savanne also furnish illu- strations of a good deal that has been said. These lands on account of their elevation * receive a great deal of rain from * The approxim. altitude above the sea of Mare aux Vacoas is 1706 feet. ,, ,, „ of Grand Bassin is ... 1978 „ ,, „ ,, of Bassin Blanc is ... ,, „ ,, of the highest part) of the ridge between Grand Bassiu and Bassin Blanc j 1360 2279 tlie humid winds which pass over them from the sea level. The water is collected and preserved in extensive marshes and lakes, whence are derived the sources of three considera- ble rivers : the Riviere Tamarin, the Riviere du Rempart and the Riviere du Poste, and whence a gradual but constant sup- ply of water is furnished at all seasons of the year. The pro- gress of cultivation, and the demand for timber are quickly bringing about the clearing and draining of these lands ; when once they have been cleared and cultivated, the con- stantly flowing streams already somewhat reduced during the dry season, will undergo still further change, and in their place will be seen swollen torrents in rainy weather, and dry chan- nels during the rest of the year. Now such being the real action of forests in connexion with the water supply, it follows that we must either maintain our forests, at any cost, or adopt artificial means which may serve the same purpose, in the preservation of the rain, after it has fallen. The choice between the alternative courses open to us will not be difficult, for it is easy to see that it will be utterly im- practicable to maintain any sufficient extent of forest land, whereas there will be little difficulty, and ultimately less ex- pense, in establishing artificial reservoirs. The forest laws now in force affect a very small portion of the existing forests ; and yet if we are to depend upon forests for the preservation of the water it is clear that present ex- tent of forest land must not only be reduced, but must be added to ; for the call for more water has long been heard, during the dry season, and it will certainly become more and more urgent, with the increase of population. All the advocates of the forest system acknowledge this ; and though no one has been bold enough to advocate the to- tal prohibition of any further clearing of forest lands, yet it has been proposed to add to the extent of forests under the protection of the laiv by requiring each proprietor to set aside a certain proportional part of his land for the purpose, so as to divide the burthen equally amongst all. But such isolated patches of trees, scattered about the Island could have no appreciable effect upon the water supply ; not only is it ne- 76 - cessary that the forests be massed together, on a large scale, to be of any service, but the forests which should be preserv- ed are those particular forests of Moka, Plaines YVilhems, Vacoas and Savanne, and no others will answer the same pur- pose. It would be useless to establish forests about the low- er parts of the rivers and at the same time leave the sources naked and exposed. The forests must be regarded as reser- voirs, and as by far the greater part of the rain falls on the high lands, the forest intended to preserve it must be placed there, and not on the low ground ; for by the time the water reaches the low ground it will have been collected into large streams, having velocity sufficient to rush onwards to the sea, no matter whether it has to pass through forests or not. A reservoir placed near the mouth of a river would merely supply a small quantity of fresh water to the sea, but if placed around and about the source, it would give a large and regular supply to the whole line of country through which the river might flow. Nothing short of a positive prohibition of all future clearing on the high table lands before mentioned, will meet the views of those who trust to forests, for the maintenance of the water supply, but if these lands are to be protected by law, they must be purchased from the proprietors, and doom- ed to be forever unprofitable. Considering the extent and the value of the land, such a measure would seem both impolitic and impracticable. If we wish the Island to advance in ma- terial prosperity, we must adopt an opposite policy, and find means to throw open to cultivation as much land as pos- sible. As facilities and inducements for extending cultivation in- crease, so will the impracticability of maintaining so much forest become more evident. A simple calculation will show that each individual of the population must use something like one cord of brush wood or other fire wood in the course of a year ; in all about 240,000 cords; taking the produce of one acre of land at 75 cords, the consumption will be equivalent to the produce of 3,200 acres every year. Now it is probable that more than this quantity of fuel is consumed at the various Sugar Manufactories, Di- stilleries, Lime Kilns etc., and probably as much more is used annually for various building purposes, so that it does not seem unreasonable to conclude that in one shape or an- other wood, equivalent to the produce of between 9,000 and 10,000 acres is cut every year; land so cleared, must be con- sidered as permanently abstracted from forest land. Now if forests are to be kept up, this enormous amount of clearing must be stopped altogether, and those who advocate the measure must be prepared not only to pay indemnities to the proprietors of the forest lands, but also to throw upon the colony the immense expense of substituting other fuel, and other timber for building purposes, in place of the fuel and timber now used. But even when left to themselves, and when no active steps are taken for their destruction, there seems to be a gi’adual decay of the forests, which it is difficult to explain. The number of dead trees in some of the most important forests is very great. It may be that the soil is exhausted of the nourishment required by that particular description of tree, and that some other species of vegetation may hereafter spring up, to take the place of the dead trees, but at present there are no signs of such a process having commenced. A parti- cular kind of long grass is the chief species of vegetation which at present flourishes near the dead trees. In fact it seems certain that everything deserving of the name of Pempirisme a tous les droits possibles ; mais ea verite, que peijser de Peffet de certains simples reputes inoffensifs. quand ceux-la qui savent en tirer un si beau profit pecuniaire ne savent meme pas distinguer entr’elles les nombreuses affec- tions auxquelles ils les appliquent et qu’ils confondent sous le nom tant de fois prononce dans ce Rapport et par lequel nous terminerons : “ Tambave.” Dr. C. REGNAUD, — Rapporteur. Ph. B. AYRES, M. D. Dr. LEJUGE. INFLUENCE IMS GUANOES PLI IKS SIR LA VEGETATION. La note suivarate est communiquee par le Secretaire dans, la seance du 22 Mars 1860 : “ Les pluies abondantes que nous avons eues, et l’excessive chaleur qui s’est fait sentir pendant les intervalles ou a reparu le soleil, toutes conditions si favorables a la vegetation tropi- cale, ont produit sur les pi antes un developpement luxueux de rameaux, de tiges et de feuilles. ec En resume, c’est un grand bien, du moins il faut le pren- dre ainsi, quoiqu’il arrive parfois qu’a cote du bien se trouve le mal, occasionne souvent par la meme cause. “ Dans eertaines parties froides et elevees de Pile, les Cannes nous l’avons entendu dire, ont evidemment souffert de ce sur- croit outre mesure d’eaux pluviales. L’experience et les faits ont appris que dans les terrains ou le sol n’absorbe pas la quantite d’eau qui tombe et ou le soleil, cache par les nuages, ne peut l’enlever par l’evaporation, il survient chez la plante sejournant longuement dans un sol trop humide, une decolora- tion des feuilles qui pi’ennent une teinte jaunatre ; plus tard le tissu de la plante subit une decomposition dont la mort est la consequence indubitable. “ Cette couleur jaune, dit le Dr. Lindley, provient, d’apres quelques chimistes, de la destruction par l’eau d’une matiere bleue particuliere a la plante, laquelle melee de jaune produit la couleur verte naturelle a la vegetation. “ Dans quelques cas, quand Phumidite se prolonge, les ar- ticulations de la tige se separent ; dans d’autres cas, la plante pourrit dans la terre par les racines. Ces resultats varient en raison du plus ou moins d’affaiblissement de la lumiere et d’abaissement de temperature dans le sol. Decandolle est d’opinion que la quantite d’eau qui sejourne autour du collet de la plante, intercepte a l’oxigene de Pair tout acces aux yacines. Quoiqu’il en soit, trop d’eau peut nuire a la plante, soit en — 90 — produisant la decomposition dont nous venons de parler, soit en lui donnant des dimensions en dehors de ses formes et de ses habitudes ordinaires, et la transformant en monstre, phe- nomene dont bananas que je presente ici, est un exemple. “ On y voit le pedoncule principal -considerablement renfle vers la base, se subdivisant en d’autres pedoncules qui se bi- furquent, et se terminant par de tout petits fruits dont quel- ques uns sont soudes par leurs ovaires les uns aux autres. Ces fruits sont surmontes comme d’ordinaire par le bourgeon central ou couronne qui a pris un assez grand developpement. L’ensemble de toutes ces couronnes terminales a l’apparence d’une touffe de jeunes plantes sortant du sol. “ Un autre inconvenient peut provenir de cet exces de pluie et nous en avons vu des exemples. “ On a pu remarquer que certains de nos fruits a pulpe char ) nue, la mangue, par exemple, ayant perdu sa saveur accoutu- mee, avait, comme on dit communement, gout cVeau. Les melons gorges de sue aqueux en ont absorbe plus que leur etat physiologique le leur permet. La transpiration si neces- saire a la plante n’a pu s’effectuer dans les conditions voulues et les fruits se sont fendus, ou ont coule. c< C’est quand les fruits sont au moment de murir que les ar« rosemens doivent diminuer et cesser ; et le contraire a eu lieu ici: “ The quantity of water in the soil, dit Lindley dans “ dans son traite d’horticulture, should be diminished when “ succulent fruit is ripening. — Not only is the quality of such “ fruit impaired by a wet soil, but, because of its low perspi- “ ratory power, the fruit will burst from excess in moisture, “ as occurs to the Plum and Grape in wet season.” “ Les plantes a racines charnues et nutritives ont egalement souffert dans ce sens que toute la vegetation s’est portee sur les tiges et les feuilles qui se sont developpees d’une maniere prodigieuse au detriment des racines reduites a des lilets gre- les. On en a des exemples dans des tiges de patates qui se sont elancees comme de grands Convulvulus sur de jeunes ar- bres qu’elles ont entortillces et couvertes de leurs feuilles trop abondantes et trop touffues.” — 91 La Societe Royale des Arts et des Sciences s’est reunie mardi, 3 Avril 18G0 a la Chambre d’ Agriculture. Le but de la seance a ete la communication faite par l’hon. M. Fropier du Rapport qu’il avait ete charge de preparer sur l’Exposition Intercoloniale d’Aout et Septembre derniers. Le Rapport a ete ada>s plus par celui-ci que par celui-la. ulamrnent de ces principes elementaires et constitu- dans cette plante des matieres salines, do soude et de chaux a acides varies qui, lorsqu’on la brfde, constituent la majeure partie des cendres qu’elle laisse pour residu. Les matieres minerales out toutes ete puisees dans le sol, toutes sont egalement necessaires a la constitution de la plante. Quant aux aeides, ils peuvent changer a l’infini dc bases, ou etre reduits et remplaces par les aeides organiques que la vegetation engendre. II est done de toute necessite que les racines trouvent ces sels mineraux dans la terre, soit qu’ils y existent naturelle- ment, chose douteuse, puisque la canne les epuise, soit qu’on les y ajoute dans un engrais. Aussi, les engrais n’agissent-ils pas toujours par les matieres azotees qu’ils contiennent, mais encore par les sels qui y sont contenus, De meme encore la necessite d’employer des cendres qui, placees a propos, impri- ment a la vegetation languissante une vigueur, une activite que les engrais seuls ne pourraient lui communiquer. Le carbone, I’oxigene, l’hydrogene et l’azote sont les veri- tables aliments de la canne, comme ils le sont de toutes les plantes ; mais une fois qu’ils y sont entres, ils ne restent plus isoles les uns des autres. Par suite des phenomenes de la vegetation, il s’opere de nouvelles et de nombreuses combinaisons ; les elements de la plante en s’unissant deux a deux, trois a trois, ou meme tous les quatre ensemble, don- nent naissance a tous ces principes immediats qui y existent et qui s’y sont formes de toutes pieces par les seules for ces de la vegetation unies avec les sels, les oxides ou leurs radicaux reduits ; tels que soufre, phosphore, etc., seules ma- tieres qui soient empruntees par la plante aux milieux dans lesquels elle vit et se developpe. L’ Agriculture de Maurice laisse encore beaucoup a desirer ; il y a des proprietes ou l’on ne s’occupe pas des engrais pre- paratoires ; pourtant, un sol ne peut pas toujours produire, s’il n’a pas les elements voulus pour cet efFet ; je pourrai dire a ceux-la ce que le fameux cliimiste Liebig repondit aux pay- sans qui avaient ete le trouver pour s’enquerir aupres de lui, de la cause qui empechait leur sol de donner toujours les memes recoltes, qu’ils voyaient diminuer tous les ans.. “ Rendez au sol, leur dit ce celebre chimiste, ce que vous lui prenez en principes, et vous n’aurez pas de deceptions a la fin de vqs recoltes. ” Selon ma conviction, je dirai : Ne laissez pas votre sol s’epuiser en y laissant les souches de vos Cannes vieillir ; ne plantez vos Cannes que sur un bon engi’ais que — 9G — rous pouvez aisement fabriquer, car toutes les niatieres dont vous avez besoin se trouvent chez vous et vous les laissez perdre. Je ne citerai, a l’appui de ce que j’avance que l’etablisse- ment Bonne Mere, a Flacq. Get etablissement qui marclie en premiere ligne a Maurice et qui, avec le peu d’etendue de ses terres, donne de tres beaux produits, n’entreprend jamais de plantations que sur un bon purin, compose des detritusde la propriety ; l’herbe ne pousse jamais dans ses champs ; ses plantations sont achevees lorsque les voisins pensent a com- mencer les leurs. Aussi, quels sont les resultats qu’on ea retire ? Ils sont, au dire des personnes intei’essees, invaria- bles ; les terres s’ameliorent cbaque annee ; le meme sol/apres les deux seules coupes que Pon se contente d’y faire, est re- troue avant meme que les racines de la plante n’aient pu s’etendre ; peu apres, le carreau est replante et les Cannes y viennent toujours avec une vegetation nouvelle. Je vais maintenant vous parler de la propagation de la canne a Maurice. Les premieres plantations sont generalement faites avec de bonnes tetes ; plus tard on prend tous les plants,, quels qu’ils soient, pour les confier a la terre ; quelquefois, on va chercher au’ milieu des carreaux abandonnes, des Cannes epuisees par l’herbe, dans laquelle on les a laissees grandir pour les planter. Quels sont les rejetons de ces mauvais plants, que font-ils voir en se montrant au jour ? Des Cannes degenerees. Ce fait seul denote les taches de maladie qui out eu lieu dans plusieurs localites sur la canne Bellouguet et qui menacent cette espece d’une destruction prematuree. J’ai pense aussi a une chose qu’il est de mon devoir de si- gnaler a la Societe, afin que Pon puisse la mettre en pratique, si la chose est jugee convenable ; c’est de faire Pechange des tetes entre les quartiers secs et les quartiers humides. Je crois que cette alternation serait encore d’un grand secours pour empecher la degenerescence complete de la canne Bel- louguet qui est la scule, jusqu’ici, qui ait pu remplacer la canne blanche avec avantage, par sa ricliesse en vesou. La sommite de ces Cannes dans les quartiers humides est d’une belle venue, mais quelquefois trop tendre pour etre plan- tee dans le lieu qui lui a donne naissance ; car, pour peu. — 97 qu’il fasse pendant la saison une grande quantite de pluie, elle pourrit et la plantation manque ; car cette tete contient en elle assez d’eau pour que, alimentee par la chaleur atmosphe- rique des mois favorables a la plantation, elle puisse germer et faire la canne vegeter en attendant que ses racines puissent atteindre le sol et s’y nourrir. Au contvaire, dans les quar- ters secs, il arrive, lorsque le plant subit une secheresse, que la plantation manque ; parce que la tete des Cannes dans ces quarters ou la vegetation est tout-a-fait arretee lorsqu’arrive la coupe, est naturellement seclie et tend encore a secher par le soleil ardent sous lequel elle est nee ; e’est pourquoi je propose P alternation des plants, essai deja fait a Flacq, sur l’etablisse- ment Mon Reve et qui a parfaitement reussi. II est evident que les tetes tendres des quartiers bumides, plantees sur un bon fumier pousseront mieux dans les quarters secs, rechauf- fees par le soleil, et que celles des climats secs qui ne deman- dent que de la pluie, fructifieront mieux dans les conditions ou elles se trouveront. Quant a la question du Borer, les quartiers humides en seront toujours exemptes par les pluies qui les arro- sent, et ils diminueront dans les quartiers secs par les tetes saines que leur fourniront les quartiers eleves. D'ailleurs, la chose est prouvee par l’usage etabli en Europe de faire venir les semences d’Egypte, parce que ce pays produit de plus beaux grains, par le fait du renouvellement du sol et par les depots qu’y apporte le Nil pendant la crue des eaux et qu’il y laisse en rentrant dans son lit. De meme, la tete de canne des regions humides jouissant d’une vegetation continuelle est plus belle et promet de plus beaux resultats aux quartiers secs en y apportant ses premiers elements de vegetation, et la tete des quartiers secs, en retrouvant dans les quartiers humi- des les elements nourriciers dont elle a besoin. Ce moyen employe a l’unisson regenerera cont^nuellement notre espece de Cannes et la rendra exempte des maladies sous lesquelles la canne blanche a succombe. Pour abreger ce travail deja assez long, je vais vousrparler des engrais. Commenyons par l’engrais preparatoire qui doit etre forme par : 1. Les herbes de vos champs, pour rendre a vos terres les principes que ces plantes y ont puise. 98 — 2. Les produits de vos ecuries qui serviront a rendre au sol les substances qu’il a perdues, et qui sont fournis par la nour- viture que Pon donne aux mules, par leurs excrements et les urines qui imbibent les litieres et dont voici, d’apres deux chimistes, l’analyse telle qu’elle est donnee dans la chimie or- ganique de Liebig : Crottin de cheval ou de mulet. Urine de cheval ou de mulet. (Jackson,) Phosphate de chaux 5,00 Carbonate de chaux 18,75 Phosphate de magnesie... 36,25 Silice 40,09 100,00 (Vauquelin.) Phosphate de chaux 11 Carbonate de soude 9 Hippurate de soude 24 Chlorure de potassium... 9 Uree 7 Eau 940 1000 3. Les produits du pare a bceufs et de l’etable dont la com- position chimique est : Urine de vache. — ( Blande.J Chlorure de potassium et sel ammoniac 15 Sulfate de potasse 6 Carbonate de potasse 4 Carbonate de chaux 3 U rde 4 Eau 968 1000 Bouse de vache. — ( Haidhlen .) Phosphate de chaux 10,9 ,, de magnesie... 10,0 ,, de fer 8,5 Chaux 1,5 Sulfate de chaux 3,1 Silice et perte 66 100,0 4. Cendres a bagasse, ecumes de vesou, recouverts, dans la proportion d’un pied d’epaisseur, d’un pouce de chaux et noyes dans une lessive composee en meme proportion d’eau douce, d’eau salee et de sirop. Get engrais doit etre fabrique dans m bassin et ne doit stre employe que trois mois apres, pour donner le temps a l’acide acetique produit par la fer- mentation de se combiner avec d’autres substances pour for- mer des sels utiles a la vegetation ; deux ou trois livres de cet engrais suffisent pour un fosse. L’analyse de plusieurs echantillons de terre de differentes loealites m’a suggere l’idee de vous parler encore des engrais que vous employez dans vos plantations; il m’a fallu coinpa- — 99 rer l’analyse du vesou, celle du sirop, celle ilu sucre, pour me rendre compte de ce qui manque et des moyens d’y pourvoir. Generalement nos sols contiennent de la silice, de l’alu- mine, peu de silicate de chaux, peu de magnesie. Les par- ties hautes de Pile contiennent du fer en quantite notable, mais les parties du littoral ne laissent voir que des traces de ce metal. L’analyse de la canne varie en : Silice 40 V a 50 Acide phosphorique 3 a 9 „ sulfurique 5 V a 12 Chlorure 1 a 10 Chaux 4 V a 15 Magnesie 2 V a 16 Potasse 10 V a 28 Soude 1 V a 5 Cependant les terres de Maurice, a l’exception de la silice, ne peuvent guere fournir a la plante ces elements que vous avez tous chez vous et qui se trouvent en pure perte et qui fourniraient a la canne la nourriture dont elle a besoin. Peu de planteurs savent profiter de ces avantages, qu’il leur serait facile d’utiliser. Les herbes de leurs champs, les pail- les de leurs Cannes, les cendres, les sirops, les ecumes, voila des elements qui se perdent et qui pourraient leur rendre de grands services. I Is pourraient avoir des plateformes sur lesquelles seraient dresses en meules, tous les produits qu’ils pourraient reunir ; preparer des lessives composees de leurs sirops, d’eau salee, de chaux ' et d’ecumes de vesou ; l’arrosage par cette lessive hxerait les sels qui se perdent. Cependant on neglige de ras- sembler ces produits, qui formeraient une grande partie des substances dont la canne est composee et dont elle a besoin pour se nourrir. Les cendres conservees dans des endroits, a l’abri de la pluie, appliquees en Janvier ou Fevrier donneraient a la plante une vegetation luxuriante. Les charbons des usines joints au fumier imprimeraient une grande amelioration au sol, qui de- viendrait plus riche, pourrait facilement supporter les engrais commerciaux et doublerait la valeur des produits. 100 — Le sirop desseche produit environ cinq pour cent de cen- dres dont une partie est composee pour op de : Carbonate de potasse 30 „ de chaux 15 „ de magnesie 15 Oxide de fer 6 Chlorure de potassium 22 „ de sodium 9 Acide sulfurique . 3 100 Voila les matieres dont la canne a besoin pour se nourrir ce sont celles qu’il faut rendre au sol. Ne pouvant m’etendre plus longternps sur ce sujet, je me mets a la disposition des personnes qui auraient besoin de plus amples renseignements. Je prierai en terminant M. le President de faire un appel d MM. les planteurs pour leur demander des echantillons du sol de leurs proprietes, pris entre quatre et six pouces de pro- fondeur, ceux que j’ai eu et dont je fais connaitre plus bas la composition n'etant pas assez suffisants pour l’etude d’une question importante a P agriculture de Maurice et a la fabri- cation d’engrais speciaux. Analyse cl’un echantillon de terre de V etablissement Belle Mare sur lequel on venait de couper des\ Cannes de re- pousses. Alumine . . Silice . . Magnesie . . Chaux.. .. Fer . . 2(1 72 1,06 04 Trace ]<)<),()() — 101 Etablissement Argy. — Terre ev f riche. Silice 75 Alumine 10 Chaux 2,06 Magnesie 1,00 Humus 5,08 Fer 5 100,00 Ate. Paruit D’Esmery. « MW ZEALAND FLAX. (Communicated by Mr. Jm. Diore.) This plant is indigenous to New Zealand, and was known from the time Tasman discovered these islands in 1642. This fact is so true, that the New Zealand Flax is to be found throughout the land, both in the North and in the South. It is employed by the Natives (Maories) for the manufacture of their garments as well as for various packages in which they make up the Wheat, Gum, Potatoes, &c., which they grow for their bartery with the European settlers. The Natives equally make use of it for “ fishing Nets” and tc fishing Lines,” and is frequently exported to Europe where it is mixed with Hemp for the purpose of making Ropes. I have no doubt that this plant would be well adapted for making bags in which Sugar could be packed ; it being much stronger and more supple than the Vacoa, the brittleness of which is sometimes the cause of heavy losses to shippers and exporters. The New Zealand Flax will grow in any middling good soil, provided it be pretty well watered. The ordinary mode of planting it is to place three or four seeds in a hole of about eight inches in diameter and four in depth, covering the same with not more than one inch of soil, taking care, at the same time, to place the holes at a distance of three feet one from the other. When the shoot is suffi- ciently long, it should be earthed up in order to give it sup- port. The plant attains the height of seven feet two years after the sowing of the seed, at which time the leaves are fit to be cut; — and, after the first crop, every eighteen months; — but different from the Vacoa, it does not grow any branches, the leaves shooting from the stem out of the earth ; these leaves grow in a bushy (touffu) form and are abundant. When the leaves are cut, they are split like the Vacoa into — 103 proper widths and dried during two or three days by hanging- up in a shed or in the shade, (and not in the sun) previous to manufacturing the mats or packages. The Flax must not be too dry when manufactured, and cutting the same three days before employed will be found quite sufficient. Soaking the leaves for a couple of hours after drying in the shade, is also a great assistance for softening the fibres. The accompanying specimens of Native workmanship, namely : 1 . A war cloak, 2. An ordinary cloak, 3. A kit (Maorie name for a bag), will give an idea of the use made of the New Zealand Flax. Having resided during a period of five years in New Zea- land, and returning to my native land, I ventured to import a small quantity of this seed with the view of demonstrating its utility for agricultural purposes, and, shall be satisfied if a trial thereof should prove successful. In conclusion, I may mention that this seed is abundant and easy to be procured. •»»>>» London, 19th November 1860. To the President and Gentlemen of the Royal Society of Arts and Sciences. Gentlemen, Nothing but confusion exists in the accounts of the early navigators in reference to the islands now called Bourbon and Mauritius, a ad there is even no authority for proving that they were discovered by the Portuguese at all ; though if di- scovered by them it was decidedly not in the first year of the Governor Almeida in India, as is clearly proved by the ex- tracts from the works of Faria Y Souza already transmitted to the Society. Nothing is clearly distinguishable until the first real settlement on the island of Mauritius by the Dutch under Van Neck in 1598. Grant is the authority for all the subsequent English writers on the subject who copy his pages without any trouble whatever to verify his statements ; but it is quite clear that Grant had no oi’iginal documents to consult for the early Portuguese portion of his history. So with the French writers ; even in the excellent map Afrique published by Sanson in 1674, the island is put down as “ lie Maurice ” though at that date it could only be known by the name of Cirne or one of its many corruptions, as it was not until 1698 that any appellation like that of Mauritius was be- stowed upon it ; a fact which proves either the ignorance of Sanson, or that the map cannot be so ancient as marked, viz. 16/4. As the Society has a copy of this map, as far as I can remember in the collection of maps made the originals by Mr. E. Froberville, the Society can consult it for themselves. With regard to the term f Cirne/ it has no relation what- ever to the Portuguese word signifying “ Swan ” on account of the number of the “ Dodos ” seen on the island, but is simply a misconception of the geographical position of the aucient “ Cirne,” and can be clearly seen from Mr. Lemaire’s notes to Pliny (Nat. Hist. IV. 9) as well as from the very learned dissertations of Falconer on the voyage of Hanno. (Greek Text, explained from the accounts of modern travel- — 105 — lers ; London 1707.) With regard to the term ‘Apollonia’ this also is an imaginary one, though having no reference to the ancient town Apollonia, of which there were 33 ; but to the St. Apollonia whose feast is in December, and it being the common practice of the Portuguese to attach the names of saints to places they saw, or imagined they saw. With re- gard to the dates of the first discovery of this £ Cerne,’ they vary in a remarkable manner, such as 1500, 1507, 1505, 1528, 1545, 1502 etc. evidently showing there was no certainty in the matter. It was even called “ Diego Roys ” by some na- vigators ; and was even confounded with4 Juan de Lisboa,’ though in the early charts, (some rare copies of which I shall be able to forward to the Society next month) Juan de Lis- boa is placed many degrees to the South of it, and even of tire south point of Madagascar. In some of the very early maps “Cerne” is even represented as North East of Madagascar, Mascarenhas lying between them and St. Apolonia (someti- mes San Polonia) a smaller island, holding a North West po- sition of Mascarenhas towards Madagascar. In an ancient chart of 1546, this is their relative position : — — 106 — Juan de Lisboa lying so far to the South, may possibly have been what is now called “ Amsterdam Island.” In some of the early charts, an island holding the position of Bourbon is designated under the name of “ Drmobaz” and ‘ Cerne ’ under that of “ Dinaroby ; ” in others of rather later date, Cerne is also named under the following : Ilhada Cirne ; Do Sirne; Do Cirn: Le Arone ; le Arene ; Cygnoea ; and the geographers of the 16th century have mentioned, what I fancy from its position, must be intended for Mauritius, un- der the following names : Ilha Draarco ; Alhadaarco ; Dala- dladarco ; Y Daladia ; Y Darca ; I de l’arca ; Do Aro ; x\lia- doro ; Aldabarne ; Adarno ; Area ; Atces ; Atques. These strange names are not found in the Portuguese Historians, but only in their charts, and exemplifies that tendency to cor- ruption of names of which Dr. C. Regnaud has given an in- teresting instance in the “ Quelques mots sur le veritable nom de l’lle Diego Garcia.” (See Transact. 1860, p. 280.) The Ilhas de Mascarenhas give their name to a group of islands near the Equator ; and tracing the route of the ear- liest Portuguese navigators, these, it seems to me, must have been the islands they came across in the Viceroyship of their first governor in India, Almeyda; and not Bourbon, which lay quite out of their track, which was to Coast Africa all the way, visiting Natal, Cape Corrientes, Quiloa, Mombaza, up to Aden, at which point they seemed to have kept a strict watch on all merchant ships, which they obstructed in their passage up the Red Sea, importing by this way their commerce into Europe. They then crossed over to the Coromandel and Malabar Coasts, and naturally came early upon Taprobana or Tapropana, now Ceylon ; from this island they directed their course through the straits to Bantam and the various spice islands, China etc. On the return voyage they followed the same route, unless driven by contrary winds, as they were invariably in pursuit of other ships richly laden with similar merchandise to what they carried, and which were steering their course to the Red Sea. It was only by chance that the West Coast of Madagascar was visited by Soarez, his ship having been driven too far Eastward in making his way up Mozambique Channel to Quiloa, Juau de Nova is, I fancy, 107 — one of the Comoro group, or some rock to the Southward of them, and should be, according to the ancient Portuguese charts, placed between Quiloa and Mozambique. Some set down two different islands for Juan de Nova; but the island between Madagascar and Africa is that usually accepted as Juan de Nova ; it is quite clear, however, that the early navi- gators, such as Juan de Nova, Mascarenhas, Acunha etc. were in the habit of giving their names to different islands. Such gentlemen, are a few observations on this obscure point ; the maps which will reach you next month, and which are of great rarity, will be an additional confirmation ; but the whole of the early Portuguese portion of Mauritian history requires to be re-written. I remain, gentlemen, very truly yours, James MORRIS, 8 Gt. Ormond street, Queen Square, 19th December 1860. To the President and Members of the Royal Society of Arts and Sciences. Gentlemen, Since my last communication, I have carefully examined four important Portuguese Historians at whose disposal, for the purpose of composing their various histories, tho whole of the papers preserved in the Archives of Portugal were placed. Little relating to early Portuguese history may be supposed to remain in Lisbon and elsewhere which has not been seen by the historians of whose works I am about to speak. In addition to this I have been allowed to inspect and have co- pied some of the unique and rare maps in the collection of the British Museum, and I have received some valuable in- formation from the learned Curator of that department, whose admirable work on early Australian History has already been published by the Hakluyt Society. All the information I — 108 — have collected, goes to prove most incontestably that Mauri- tius was not discovered by the Portuguese, either by the per- sons, or at the time mentioned by all the modern writers on the subject. No mention of such a discovery, or of such an island appears in the great Historians from whose works I have copied those passages which, while detailing the lives and exploits of the persons supposed to have made the dis- covery, prove collaterally by the silence of the Historians, that such was not the case. Barros, the author of the Asia Portuguesa, is always rec- koned the greatest and fullest of the Historians of Portugal ; it is an extremely rare work, and rarer still to meet with all the Decades complete, as Decade VI for instance, was nearly all destroyed by fire. Only the First Three Decades also are by Barros ; the rest are by Diego Couto up to XII, and the XHIth is by A. Bocarra. The First Decade begins with the first voyages to India under Vasco Gomez, Pacheco, Cabral etc., and the voyage of Governor Aln.eida (1505) to India as the first Viceroy, does not begin before the 8th Book of the First Decade. The whole of the principal events and voya- ges to and from the Indian Ocean in his time which were in any way near Madagascar, or connected with the discovery of that Island, or Ceylon etc. have been copied. The names of the various captains of the different fleets sent out to explore in these seas, have also been added. Those chapters contain- ing nothing bearing on the subject, have had merely their contents put down, so as to connect them with the rest of the history. The voyage of Joao Gomez D’Abreu, (one of D’Acunha’s fleet), to the River Matatana on the East Coast, where he was left behind with some of his men who after- wards set out (it is said) for Mozambique, is evidently the only time they were likely to have come across the islands of Bourbon or Mauritius, though no mention of such islands, by any names whatever, occurs, as will be seen by the Extracts copied from the Decada Sequerela liv. T. C. I and II etc. The voyages and adventures of the famous Albuquerque and other celebrated captains have been extracted ; at Ch. VII is mentioned his ship which is called the Cirne ; and also in Book V. C. III. In Book VII Decada II occurs the first — 109 — mention of D6 Garcia Noronha, in whose fleet of 16 ships which left Portugal in 1511, the name of Pedro Mascarenhas, one of his captains first occurs. (Cap. II.) This Chapter is, of all others, the one most bearing on the point, and his vo- yages in these parts, as well as his route from Madagascar is copied in full ; and his whole career up to his return to Por- tugal in 1527, is extracted. In this Cap. there is mention of a ship called Galeya ; but not the most distant intimation of anything bearing on the discovery of the Islands, afterwards Bourbon and Mauritius, is to be found. CASTANHEDA (1552.) This historian is one of the most complete and elaborate of the Portuguese writers. The extracts made from his work, particularly from Books II and III at the time of the Gover- norship of Almeida when Bourbon and Mauritius have been set down as having been discovered by Mascarenhas ; the account of the discovery of Ceylon and Madagascar, showing how they reached those islands and by what route they left them, will show what authority there is for any such asser- tion. No mention is made of these islands under any of their many names, nor does the name of Mascarenhas occur at all, even as a subordinate, in any of their ships, of which, at the commencement of every expedition, it was the custom to re- cord the names of the commanders and officers in full. Some writers, Strickland among the number, surmise that it is pos- sible the Portuguese may have come across those Islands when they reached the River Matatana on the East Coast o^ Madagascar, at which point they were the nearest to them, being nearly opposite to Bourbon : (See Extracts C. XXIII C. CVII Book II.) Near this point some of the ships were dispersed. (See also Barros, Dec. II Cap. I and VI of lib. 1.) In this expedition, there was no Mascarenhas, nor does his name occur until Book VI Cap. CL (Lie of the ships of the expedition was called irne, (Book II Cap XXXV.) A list of the Islands known at that time to the Portuguese, is appended, selected with considerable trouble from Castenhe- da’s Great History. — 110 — If Mascarenhas was mvarded, as Grant, and other AArriters affirm, for his discovery of these tAvo islands in 1505, it Avas certainly long after the time he is said to haATe discovered them. He Avas more likely reAvarded for his Avarlike and cou- rageous attack on Bantam and other places which he subject- ed to the authority of Portugal. There is also another group of Islands near the Equator which bear his name; it Avas common among the early navi- gators either to name, or have named after them, various islands, and this circumstance has tended to increase the geo- graphical confusion so prevalent at this period. There is no entire translation of Castanheda, except the extremely rare one into Italian by Ulloa ; the first Book only has been tran- slated into German 1554, and into French, by Grouchy 1553. This Book only has also been translated into English. OSORIUS. The principal parts of this learned and copious historian have been extracted, and translated mostly from the latin for this occasion, bearing in the viceroyship of Almeida in India. The Avhole of the chief events, vcyages and discoveries during his governorship in India; the voyages of Albuquerque, and all that is mentioned of Pedro Mascarenhas, until he return- ed to Portugal in 1527. (Bks. VIII to XVII) He Avent out, Osorius says, in the fleet of Garcia Noronha, the nepheAv of Albuquerque, as Captain, about 1511. It appears singular that at Cap. XVII there is a mention of the Admiral’s dag ship as the St. Denis, in Avliich the Governor Sampayo wished to sail, but Avas forced by his rival, Mascarenhas, to go into another. The names of the tAvo other Aressels Avere also sin- gular,— the St. Louis and the Zamorin . The AA'ork of Osorius contains more details of Mascarenhas than even the other historians. At the end of the extracts is appended a list of all the islands then knoAvn and described in this very voluminous work of 20 books, all of Avhich have been carefully gone over by me. — Ill — SAN ROMAN. This likewise is one of the early and important Historians of Portugal. The extracts from his “ Historia ” aomprise only a short resume of the time of Almeida, and the chief points in the career of Mascarenhas, which completely confirm the view taken above, as no mention of the Islands or any disco- very of them, is anywhere made. MAPS. The Maps sent are all extremely rare, and are facsimiles Pigafetta, and a few others deny that Taprobana is Ceylon, (see Blactin Behaim’s Map.) The Map of the early part of the 16th century, is an Arabic one and very curious ; the names. Din Aroby and Dimo-Bay seem to be the Arabic po- sition for the islands afterwards Bourbon and Mauritius. Juan de Lisboa must evidently be some rock or islet to the South of Mauritius, for the place of this island is the same in all the early maps. I fancy that Apolonia (Apolina etc.) is a much more ancient name than Cirne or Mascarenhas, and is found on much earlier maps than either of these, and has been given to Bourbon, and probably comprehended both the islands to- gether. Madagascar, in most of the early charts, is the real Cirne (Othiopica) Yel Insula Manuthias, Vel Manupias. The Illuminated Chart from the grand Vellum Altas of Diegus Homen (1558) is unique, and is carefully preserved in the King’s Library. Sir Frederick Madden gave me special per- mission to have it copied. This map is one of the first in which these Islands are called u Mascarenhas.” The other Illuminated Map by Johann Rotz, the most ancient Portu- guese Portulan in England in which the name c' Mascarenhas ” is given to these Islands. It has been copied from the vellum original in the King’s Library, the only' copy extant. In this Map, Bourbon is called Apolina, and Mauritius, Mascarenhas . The Arabic Maps and Books will be examined by me when 1 can find time ; for the above reseai’ches have occupied me an entire month, and I have had the work copied in the most economical manner possible for the Society, consistent with J the care required in making the extracts etc. which have to be done by regular and competent copyists. I wish to call at- tention to one Map of the Froberville Collection, “ Extrait de la Novissima Africa de"criptio” Amsterdam, Apud I. Blaev 1569. There must be an error of date here, for this Map is nearly 100 years later. The curious papers connected with the French Revolution shall also be examined when I can find time. * James Morris. I remain gentlemen, sincerely yours. SIR LE MODE DE REPARTITION DE CERTAINES PLANTES A MAURICE. J’ai pu constater, dans une tournee que j’ai faite il y a quel- ques mois a la Nouvelle-Decouverte, en suivant la route qui forme au sommet d’une des chaines de la Montagne des Ca- lebasses, le passage appele la Coupee, la marche qu’ont suivie certaines plantes tant exotiques qu’indigenes, sur la croupe de la montagne et tout le long du chemin. Les unes ont adopte une marche ascendante dans leur mode de reproduction ; d’autres au contraire, semblent etre descendues du haut de la montagne pour venir s’etablir dans la plaine, et jusqu’a une assez grande distance au bord des rivieres. Je parlerai d’abord du Tridax procumbens, connu sous le nom vulgaire de “Herbe Caille.” Cette plante est aujourd’hui disseminee sur presque tous les points de File, et croit meme dans les rues de la ville, sur les murs et les montagnes avoisi- nant Port-Louis. Son point de depart vers 1830 ou 1831, a ete le Jardin Botanique des Pamplemousses, ou elle avait ete cultivee dans le parterre dn Directeur, comme plante d’agre- ment, a une epoque ou l’on se montrait probablement moins difficile qu’on ne l’est anjourd’hui, dans le choix des fleurs propres a orner un jardin. De la, elle a pris son vol pour aller s’ebattre partout ou les vents ont transports ses aigrettes* qu’ils ont disseminees dans toutes les directions. TFautre plante egalement introduite dans le pays et qui sem- ble offrir dans son mode de reproduction plus de difficulte que la premiere, puisque son fruit est une baie charnue que le vent ne peut enlever, sortie egalement du Jardin Botanique des Pamplemousses, s’est d’abord repandue dans les plaines au has de la montagne et s’est progressivement elevee jusqu’au sommet. C’est le Daphne viridiflora ou Wickstroemia viridi- Jlora Meisn. in DC. P. Elle s’est egalement propagee sur d’autres points, en suivant touj ours une marche ascendante. Une troisieme plante, V Elephantopus scaber suit une ligne diametralement opposee a celle du Wickstroemia viridiflora , — 114 — c’est-a-dire que de nombreux individus sont sortis des fo- rets elevees a Pombre desquelles on en rencontre des masses, pour descendre et s’etablir dans les plaines, au bas de la mon- tagne. J’ai pu en observer jusqu’au bord de la Riviere des Calebasses. Cette derniere plante est indigene a Maurice. Dans une exploration subsequente, j5ai pu constater l’en- vahissement dans les forets d’une espece de Rubus originaire de PInde ou de Java, le R-Ramiltonicums introduit a Mau- rice il y a une trentaine d^annecs, et d*un Passiflora P. fcetida qui se sont aussi considerablemcnt repandus sur les limites des forets. On peut se rendre compte de la propagation du Ru- bus en question par la dissemination des graines faite par les oiseaux. II est plus difficile de se rendre compte de la natu- ralisation du Passiflora. Ces plantes sont devenues si communes dans plusieurs lo- calites de Maurice, qu’on pourrait les croire indigenes. Toutes cependant sont exotiques, a l’exception seulement de VEle- 'phantopus scaber, et j’aitenu a signaler ce fait, afin que les botanistes dont nous recevrions plus tard la visite, pusseut se tenir sur leurs gardes et ne pas confondre ces plantes avec celles propres au pays meme. L. Bouton. 1 -yy »>- ETUDES SIR LA PLANTE. ( Article communique par un membre de la Section d’Histoire et de Litterature.) L’homme a, dans tous les temps, voue a la plante une sorte de culte. Si vous remontez a l’origine des siecles, dans les temps fabuleux, vous voyez chacune d’elles ou du moins les plus utiles d’entre elles, placees sous les auspices de divinites protectrices. Pour parler le vieux style, nous vous dirons, par exemple, que Flore et Pomone produisaient pour nous leurs bouquets et leurs fruits — que Ceres, semblable a line mere nourriciere, nous offrait ses gerbes de ble ; Bacchus, ce Dieu eonsolateur, sur lequel toutefois il ne faut pas trop se tier, nous donnait ses raisins a pressure!’, tandis qu’Esculape prc- parait de ses mains des remedes aux maux que devait neces- sairement susciter, a des creatures, loin d’etre aussi raisonna- bles qu’elles le sont de nos jours, l’usage immodere de tous ces dons prodigues par les Dieux. La plante n’en est pas moins restee jusqu’aujourd’hui l’ob- jet d’une vive sollicitude de notre part. Elle s’etend cette sollicitude ou plutot elle se concentre sur cette foule de vege- taux si necessaires a nos besoins, sur nos cultures de grains, de ble, d’orge, d’avoine et ici a Maurice sur nos champs de Cannes a sucre. Partout c’est un hommage rendu a la plante et corame un devoir que nous remplissons envers elle ; c’est un soin religieux donne a son entretien et a sa culture, source intarissable de nos richesses, de notre bien-etre et de nos jouissances. Et cependant quel que soit l’hommage qui lui est rendu, la plante, sous le point de vue ou nous voulons Penvisager, n’est pas placee dans l’echelle de la creation au rang qu’elle devrait occuper — du moins nous le pensons — et voila pourquoi nous voudrions la rehabiliter, et nous assurer si cet etre croissant, vivant, souffrant et mourant comme les autres etres places plus haut que lui, n’est pas en definitive quelque chose de — 116 — mieux qu’un etre inerte — insensible — passif — s’il n’est pas cn- fin, tranchons le mot, doue d’une sensation quelconque. “ Les vegetaux sont des corps qui se nourrissent et peu- vent se reproduire, mais qui ne sentent, ni ne se meuvent vo- lontairernent.” Telle est la definition que les botanistes nous donnent de la plante — selon eux, la plante est done indubita- blement un etre vivant, mais attachee par ses racines au sol ou elle puise sa nourriture, et se developpant a sa partie su- perieure, et vers le ciel en tiges, en rameaux et en feuilles. Le professeur Lindley, un des plus grands botanistes de notre epoque, la decrit ainsi : drops of the rate gt. — .51 have the same size as those of the rate gt. — .64. In order to establish more precisely the posi- tion of this minimum and the general relation between rate and size, a more minute division of the time must be made and the table must be more extended. From this short Table however may be gathered how extremely sensitive the size of the drop is in regard to the time wdiich it takes to form. * Table I, T = 28°. 5. of ropi 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 — 173 — TABLE IY. T = S9°C. Sp. Gy. = 0.9195, Time veen fall )f first one and t Drops. • Weight of Drops. Number of D:'ops. Time between fall of first but one and la .t Drops. Weight of Drops. 25” 4.9543 30 34” 4.6013 25 4.9613 30 35 4.5340 25 4.9608 <30 35 4.5334 25 4.9604 60 35 4.5420 26 4.8463 60 35 4.5309 26 4.8448 60 36 4.4021 26 4.8423 60 72 8.8066 26 4.8432 60 36 4.4013 27 4.9112 60 36 4.3925 27 4.9107 60 37 4.3932 27 4.9121 60 37 4.3891 27 4.9100 60 37 4.3925 28 4.7530 60 37 4.3938 28 4.7534 60 3S 4.3934 28 4.7515 60 38 4.3940 28 4.7459 60 38 4.3932 29 4.7594 60 38 4.3907 29 4.7588 60 40 4.3857* 29 4.7607 60 40 4.3560 29 4.7591 60 40 4.3564 30 4.8105 60 40 4.3565 30 4.7123* 60 45 4.2319* 30 4.8099 60 45 4.2623 30 4.8111 60 45 4.2619 31 4.8184 60 45 4.2588 31 4.8084 60 50 4.1442 31 4.8055 60 50 4.1400 31 4.8095 60 50 4.1420 32 4.7714 60 50 4.1398 32 ' 4.7782 60 60 3.9644 32 4.7785 60 60 3.9627 32 4.7786 60 60 3.9622 33 4.6194 60 60 3.9619 33 4.6177 60 90 3.7294 33 4.6141 60 90 3.7294 33 4.6126 60 90 3.7296 34 4.5960 60 90 3.7291 34 4.5964 60 120 3.5920 34 4.5996 60 120 3.5913 TABLE IV ( continued }) T = 29° C. Sp. Gy. = 0.9195. Number of Dropsi Time between fall of first but one and last Drop. Weight of Drops. (Number of Drops. Time between fall of first but one and last .Drop. Weight of Drops. 60 120” 3.5916 60 300” 3.2813 60 120 3.5926 60 300 3.281 1 60 180 3.4243 60 300 3.2811 60 180 3.4263 20 240 1.0400 60 180 3.4268 20 240 1.0402 60 180 3.4278 20 240 1.0402 60 240 3.3379 20 240 1.0399 60 240 3.3348 . . . • • • 60 240 3.3358 ... ... • • • 60 240 3.3371 • • • • • • 60 300 3.2814 ... ... From this Table the following Table V is derived. Column I shows gt. the growth time of the drops, column II shows the corresponding mean weights of the single drops. Column III shows the rate of delivery per second in grammes. It was found impossible to arrest an exact number of drops when the rate was faster than 60 drops in 25”. A fen* rather dis- cordant results got at the rate of 60 drops in 20” gave a mean of 5.5584, tending to show that at this high rate the drops were considerably larger than at any lower rate. Towards the end of the Table at the slower rates the error of time becomes so magnified, the least alteration in the ad- justment of the instrument makes such a sensible alteration in the entire time lapse that it is nearly impossible to avoid an error of less than 0”.5 on the whole time of several minutes. Although the time error thus becomes palpable it remains nevertheless relatively to the whole time lapse, as im- materially small as are the inappreciable errors of the swifter rates of dropping. TABLE V. T = 29° C. Sp. Gy. = 0.9195. 1. II. III. U t •' Mean Weight of Single Drop. Weight of oil passing per second. (0”.333) Grms. ( 0.09264 ) Grms. ( 0.27792 ) 0”.417 0.08265 0.19837 0”.433 0.08074 0.18631 0”.450 0.08185 0.18189 ■ 0”.467 0.07918 0.16968 0” 483 0.07932 0.16412 0”.500 0.08017 0.16035 0”.517 0.08017 0.15518 0”.533 0.07961 0.14927 0”.550 0.07693 0.13985 0”.567 0.07664 0.13524 0”.583 0.07558 0.1.2957 0”.600 0.07334 0.12221 0”.617 0.07320 0.11871 0”.633 0.07321 0.11560 0”.667 0.07260 0.10891 0”.750 0.07102 0.09469 0”.833 0.06902 0.08283 1”.000 0.06605 0.06605 1” 500 0.06215 0.0 1144 2”. 000 0.05986 0.02993 3” .000 0.05710 0.01903 4” .000 0.05561 0.01432 5”. 000 0.05469 0.01094 12” .000 0.05201 0.00 133 These numbers present several interesting and important facts. From fft. = .333 to f)t. — .433 there is a dimimition. » = -i33 .450 ,, an increase. » = -4'50 3) .467 ,, a diminution. » = -467 )) .500 ,, an increase. )3 — .500 D 12.000 }) a continual di munition. The most prominent fact is that, on the whole, the drops undergo a continuous diminution. To such an extent is this the case that the most rapidly falling drops of the above Table are nearly twice as heavy as the most slowly falling ones. The cause of this is probably to be sought for in the circumstance • # that when the flowing to the solid is more slow, the latter is covered with a thinner film of liquid, so that as the drop parts, the solid reclaims by adhesion more of the root of the drop than is the case when the adhesion of the solid to the liquid can satisfy itself from the thicker film which surrounds the drop in the case of a more rapid flow. The influence of rate is seen to extend even to the exceedingly slow rate of gt.— 12”. This connexion between rate and weight (or quantity) should not be lost sight of by prescribers and dispensers of medicine, where a certain number of drops are to be given : A Pharmacist who administer 100 drops of a liquid drug at the rate of 3 drops per second may give half as much again as one who measures it at the rate 1 drop in two seconds : and so on. For our present purpose the effect of rate upon the size of a drop is of great moment, because it proves that there is no such thing as a drop of normal size. At no degree of slow- ness of dropping do drops as mme a size unaffected by even a slight change in the rate of t leir sequence. Hence, whenever a comparisor. has to be made between the sizes of different drops, we shill have to elimiiate this source of difference by taking drops at exactly the same rate. About the rate at which the diminution of size takes place for equal increments of gt., the table gives us little informa- tion, beyond the fact that on the whole, the sizes of the drops at the slower rates are less influenced by equal increments of gt. than are those of the quicker rates. This however only appears distinctly at and below the rate of about gt. — 1”.00. If the connexion between gt. and the drop size be repre- sented by a curve (Fig. II. A.) the abscissae being the values of gt. and the ordinates the corresponding weights, there is no apparent asymptote parallel to the axis of X. The curve presents however in its course two secondary maxima and minima. Secondary Maxima. Secondary Minima. (1) gt. = .450 gt. = .433 Although at these minima the drops are less than at the immediately succeeding rates, yet the quantity of liquid pass- ed in a given time is, at every rate of dropping, greater than the quantity passed at a slower rate in the same time. The decrease of rate more than counterbalances the temporary in- crease in the drop size. This is seen on comparing the num- bers of column III with one another. They are found to de- crease continuously, though by no means uniformly, as the rate of dropping decreases. The second maximum (at gt—. 500 and gt—. 517) is ill re- markable connexion with the rate at which a series of drops may be converted into a continuous stream. At the rates of dropping from gt. — .2>?>2> to gt—.§Y7 inclusive the drops may be converted into a permanent stream by pouring a little of the liquid upon the sphere as the drops are falling from it. A stream is thus established which remains for any length of time if it be protected from all currents of air and vibration At the rate gt — . 519 the stream maybe established by the same means for a few seconds (about 30”) ; but the continu- ous part inevitably begins to palpitate, becoming alternately longer and shorter, thinner and thicker, until at length it draws up and is converted into drops. At the immediately succeeding slower rates of dropping, the same effect follows, but in each case in a shorter time. So that the slowest rate of dropping which may be converted into permanent running coincides with that rate which gives the second maximum size of drops (gt= .500 and .517) . The appearance of a drop-con- vertible stream is peculiar, the narrowing which it undergoes — 17S — on leaving the solid being remarkably sudden. Curve B, Fig. II. , shows the relative quantity of liquid passed in a unit of time. The abscissae give the value of gt and the ordinates the value of column 3 Table V. In order to avoid the influence of variations in rate we shall for the future take the rate of dropping in all cases the same and unless the contrary is stated the rate adopted will be 9t — 2”. The factor, the influence of whose variation on the size of the drop we have- next to consider, is tire constitution of the liquid of which the drops arc formed. For the above experi- ments concerning the influence of rate cocoanut oil was em- ployed on account of its non-volatility. On allowing a quan- tity of it having an exposed surface of about two square inches to stand for 70 hours it was found to have increased about two milligrammes in weight, probably in consequence of oxidation: Its fixedness therefore and its perfect liquid- ness at the temperature 28° — 30w C. make it well adapted for this special purpose. Chemically and physically however it is of little interest from the present point of view, because it is a mixture of several substances the proportion between which is indefinite. It will be of great interest to examine the effect upon the size of drops of the chemical composition of liquids belonging to the same homologous series, such as the ethers, alcohols and corresponding acids. For this purpose and also for exa- mining the effect of solution of solid matter upon the drop- size we must determine the drop-size of water under fixed conditions. With mere mobile liquids, the Apparatus Fig. 1 fails to give a strictly uniform flow. As the liquid descci ds in B it adheres by capillary action to the lip of A for some time af- ter the level of B is below the lip. The air at last separates . the two, enters the flask A displaces the liquid there and res- tores the level to B. So that although tbc average height of 13 is constant yet it undergoes a series of slight but ceaseless 179 variations. As however this slight variation sensibly affects the rate of f oav through the siphon, the apparatus is slightly modified as follows. Between the reservoir B with its flask A and the dripping sphere a second reservoir W is placed. This is kept in a s:atc of continual overflow. The overflow is regu- lated by means of a few filaments of cottonwool hanging over the edge of the overflowing vessel and so fashioned that the thickest part of the cotton plug is in contact with the edge. Finally the rate of flow is so sensitive that it is impossible to procure an exact and predetermined rate by the ordinary screw adjustement of the holder which carries the siphon. For the final adjustment it is convenient to depend upon the elasticity of the siphon which is at first rigidly fixed so as to deliver the liquid at nearly the required rate. A heavy ring is then slipped on the siphon so as to bend it more or less. A little caoutchouc is wrapped round the ring where it touches the glass so as to prevent it from slipping. See Fig. III. The following table shows how the size of a drop is affected by the quantity of solid matter which it, holds in solution. The liquids examined were solutions of chloride of calcium of different strengths. They Avere prepared as folloAA's : — A solution nearly saturated (at 28 ° C.) Avas taken as the starting point. Solution 1. An accurately stoppered bottle Avas tAA'ice filled vrith solution 1, emptied into a beaker and mixed with tAvo bottles of Avater. This gave solution 2. Half of this was kept and the rest, mixed again with its own volume of wa- ter gave solution 3 and so on. In this Avay without knoAV- ing the strength of solution 1 : Ave knoAv that the successive strengths of the solutions whether there be loss of volume, due to chemical combination, or not, are as S, S S S S S 0 } -4 ) 8 j 16 > 32 These numbers give exactly the relative quantity of solid matter in a unit of volume of the liquid. As however solution I on dilution evolves heat, the sizes of the drops cannot be derived from their Aveiglit directly. The specific gravity of each solution has to be determined. TABLE VI. m. m. fft. - 2”. T = 28° C. Radius of Sphere = 22.1. Solution of Cacl. Wt. of 30 drops. Mean Wt. of a single drop. Sp. Gy. Relative size of a single drop. 8 \ r 6.6715 ‘ 6.7031 6.8347 6.8577 > > 0.225558 1.4939 \ 0.15098 v 6.3120 \ 6.3031 6.3653 6.3771 _ 0.211396 1.2786 0.16533 S T " 5.8698 *1 5.8841 6.8746 5.8722 „ Y 0.195839 1.1721 0.16742 s 5.7265 5.7332 . 5.7279 5.7334 _ > 0.191008 1.0720 0.17817 i. J 16 ' 5.0241 ” 5.0451 5.0184 4.9790 _ > 0.167222 1.0383 0.16105 s 32 r V 5.2149 ' 5.2175 5.2368 5.2420 _ 0.172593 1.0172 0.16967 r 5.1842 ' 5.1854 5.1904 5.1889 _ > 0.172907 1.0084 0.17147 S 128 5.0275 5.0520 5.0536 5.0433 _ 0.168137 1.0039 0.16750 Water < r~ w 5.5534 " 5.5534 5.5524 5.5584 5.5524 5.5598 > 0.185166 1.0000 0.18517 — 181 The column of the relative sizes of single drops (which is got by dividing the mean weights by the respective specific gravities) shows that, under like conditions, a drop of water is larger than a drop of solution of chloride of calcium of any strength whatever. The comparatively small quantity of so- lid matter in S/128 causes the drop to diminish about l/g of its volume. Me must bear in mind that the successive incre- ments of solid matter affects the size of the drop in several ways. By affecting the cohesion of the water : by asserting its own cohesion j by its superiority in weight determining a fall of a drop comparatively sooner, and in this case by the che- mical affinity of the solid to the liquid, which may be saltatory according to the possible hydrates of chloride of calcium. It is seen that these various influences cause an irregularity in the diminution of the size of the drop as it acquires more so- lid matter. In fact, it is only when the liquid has the great strength of S/s that the diminution in drop size becomes, con- tinuous. On account of the chemical union which takes place on dissolving Ca Cl in water I have not given the absolute strengths of the various solutions. To see how much of the intermediate irregularity is due to the existence of chemical union between the two bodies of which the liquid is compos- ed, we may next take nitrate of potash which as far as is known does not combine with ■water at all. Solutions of nitrate of potash were made of the following strengths by weight : — .22 of water to 1 of nitrate of potash. •)9 ) * 9 yy 90 y y 3 yy yy y ) 90 } y 4 y y yy 22 22 22 22 yy y y 9 (j 8 .) f y y yy yy yy yy yy These were made to drop from the ivory sphere (Fig. HI) at the rate of yt. — 2”. In each instance four batches of 30 drops each were weighed. TABLE VII. m m. yt . = 2”. T = 28° C. Radius of Sphere = 22.1 I. II. III. IV. V. Solution HO KNO A 6 Mean weight of single drop. Specific gravity hv experiment Relative size ! of si ngle j drop. ■ Weight of KN06 in single drop. 22/s 0-18022 1-1267 •16014 22/; 0-18611 1-1130 •16723 •05921 22/c 0-18254 1-0987 •16618 •01978 22/5 0-17805 1-0832 •16439 •04047 22A 016917 1 -0680 •15810 l •16853 •03075 22/3 0T7714 1-0511 •0.2411 22/2 0-17908 1 0341 •17318 •01628 »/l 0-18613 1-0164 .18314 •00846 22/o 0-18517 1-0000 •18517 •00000 On comparing the numbers of column IV with one an- other we cau trace the following effects, bearing in mind that the chief factors are ( 1 ) the cohesion of the water to itself. (2) the cohesion of the nitrate of potash to itself. On the addition of the first, parts of nitre { " ““ -4r ) the cohesion of the water is successively diminished. Af- oo oo tenvards ,?) tlie cohesion of the nitre begins to as- sert itself whereby the size of the drop is partly recovered. There is a stage of dilution in the case of nitre when the Sp. Gv. is 1, 1(380 where the drop size is a minimum. Further if is seen from column Y that the quantify of nitre in a drop 18:’, — increases continually as the strength of the solution increase* although the weight and volume of the deep both vary. Inversely the regularity of the variation of drop size in the ease of nitre, points to the absence of definite hydrates of that body. It would be easy but delusive lo construct a formula con- necting the specific gravity with the drop size or dee]) weight of the solution. But a graphic representation seems to show the connexion between the variables. In fig. II the abscissae of the curve C represent the quantities of nitre dissolved in the same quantity of water. The ordi- nates of curve C show the corresponding weights ; those of P, the corresponding volumes of the drops ; those of E, the corresponding weights of nitrate of potash contained in a drop. It is confessedly a matter of great interest and still greater difficulty to determine exactly the relation which exists he- V V tween a dissolved solid and its solvent. The question may perhaps receive additional light from experiments similar to the above but more extensive and with this special object in view. Comparing the tables VI and VII there can for instance be little doubt that the apparent irregularities in table VI are owing to the existence of definite hydrates of chloride of cal- cium, while the uniformity of the numbers of table VII show that no hydrate of nitrate of potash exists at this tempera- ture. If this be the true explanation we may certainly make use of the method of drop-weighing to trace the exist- ence oi1 absence of hydrates in solution of salts, or generally the existence of definite compounds in mixtures. And thus perhaps Berthollcts hypothesis of reciprocal recomposition may receive confirmation or the reverse. An investigation of this kind would lead away from the present purpose. he have next to consider the influence which the variation in the chemical nature of the drop-forming liquid may exer- cise upon the drop-size in the case SLG. The liquids which were selected for this purpose were clio-* j 8 i sen a* being typical of extensive classes rather than as being connected with one another in immediate chemical relation. They were : Water; Alcohol; Acetic Acid; Acetic Ether; Butyric Acid ; Oil of Turpentine ; Benzol; Glycerine and Mercury. The several liquids were allowed to drop from the same platinum cup. The arrangement of the apparatus was quite similar to that described in T. the ivory ball being replaced by the platinum cup, and the overflow of the cup being deter- mined by strips of paper bent. over its edge. The last ease, mercury, is the only one which requires some explanation. A few years ago (. noticed a fact widen has probably been ob- served by others, but of which I find no mention: namely that mercury which holds even a very little sodium in solu- tion has the power of “ wetting” platinum in a very remark- able manner. The appearance of the platinum is quite simi- iar to that of amalgamable metals in contact with mercury, but the platinum is in no wise attacked. Further, the amal- gam may be washed off by clean mercury and the latter will also continue to adhere equally closely to the platinum. All the phenomena of positive capillarity are presented between the two. The surface of the mercury in a platinum cup so prepared is quite concave; and a basin of mercury maybe emptied if a few strips of similary prepared platinum foil are laid over its edge : just in the same way as a basin of w ater may be emptied by strips of paper or cloth; and under the same conditions, namely that the external limb of such capil- lary siphon be longer than the internal one. I generallv use this curious property of sodium amalgam for cleaning platinum of vessels. It enables us now to exa- mine the size of drops of mercury under conditions similar to those which obtain in the ease of other liquids. ■■ # In regard to the above mentioned property of sodium, t,bc follow - im» observations may be of interest. At lirst, t be explanation naturally sim 'esta itself that the effect wrought hv the sodium may be due to an ubeorbtion of oxygen in consequence of the Oxidation of the sodium, Alter the cup hud been used for the other liquids, its sur- ly.ee Mcis 1 uhbecl with sodium iuruilgciivi mid washed with clean mercury. A few strips of similarly prepared platinum foil being bent ov er the edge and pressed close to the sides of the cup, the mercury could lie handled similarly to the other li- quids. The following table shows : 1 . The liquids examined ; 2. The number of drops which were w eighed ; <>. The weights found ; T. The mean weights of single drops ; 5. the observed specific gravity at the given temperature; (i. The relative sizes of single drops'. the experimental numbers obtained are given w ithout omis- sion. 1 hey arc arranged after experiment in the order of magnitude oi the relative drop sizes. the consequent diminution of the gaseous film between the two metals and the consequent excess in the superior pressure of the air. This however cannot be the true explanation, because it is found that, the perfect contact between the two or wetting, takes place equally well in an atmosphere of nitrogen, of carbonic acid and in vacuo. Hence, if I may venture upon a guess, unsupported by direct experimental evi- dence, I should be rather disposed to assign (he action to the effect of nascent hydrogen due to the action of the sodium upon traces of moi- sture Perhaps even the least oxidizable metals may be coated wi'h a thin film of oxide which is reduced by the nascent hydrogen at the same moment that the mercury is presented to the reduced metal. It i* found that iron, copper, bismuth and antimony are also wetied by mer- cury if their surfaces are first touched with sodium amalgam. Not onlv do the latter metals lose this power on being heated (as we might expect in consequence of their superficial oxidation) but platinum, from which the adhering 'mercury film has been wiped by the cleanest cloth or from which it has been diiver. by heat, also loses the power. The surface of clean platinum condenses, it is supposed a film of the oxy- gen ; and the removal of this might alter the adhesion between the mercury and platinum. But such a film could scarcely exist in vacuo or in another ga^- m.m — 186 — TA BLE MIL T=26w C. gt. — S” — Ivadius of curvative ot platinum cup 11.4 V. VI. .Relative Size of Single Drop . I. 11. 111. IV. Name and Formula 3 Weight Mean of u* x k & ~ 0 - u 5 a of Weight of Single Liquid. y, Drops. Drop. .. — r 20 2 9703*1 2.9923 | AY a ter 1 20 20 j 2 9172 ). 0.14828 HO 20 2.9603 | i 20 j 2.9583 J Glycerine 20 2.5496 ■) CG H8 o* Butyric Acid e8 h8 o4 Mercury HK BenZ'l ( :12 Turprntol C.20 H 1G Alcohol ( 4 H6 Oo Acetic Ether c, b5 oc, h, o3 Acetic Acid HOC., II3 03 21) <2.5576 - ( 10 1-2877 J 20 20 20 i ( L t Vi 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 30 20 20 1.1616 ) 1.1630 > 0.05813 1.0017 '0.05303 1.1034 J 7 9655 A I'SiSJ ( 0.78703 13 5728 0.05798 1 .rJ <7 l 7.8197 J 0 9514-4 0 95791' 0 04778 °-8045 0 05-527 0.9644 ; 0 8650 r 0 01331 0.863 i 0.05016 0. 0.04960 0 7890 1 0 7910.- 0.03949 0.8103 0 7S96 J 0.821 4 ] 0 8300 > 0.04149 0 8930 0.8381- J l.3636*i 0.9055 - : 0.0 J 5 40 1 .0552 0 04302 0.9095 ) ; 0.04647 The numbers of column 6; with which we arc now exclusi- vely concerned present several points of great interest. In the first place it appears that the specific gravity ol'u liquid is not by any means the most powerful determinant of the drop- I size. Thus butyric acid which lias sensibly the same specific gravity as water, gives rise to a drop of less than half the size of the water drop: while mercury of singular specific gravity lias no exceptional drop-size. Lastly it may be observed how that remarkable body, wafer asserts here again its pre-emi- nence. 'flic first impression which these numbers make is that there is three groups of magnitude n, 2n, 3n. But it is possible that a change in the nature of the solid might throw these drop-sizes into a different order; and certainly until a very much greater number of bodies is examined in this sense it would be premature to attempt to establish anything like a law. It is sufficient for the present to point out that the drop- size is not directly dependent upon either the specific gravity or boiling point. Xor does it stand in any obvious relation to what is sometimes called the liquidity, mobility or “ thin- ness ” of a liquid. For we find that glycerine and (from for- mer experiments) cocoa -nut-oil both from smaller drops than water, the one being heavier and the other lighter than that body ; and both being sluggish. On the other hand alcohol and acetic acid both perfectly mobile liquids give rise to drops about half as large as those of glycerine.* Hence it is clear that we are still ignorant of that property of a liquid which determines its drop-size, and arc not yet in a position to connect the drop-size with any of the known physical or chemical properties of liquids. W e approach the solution of the problem by studying the effects of change in some others of the variables. The adhesion between the liquid which drops and the solid from which it drops is also affected by the curvature and ge- neral geometric distribution of the solid at and about its low- * Tie evaporation of the more volatile of these liquids is a source of slight error ; not so much on account of t he direct, loss by weight of the drop in falling, as by reason of the cooling which it causes and the con sequent variation in density and adhesion. Such source rt variation ■will form a separate subject ot investigation. — 188 — est point. And the variation in the adhesion between the solid and liquid caused by the variation in the geometric dis- tribution of the solid, mat and does in its turn affect the size of the drop. From this aspect one of the simplest kinds of variation is that offered by a system of spheres of various radii but made of the same matter. And this ease is an important one be- cause it undoubtedly offers the key to all drop-size variation arising from a similar cause. To study this point we may make use of any one convenient liquid such as water, and cause it to drop at a fixed rate from spheres of various radii, including the extreme case of a horizontal plane. This extreme case however presents certain practical diffi- culties. From a plane it is almost impossible to get a series of drops, uniform in growth-time and iu position. A ripe drop hanging from a horizontal plane of a substance which it wets will seek the edge thereof. Several drops may form upon and fall from the same plate at the same time and indepen- dently of one another. It is only by employing a plate not absolutely flat that an approximation to the required condi- tions can be made. Taking r for the radius of curvature there- fore, the first numbers for r — cc can only be considered as an approximation. The arrangements for the other cases were quite similar to that described in I Fig. III. No. 1. A glass plate, fastened to and held by a vertical rod. Nos. 2, 3, 4. Selected globular glass flasks. Nos. 5, 6, &c. Perfectly spherical solid glass spheres. 189 — TABLE IX. Water. gt . = 2” T =: 22 ~ .5 C. II. III. IV. V Number of Drops. Radius of Curvature. Weight of Drops. Mean Weight and relative size of single drop. 1 { 20 \ 20 / * { 5.3325 \ 5.2873 J 0.26549 3 { 20 1 20 J mm r- 113.1 -l 4.9226 \ 5.0007 J 0.24808 3 { 20 I 20 J 70.1 ^ 4.5260 1 5.5218 J 0.22619 4 { 20 \ 20 J 47.2 ^ 4.2781 1 4.2249 J 0.21257 3 { 20 T 20 J 17.5 ^ 3.5055 1 3.4733 J 0.17497 3 { 20 \ 20 J 15.1 ^ 3.3562 \ 3.3500 J 0.16765 7 { 20 1 20 J 11.5 ^ 3.0281 ) 3.0206 j 0.15122 8 { 20 1 20 J 11.2 | 2.9803 \ 2.9780 j 0.14896 0 { 20 \ 20 J 10.0 | 2.8665 1 2.8619 J 0.14321 i° { 20 1 20 J 7° \ 2.6765 \ 2.6660 J 0.13356 { 20 9 J - { 2.5752 \ 1.1591 J 0.12877 It appears, therefore that the drop increases in size accord^ ing as the radius of the sphere increases from which the drop falls ; and further that the difference of drop-size brought about by this cause alone may easily amount to half the lar- gest drop-size. For dispensers of medicine this fact is as im- portant as that pointed out in I ; where it was shown that the — 190 — growth time so materially influenced the drop-size. The lip of a bottle from which a drop falls is usually annuloid. The amount of solid in contact with the dropping liquid is deter- mined by the size of two diameters ; one measuring the width of the rim of the neck, the other the thickness of that rim. In most cases the curvature and massing of the solid at the point whence the liquid drops, is so irregular as not to admit of any mathematical expression. The reason why drops which fall from surfaces of greater curvature arc larger than those which fall from surfaces of lesser curvature is surely this : In the case of a surface of greater curvature the base of the drop has more nearly its maximum size ; the neighbouring liquid film, from which the drop hangs, is, on the whole, nearer to the centre of gravity of the hanging drop; .the contact between the two is more ex- tensive and intimate so that the drop is held for a longer time and therefore grows more. On comparing columns 3 and 5 of Table IX there does not appear to be any obvious law of connexion between the two ; nor indeed can the numbers of column 4 pretend to such a degree of accuracy as would jus- tify us in attempting to establish one. This is seen on com- paring inter se the numbers of column 4. Especially with the spheres of longer radii there is so much difficulty in getting an uniform wetting of the surface whence the drop falls, and this so materially influences the drop-size, that the mimbers found are seen to vary considerably. Greater accord is ob- tained with spheres of less radii. As we might have expect- ed, the same absolute increase in length of radius, takes less effect upon the drop size in the case of longer than in that of shorter radii. The infinite, or at least indefinitely great dif- ference between the radii 1 and 2 produces about the sarre effect upon the drop-size as the difference of 43mm- between the radii 2 and 3, and so on. The following table of first dif- ferences shows this more strikingly : 191 — — r w — w + 1 n n+1 00 0.01854 43. 0.02189 22.9 0.01362 29.7 0.03760 2.4 0.00732 3.G 0.01643 0.3 0.00226 1.2 0.00575 2.5 0.00965 0.4 0.00479 The relation exhibited in this table supports the supposition that the size of the drop varies inversely as some function of the figure bounded below by a circular horizontal tangent plane of coifttant diameter, (less than that of the sphere), la- terally, by a cylinder of vertical axis' standing on the tangent plane and cutting the sphere, and above by the convex sur- face of the sphere. Fig. IV. As the diameter of the sphere still further diminishes, the size of the drop is limited by the possible size of its base : un- till finally the sphere is completely included in the drop. It would be interesting, but it would take us too far to consider the various cases of liquids dropping from cones ed- ges, solid angles, cylinders, rings &c. We must content our- selves, in this direction with the fact that the size of a drop is greater the more nearly plane is the surface from which the dropping takes place. If it were possible for a drop to fall from a concave surface we would anticipate a still further in- crease in its size. The relation between drop-size and curvature may be more strikingly shown by arranging the spheres one above the other in the order of magnitude Fig. Y. Each sphere receives the drops from the higher one. The quantity of water which drops in a given time, is the same for each sphere. Hence in every case the number of drops is inversely as their size, So — 192 — that by counting the numbers of drops which fall from any two spheres in the same time, we get at once the relative sizes of the respective drops. For several reasons this plan of comparison is not sufficiently accurate to measure drop sizes, but it offers a method for making the difference of drop size visible to any number of persons at once. The only other variation in the geometrical relation be* tween the solid and the liquid which we shall consider is the variation in the size of a circular horizontal plane from which drops fall. • g A Q Five discs of copper foil were cut of the radii '20 ^0 2 1 \ — ^ ~ , of an inch respectively. These were fastened hori- zontally to vertical wires and having been thoroughly cleaned by momemtary immersion in nitric acid and washing, water • was made to drop from them as before, at the rate gt.— 2” Table X shows the influence of this kind of variation upon drop size. The want of accord in the numbers of the largest disc is owing to a peculiar tremor which the drops exhibit at the moment of delivery. The same phenomenon occured also but to a less extent with the next smaller disc. With the VC' mainder it was not noticeable. — 193 — TABLE X. gt. = 2”. T = 23^ C. Water. 1. 2. 3. 4. Radius of Disc. Number of Drops. . r 20 in. 20 0 < 20 20 20 L 20 • r 20 ,m- i 20 if ■< 20 20 20 Weight of Drops. 3.3682 3.1193 3.2523 3.3256 3.2594 j 2.9693 2.9854 > 2.9746 3.0031 Mean Weight and relative size of single drop. 0.16325 0.14915 in. 3 -< 20 in. A < 20 in. 1 < 20 20 20 20 (vV/ 20 20 20 20 20 20 20 1.9333 ~ 1.9244 1.9504 1.9248 1.4618 " 1.4672 1.4688 1.4682 0.8250 T 0.8212 0.8208 0.8190 0.09666 0.07332 0.04107 The curvature and shape of the Solid and its consequent massing towards the liquid is intimately connected with the next phase of variation which we shall consider, to wit, the variation in the chemical composition of the solid from which the drop falls. The influence of this kind of variation is to he studied bv examining the size of drops, formed under like 194 — circumstances from spheres of the same size but made of dif- ferent material. Since, in this case, the liquid remains the same, Ave must limit the solids examined to such as the given liquid completely wets. In this case variation in the drop size implies a variation in the thickness of the liquid film covering the solid. The latter must be caused by variation in the adhesion between the solid and liquid. Finally such adhesion can only vary through one or both of two causes, namely variation in the density of the solid or in its specific adhesion dependent upon its chemical nature. The first qualitative experiment was made upon three equal spheres of Brass, Glass and Cork respectively. They were hung one above the other in the manner before described, so that the drops from one fell upon the lower one.* It was found that, in whatever order the spheres were arranged, when the flow was uniform and not quicker than gt — 2”, the dropping from the Cork took place with the greatest ra- pidity, that from the Glass next and that from the Brass most slowly. Showing that the brass gives rise to the largest, the glass to the next largest and the cork to the least drops. From this it would seem that the drops are in the same order as to size as arc the solids as to density. We shall find how- ever that this is not always the case : and that some other property as well as density is at work to influence the drop- size. i The quantitative experiment, the results of which are given in Table XI confirms the results of the qualitative ex- periment given above ; but shows, at the same time that the joint influences of density and chemical diversity of the solid have only a trifling effect upon the drop-size. The condi- tions of the experiment were similar to those previously des- cribed. * In this kind of experiment there should be a considerable mass of cotton wool on each sphere to receive the drops from the higher noe and, by acting as a reservoir, to regulate the flow- 195 — TABLE XI. i mm. Water r/t. = 2”. T=22w.9 C. r. — 7. 1 Number of drops =20. Substance. Weight of 20 drops. Mean weight of single drop Cork Glass Brass r i 1 L < 2.4846 2.48 18 2.4832 2.4789 2.4821 2.4877 2.5930 2.5985 2.5989 2.5949 2.5953 2.5900 2.6225 2.6229 2.6260 2.6295 2.6296 2.6116 S- 0.12418 > 0.12975 0.13118 When a liquid drops from a solid it is not always that the adhesion between the solid and liquid is overcome. The phenomenon of wetting ” implies a superiority of the adhe- sion between the solid and liquid over the cohesion of the li- quid : and in all cases where a liquid drops from a solid which it wets, the act of separation is a disruption of the liquid and not a separation of the liquid from the solid : that is, the sepa- ration is a failure of cohesion and not of adhesion. We arc not, however, on this account, justified in anticipating that the size of a drop is unaffected by the chemical nature of the solid from which it drops, even in those cases where the ad- hesion between the solid and liquid is greater than the cohe- sion of the liquid, that is, where the liquid completely wets the solid : because although it is the liquid which is broken, yet — 196 the size of the broken off part or drop depends in great mea- sure upon the thickness of the residual film, as we have seen in examining the influence of the growth time, and the radius of curvature. Adhesion may also exist between a solid and a liquid which does not wet it, as when a drop of mercury hangs from a glass sphere. 13 ut the cohesion of the liquid in such a case, by its effort to bring the liquid to the spherical form, and the weight of the drop so modify the adhesion between the solid and li- quid by altering the size of the surface of contract between the two, that the size of the drop gives no direct clue to the cohesion of the liquid. We may now examine a few cases in which, the size of the sphere remaining the same and its density in some instances nearly so, the matter of the solid varies ; the liquid however wetting it in all cases. This Avill show whether the differences of Table XI are due wholly to differences of density of the solid or also or wholly to differences of chemical constitution. Equal spheres of the substances were made by casting them in the same bullet mould. The surfaces of the metals were roughened by momentary immersion in acid : Tin and Anti- mony in Hydrochloric and the others in Nitric acid. Without this precaution a metallic surface is apt to be wetted only lo- cally, the base edge of the drop is irregular and inconstant and the drop -weight varies. Indeed with some metals such as Tin, a smooth and bright surface is scarcely wetted by water. As the bodies examined have different coefficients of ex- pansion by heat ; and one of them expands on solidification, it was necessary to test the equality of their size and remedy any inequality. This was done by arranging three of them one at each corner of small equilateral triangle drawn on a large piece of plate glass. Another piece of plate glass was then placed upon the spheres, so as to rest on all three and was slightly loaded. On passing a gauge between the plates at their edges, the slightest inequality of the spheres could be detected because the gauge lifted the plate off the smallest 197 of the three balls, which could then be moved. The larger spheres were then reduced in size by brisk agitation in acid. The sulphur and phosphorus were for the same purpose wash- ed with ether. TABLE XII. nuu. Watery. = 2”. T = 23° C. Radius of Curvature = 7 1. II. III. IV Substance. Antimony -< r Sulphur Cadmium Zinc Lead 1 Phosphorus Bismuth ■< Tin 1 J Weight of 20 drops. 2.3905 2.3980 2.3968 2.4016 2.4019 2.4067 2.4046 2.4063 2.4022 .2.4462 2.4387 2.4374 2.4358 2.4495 2.4481 2.4518 2.4478 2.4522 2.4525 2.453 2.4528 2.4532 2.4564 2.4528 2.4584 2.4580 2.4589 Mean weight of single drop. > J 2.4843 2.4864 2.4829 2.4861 } 0.11984 0.12021 0.12185 0.1224-6 0.12264 0.12274 0.12285 0.12425 Specific Gra- vity of Solid. 6.80 .00 8.70 6.86 11.44 J.08 9.90 7.29 — 198 — Although there is only slight difference between the conse- cutive terras of column 3, yet between the extremes of Anti- mony and Tiu, a well-marked difference exists. This table shows that the drop size stands in no simple rela- tion either to the equivalent, density, or chemical character of the solid : and establishes the existence of a specific adhesion, independent of these. Although the differences of table XI may be partly owing to the difference of density of the so- lids, cork, glass and brass, yet we see from XII that there is about half as great a difference between the sizes of drops from Antimony and Tin as between those from Cork and Brass : although the difference of density between the first two is small compared with that between the last. Again, Sulphur gives rise to drops intermediate between those of Antimony and Cadmium. Without therefore venturing to assert that density is with- out influence on drop-size it is clearly proved that it does not exert the most powerful influence. We have finally to examine the direction and extent of al- teration in drop- size caused by change of temperature. A change in the temperature of the dropping liquid may affect the drop-weight without altering the drop-size, by altering the density of the liquid. It may further alter the drop-size by altering the size and therefore the curvature of the solid. Any error introduced by the first of these sources is elimi- nated by dividing the observed weight by the specific gravity at the proper temperature as in the case of different liquids at the same temperature : Errors from the second source may be certainly safely neglected, being far within the errors of observation. In the place where these experiments were made the range of natural atmospheric temperature is very small. From the coldest to the hottest season the difference scarcely exceeds 10° C. This circumstance made an extended and minute study of the influence of temperature impossible : by prevent- ing more than one observation at each temperature being made. 199 — The liquid taken was water and the solid was glass. The water was heated to the boiling point and placed in the appa- ratus Fig. III. The sphere from which the water fell was the bulb of the thermometer which measured the temperature. Fully the upper half of the sphere was covered with cotton wool so that the whole of the sphere was kept wet. The con- siderable mass of mercury in the bulb of the thermometer or dropping-sphere itself served to make more uniform the tem- perature of the drops : while the actual contact between these and the spherical bulb insured a tolerably close approxima- tion between the actual temperature of the drops and that in- dicated by the thermometer. Though the temperatures observ- ed cannot therefore pretend even to approximate positive ac- curacy : yet they are certainly in the actual order of magni- tude. The arrangement is seen in Fig. YI. TABLE XIII. mm Water, gt. — 2” r. — 7 A. Number of drops 20. Relative mean size Temperature Weight of Weight of of single drop, corrected for tern- Centigrade. twenty drops. single drop. perature. r 44.i 2.5564 0.12782 1 40.3 J 40 2.5795 0.12897 > 0.12985 [37 2.5826 0.12913 f35 2.6083 0.13041 1 33.9 2.6105 0.13052 32.6 2.6161 0.13080 31.2 2.5960 0.12980 30.6 0.69750 1.000 0.64619 5 3.4918 5 3.5015 l 5 3.5066 - r 5 3.4235 5 3.4215 - 5 3.4235 5 3.4285 Glycerine. . . «< 5 5 3.3627* 3.4088 * 0.61508 1.245 0.55793 5 3.4063 5 3.4329 • 5 3.4090 l 5 3.3981 J r 5 2.9418 5 2.4875* 5 3.0773 5 2.9888 Benzol .... < 5 5 2.9637 2.9549 > 0.59822 0.864 0.56014 5 3.0767 5 2.9583 5 2.9352 i lio 6.0144 J 1 r 5 2.1427 •> 5 2.1900 1 5 2.1883 5 2.1960 Turpentol . . < 5 5 2.1820 2.1620 » 0.43497 0.863 0.40715 5 2.1768 5 2.1791 1 5 2.1608 u 2.1708 — 309 — The salient points of Table XVI are chiefly these : (1) The drop-size of a liquid which drops under like con- ditions through various media , does not depend wholly upon the density of the medium and consequent variation in the weight, in the medium, of the dropping liquid. Thus glycerine whose density is above that of all the other liquids examined, does not, as a medium cause the mercurial drop to assume either its minimum or maximum size. (2) The liquids in TablejXVI are in the same order as in Table VIII. Jn other words. If there he two liquids A and B which, drop under tike conditions through air ; and the drop size of the one A be greater than that of the other B, th'en, if a third liquid C be made to drop thrrugh A and through B the drop size of C through A is greater than the drop size of C through B. (3) Further, on comparing Tables XIV and XVI it ap- pears that whether Avater or mercury drops through turpentol and benzol ; the drop through benzol is greater than the drop through turpentol. This avc shall aftenvards find confirmed in other instances into the Luav : If the drop-size of A through B be greater than the drop-size of A through C then the drop-size of D through B is also greater than the drop-size of I) through C. It is further observed that while mercury exhibits its larg- est drop when falling 'through air, water assumes its smallest drop size under this condition. This method of the examination of liquids by drop size which brings so prominently fonvard or comparatively slight difference between similar liquids may be used not only to detect commercial adulterations of one liquid by another, but perhaps to distinguish betAveen those remarkably related iso- meric liquid bodies, the number of which is quickly increas- •ng; and between Avhose terms the difference has until lately escaped detection. Of these bodies the first studied were the tAVO amylic alcohols ; but the greatest number at present knoAvn is amongst ^thejiydrocarbous. 210 — We may take an example illustrating the use of drop mea- surement in approximately measuring the proportion in a mixture of its two chemically and physically similar but not isomeric constituents. Suppose we had a liquid which we knew to consist wholly of a mixture of benzol and turpentol, and we wished to find the proportion in which these two ingredients were present. We could scarcely approach to an answer by any of the means hitherto employed. The specific gravities of the tivo liquids are so close (.864 — .863) that the density of the mix- ture would give us no substantial aid. Though there is a con- siderable difference (80 ° C.) in their boiling points, no one who is familiar with the difficulties of fractional distillation, would place any reliance upon a quantitative separation based upon volatility. Their refractive indices are nearly the same*. Their vapour densities 2.77 — 4.76, though comparatively dif- ferent are not absolutely very wide apart. They are active and passive towards most of the same chemical reagents, and interfere with one anothers reactions. If we have recourse to chemical analysis (C12 He, C20 IIig) a very small experimental error would point to a great difference in the proportion of the two. To find how far the stalagmometer Fig. VII is applicable in this case, it was filled with five liquids in succession, to wit : 1st. With benzol = B 2nd. With 2 parts benzol with 1 of turpentol = B2 T The time growth being brought in each ease to 5”, the number of drops of water required to fill a given volume was counted : allowance being made for the meniscus. # The Refractive index of turpentol is 1.47G : that of benzol does not appear to have been measured ; but that it is almost identical with that of turpentol is seen on mixing the two. In those cases in which I propose to use stalagmometer chiefly, namely with isomeric bodies the method by refraction is useless because isomeric liquids seem always to have the same refractive indices. 3rd. „ 1 „ 4th. „ 1 ,, 5 th. ,, turpentol 1 =BT = B T> — 211 — TABLE XVII. Through Air T bt2 BT B‘2 T B 102 51 38 34 31 14 102 51 37 34 31 14 101 50 38 33 31 14 49 Mean 101.7 50.2 37.7 33.3 31 14 Hence a difference of 16.(1 per cent in one of the constituents corresponds to an observed difference under the most un- favourable conditions of 3 drops. In other words the stalagmometer is sensitive to an alteration of 6 op. By increasing the capacity of the recipient it is clear that the drop numbers and therefore their differences might be in- creased at pleasure. Thus by counting the number of drops necessary to fill a volume 6 times the si/e we could tell to within one per cent bow much turpentol and how much benzol were present. But it is perhaps in the cases of the still more proximate identity mentioned above of isomeric bodies that the stalag- mometer may be used rather as a stalagmoscope, to render a difference of drop-size evident, than to measure it. From Table XVII we gather the general law concerning three liquids which are insoluble in and without chemical action upon one another. If a liquid A drop under like con- ditions in succession through two liquids B and C, then its drop-size through any mixture of B and C is intermediate between its drop size through B and its drop size through C and the greater the proportion of q in the mixture, the more nearly does the drop size of A through the mixture approach to the drop size of A through ^ alone. We have already examined the influences on the drop size: in theca.se s L (! of the density of (he dropping liquid. — m — persistent und stubborn cohesions respectively, increase in the former two tends to diminish the drop size — increase in the last, to diminish it. Let us examine in like manner the influence of the similar properties of the medium : — (1.) The density of the medium. Increase in the density of the medium is equivalent to diminution in the density of the dropping liquid and must therefore be followed by a ten- dency to increase in the drop -size. (2.) Stubborn cohesion of medium. The resistance to dis- placement or stubborn cohesion of the medium tends to keep back the drop in its place and makes it necessary for a larger quantity of the dropping liquid to accumulate, that is, it in- creases the drop-size. (3.) Retentive cohesion of medium. The same force of persistent or retentive cohesion which causes the drop of a liquid to take the spherical form, would also cause the liquid to give or tend to give a spherical form to an irregularly shaped volume of a solid, liquid, gas or vacuum in it. Thus gas- bubbles, in liquids have an approximalv spherical form not by reason of the cohesion of the parts of the gas, but from the cohesion of the medium which moulds the gas into that form by which the cohesion of the liquids is most gratified. Hence increase in the retentive or persistent cohesion of the medium tends to diminish the dropsizc of the dropping liquid. In all cases of SLL, we may represent the direction the determinants by the following scheme, in which the sign -f denotes a tendency to increase, the sign — a tendency to diminish the drop size. SLL. DRorn.NG + ! Stubborn cohesion. .MEDIUM 4* Stubborn cohesion. Density. LIQUID. Persistent cohesion. Density. LIQUID. Persistent cohesion. This scheme is verified by the experimental results obtain- ed. Of all liquid^ water forms the largest drops in falling through air because in it, the stubborn cohesion prevails to the greatest degree over the joint action of persistent cohesion and weight. In water mercury forms drops greater than in all other liquids because in water (as a medium) stubborn cohesion and weight prevail to the greatest degree over per- sistent cohesion. The case SLL may be inverted if the drop forming liquid be specifically lighter than the medium liquid. Thus every case of SLL which we have examined in which a liquid A drops downwards through a liquid 13, has a countercase in which the liquid B* drops upwards through the liquid A. In order to measure the size of such ascending drops, the stalagmometer fig. VII is modified in form. It is not found possible to cause the dropping liquid to adhere with sufficient completeness and uniformity to a solid sphere immersed in the denser medium in the cases experimented on. The end of the syphon A was turned upwards and served as the solid whence the liquid dropped without the interposition of a sphere or other solid. The measuring tube D was removed from the neck of the cup C a stopper being inserted in its place. The cup C was filled with water and the measuring tube I) being also filled with water was inverted into it and held by the holder H. The modified stalagmometer is seen in fig. X. Care was taken that the end of the syphon A should always be at the same depth beneath the surface of the water in C. The drop-sizes of the liquids of table XYII were first exa- mined by this stalagmometer. The following Table XVIII shows the number of drops of the various liquids dropping through water required to fill the measuring tube up to the given mark. The mea- suring tube here employed was different from that used in * «.'ea bitfoduchou. forming table XVII ; on tins account and because the deliver- ing solid was quite different in shape and gt.—Z” no im- mediate comparison can be made between Tables XA III and XVII. Correction is made for meniscus. TABLE XVIII. gt. = 2” — T = 21°. 2 C. 286+1 251 + 1 228 + 1 204+1 102 + 1 minimum 286+1 351 + 1 230 + 1 204+1 103 + 1 286+1 250+1 229+1 206 + 1 102+1 286 250.7 090 204.7 102.7 .287 251.7 230 205.7 103.7 We gather from this table a law quite similar to that deduced from the measurement of the size of the dovvnvvavd drops of water through these same liquids ; it is as follows : The drop size of any mixture of two liquids A and B dropping upwards through a third liquid C is intermediate between the drop size of A through C and that of B through A. C and the greater proportion of ^ there is in the mixture the more nearly does the drop size of the mixture approach to the drop size of alone. It is remarkable that supplementary drops are formed in the cases immediately considered, just as in the case of water dropping through these same liquids. But the supplementary drops of benzol and turpentol through water bear a much smaller ratio to the main drops than do those of water through benzol and turpentol to their maindrops. .J udging only from the equality in their rate of ascent through the measuring tube, all these supplementary drops are of very exactly the same size. The supplementary drops were not further examined, but were always collected and measured with the main drops. Viewed as a means of quantitative chemical analysis, the measurement of the drop size of liquids which drop up through water is yet more sensitive than that of the drop sizes of water falling downwards through the liquids. Thus, from Table — 215 — XVII, the least proportional difference of drop number, cans- ed by an alteration in the proportion of the liquids, is between T and B T2 where a diminution of 33.33 per cent in the tur- pentol and an addition of 33.33 per cent of benzol causes a difference of 35 .3 in the drop number. Liquid T BT2 BT B2T B Percentage . . " B . T 0 33.33 50 100 66.66 50 66.66 33.33 100 0 Difference of") L B 33.33 16.66 16.66 33.33 Percentage. . J r t 33.33 16.66 16.66 33.33 Difference of'1 drop-number 35.3 21.7 24.3 102.0 Or this stalagmometer shows the composition of the liquid to within 1 per cent. Further if the mixture contains less than one-third of benzol its proportional composition can be determined, on an average, to within 0.33 per cent. It may be noticed wfith regard to SLL that the value of gt is of much less influence upon the drop size than in the case of SLG. It is generally sufficient in the former case that the average value of gt should be constant. This is especially the case when the drops are found from a tube (as the end of a syphon) and not from a convex solid. The reason is ob- viously that in the former case the thickness of the residual film upon which we have seen the drop-rate depend is at all rates indefinitely great while in the latter it depends upon the rate of supply. In order to compare the drop size of A through B with that of B through A under quite similar conditions : the syphon A of Fig X was inverted and applied to the cup stalagmometer of Fig. VIII. The arrangement of the end is seen in Fig. XI. In using this form of stalagmometer the end of the de- livery syphon must be at first wiped dry, so that the water may not creep back outside the syphon, and so give rise to an irregular base to the drop. Water was made to drop through A Fig. XI at the same rate gt~%” and through the same li- quids as before, to wit T, BT9. BT, Be T, B. The same — 216 — measuring tube was used as in Fig. X or Table XVIII and was filled to the same point. Correction was made for meniscus. TABLE XIX. (ft. = 2”- — T = 24 ° . 5 C. T bt2 BT Bo T B 25G 218 178 162 87 256 220 177 164 86 256 • • • , , 86 • • 86 256 219 I / / .O 163 86.2 We may now compare'Tables XVIII and XIX since the conditions of the experiments whence they are got arc iden- tical. The drop sizes are inversely as the drop numbers. Let us use the symbol Xy to denote the drop size of the liquid X in the medium Y, and XZy the drop size a mixture of X and Z through Y and so on. Comparing first the size of a drop of X through medium Y with the size of a drop of Y through medium X or finding the value of we have, putting W for water. TABLE XX. wB 103.7 — i— 1 .203 Bw 86.2 w n T 2 205.7 — — - — : 1.262 Bo Tw 163 WBT 230 — . — — — — : ; = 1 .296 BTW 177.5 WBT o 251.7 • 1.149 BTo 219 W WT 287 1.121 — 217 — Hence in none of these cases is the drop size of one li- quid through another equal to the drop size of the second through the first. We get the general law that. That if a li- quid X has a larger drop she than the liquid Y in the liquid Z then the liquid Z has a larger drop size in X than it has in Y. Further if a, liquid X has a larger drop size than a liquid Y in air; then the drop size of X through Y is larger than the drop size or Y through X. Further if the drop size of X be greater than the drop size of Y and the drop size of Y greater than the drop sizes of Z, then the ratio between the drop sizes of X in any mixture of Y and Z and the drop size of that mixture of Y and Z through X Is greatest when the ratio between Y and Z is unity. Further comparing the drop -sizes of Table XVIII with one another or all with Bw wc get : XXI. Bw 287 2.767 Tw 103.7 Bw 251.7 2.427 BTj 103.7 W Bw 230 _ — — r — -1^ .2.227 BTw 103.7 Bw 205.7 3 .983 B3Tw 103.7 Bw * 103.7 1.000 Bw 103.7 In like manner, comparing the drop-sizes of Table XIX with some another or all with W'b, we have : W B 256 WT 86.2 WB 219 % 2.541 318 WBT o 86.2 WB “ 177.5 — — = 2.059 Wet 86.2 Wb 163 — 1.890 Wb t o 86.2 WB 86.2 — — — — 1.000 Wb 86.2 ly, on comparing these figures with those of Table XXI, we get the remarkable law which it would be difficult to express in words, that WB Tw WB BT2 WB BTW WB B2 Tw w Wt Bw WBt Bw Wet Bw Wb t Bw 2 2 — 1 nearly. The main results obtained with regard to drops may be collected into the following laws : 1. The drop-size depends upon the rate of dropping. Ge- nerally, the quicker the succession of the drops, the greater is the drop. The slower the rate the more strictly is this the case. This law depends upon the difference, at different rates of the thickness of the film from which the drop falls. 2. The drop size depends upon the nature and quantity of the solid which the droppiug liquid holds in solution. If the liquid stands in uo chemical relation to the solid, m general the drop size diminishes as the quantity of solid cont ained in the liquid increases. The cause of this seems to be thatthe stubborn cohesion of the liquid is diminished by the solution of the solid. Where one or more combinations betweeu the liquid and solid are possible the drop size depends upon indeterminate data. 3. The drop size depends upon the chemical nature of the dropping liquid, and little or nothing upon its density. Of all liquids examined water has the greatest and acetic hydrate the least drops. 1. The drop size depends upon tlie geometric relation be- tween the solid and liquid. If the solid be spherical, the larg- est drops fall from the largest spheres. Absolute dilference in radii takes a greater effect upon the drops formed from smaller than upon those from larger spheres. Of circular horizontal plates, within certain limits the size of the drop varies directly with the size of the plates. 5. The drop size depends upon the chemical nature of the solid from which the drop falls ; and little or nothing upon its density. Of all the solids examined Antimony delivers the smallest and Tin the largest drops. 6. The drop size depends upon temperature. Generally, the higher the temperature, the smaller the drop. With water the effect of temperature for a difference of 20° C. is very small. 7. The nature of the gaseous medium has little or no effect on the drop size. SLL. 8. 'l'lie drop-size of a liquid which drops under like condi- tions through various media, does not depend wholly upon the density of the medium, and consequent variation in the weight, in the medium of the dropping liquid. 9. If there be two liquids A and B which drop under like conditions through air ; and the drop size of the one A be greater than that of the other B ; then if a third liquid C be made to drop through A and through B, the drop-size of C through A is greater than the drop size of C through B. 10. If the drop size of A through B be greater than the drop size of A through C, then the drop size of D through B is also greater than the drop size of D through C. 11. If a liquid A drop upon like conditions in succession through two liquids B and C then its drop size through any mixture of B and C is intermediate between its drop size through B and its drop size through C, and the greater the proportion of ^ in the mixture the more nearly does the drop size of A through the mixture approach to the drop size of A through ^ alone. 12. The drop size of any mixture of tuo liquids A and 11 droping through a third liquid C is intermediate between the drop size of A through C and that of B through C, and the greater the the proportion of ^ in the mixture the more B nearly does the drop size of the mixture approach to the drop- ing of alone. 13. If the liquid X has a large]’ drop size than the liquid \ in the liquid Z. Then the liquid Z has a larger drop size in X than it has in Y. 14. If a liquid X has a larger drop size than a liquid Y in air ; then the drop size of X through Y is larger than the drop size of Y through X . 15. If the drop size of X be greater than the drop size of V in air and the drop size of Y greater than the drop size of Z in air ; then the ratio between the drop sizes of X in any mixture of Y and Z and the drop size of that mixture Y and Z through X is greatest when the ratio between Y and Z is unity. m ANNUAL MEETING OF THE ROYAL SOCIETY OF ARTS tc SCIENCES. WEDNESDAY, 29th MAECH 1865. H. E. SIR HENRY BARKLY, K.C.B,, E.R.S., IN THE CHAIR. Present at tlie Meeting : — The Hon’ble Sir Gabriel Fropier ; the Hon’ble C. W. Wiehe, Vice-Presidents; A. Desenne, Trea- surer ; L. Bouton, Secretary ; F. Dick, Vice-President. The Hon’bles H. Leraiere and H. Pitot, Messrs. E. C. Bewsher, Ed. Bouton, W. Connor, L. Estourgies, E. Fleurot, L. Hugues, J. Kyshe, P. Lemiere, Ch. Magnv, A, Mont- gomery, V. Naz. The Secretary read the following Report : — An apology is due to Your Excellency for the delay in the annual meeting of the Royal Society of Arts and Sciences. The Committee appointed by Your Excellency from the members of the Society, to carry out the wish of the Secretary of State that Mauritius should not be unrepresented at the Dublin Exhibition, had to enter at once upon the duty of collecting the various products of the Island with sufficient despatch to enable them to reach Dublin in time, as no goods and articles could be received after the 15th of April — the Exhibition opening on Tuesday, the 9th day of May. These articles, contained in 16 cases, were successively despatched in the steamers which left on the 24th January, 7th and lStli February. They consist of the beautiful sugars of Labour donnais , La Gaiete, St.-Aubin, Benares and Schoen- fekl Estates — of vanilla grown by Messrs. J. Levieux and N. Brousse ; of cotton and tobacco, both in leaf, in carrots and cigars ; of tanned hides, specimens of textile fibres and medi- cinal plants ; specimens of rope-making and fancy rattan works by the young Indian Orphans of the Government Asylum at Ponder Mills, besides other articles of which the Committee intend to lay a more succinct account before Your Excellency. Your Excellency kindly acceded to the request ot the Secretary that avantage might be taken of the departure of — 222 — the Government steamer Victoria and of H. M. S. Rapid, to form a collection of plants from the dependencies of Mauritius. An old employe of the Society, familiar with the occupation, accordingly took his departure, and after an absence of two months, returned with a sufficient quantity of plants to enable us to form an idea of the Flora of Rodrigues, Diego, Peros Banhos, and of Mahe, one of the Sechelles Islands. It is to be regretted that the other islands of the Seychelles group were not explored, but circumstances beyond the control of the collector prevented it. The plants thus collected have been prepared by your Se- cretary for transmission to Sir W. Hooker, and the specimens of Ferns from those Islands have already been forwarded to Kew, by the Orontes, in care of Dr. Roch, Surgeon, R. A. Your Excellency encouraged the Secretary to forward to the Director of Kew Gardens, a sufficient quantity of plants to form materials for a Flora of Mauritius. He has according- ly sent at different times a large number of Phsenogamous which grow in our forests, and of such as have become na- turalised by length of time. Other specimens had already been received, especially those collected by our much esteem- ed friend the late Dr. Ayres. We also notice, in a Report on the progress and condition of the Royal Gardens, during the vear 1863, that the collection made in our Island about 30 years ago by the late Judge Blackburn, one of the former Presidents of our Society, have also been presented to Kew by Admiral Sir W. Bowles, K.C.B. These successive contributions must have formed a large nucleus of Mauritius plants, and must now supply, a sufficien- cy of materials, notes, and observations for the commence- ment of a work which is wanting, and which there is no doubt that our Plonorable Patron, Sir Henry Barldy, would gladly see undertaken. An interesting collection and which, of itself, comprises a fourth of the Flora of Mauritius, viz., the Ferns, is in the course of preparation by the Secretary. This collection also is intended for Kew. Notes and obser- vations, we confidently hope, will not be wanting. Sir Henry and Lady Barkly who have carefully studied the Ferns of our Island and those of the Sechelles and Rodrigues, will doub- tless communicate the results of their own observations to Sir W. Hooker. The wish expressed at our last annual meeting that the Cinchona plant should be introducted into Mauritius, was nearly realised. Your Excellency procured from Madras a ca- se of plants of that tree. Unfortunately, taken up too young, — 223 — they were unable to bear the voyage, and died before they reached Mauritius. The disappointment is a great one. Expe- riments would have been settled or nearly so : whether or not, certain elevated parts of our Island were suited for the culti- vation and subsequent naturalisation of the Cinchona. The Exhibition held in September last, with Your Excel- lency’s permission in the garden attached to Government House, presented rather a brilliant show of fruits, dowers and regetables. The committee, under the direction of its President, the Hon. Mr. Ch. Wiehe, and of Mr. Henry Jourdain, its Vice- President, and with the valuable assistance of the Judges, made the arrangements and the disposition of the articles ex- hibited as complete as possible. That which had never been accomplished, if we except the Intercolonial Exhibition, was this time effected ; the medals and prizes were distributed on the very day of the Exhibition. The plants and dowers exhibited by Mr. Constant Van- keirsbilck and by Mr. Eug Duponsel, and the cut dowers from La Bourdonnais and other places, were remarkable for their beauty -and freshness. Lady Barkly contributed to the pleasure of the occasion not only by her presence, but also by her cooperation, — the collection of Ferns, both indigeneous and exotic, was justly rewarded by a medal. Dr. Guthrie presented to the Society a very interesting- paper, which was afterwards printed with the proceedings of the Royal Society of London. He gives an exact description of the various volumes of what are commonly called Drops. “ This,” observes Dr. Guthrie, “ may at drst seem a trivial matter, but it is nevertheless in several points of view, a subject of importance, principally to the physician and phar- macist.” It is evident that the exact quantity contained in a drop should be well-known, when a prescription is made out, in which a substance enters that requires to be measured drop by drop, the more particularly when that substance possesses the most energetic properties. It is the same with the bubble given out by certain gases, which present the same conditions and arc subject to the same rules as drops. The volume of a drop depends upon the nature and quan- tity of the solid matter held in solution, and the chemical nature of the fluid. Of all the liquids subjected to examination by Dr. Guthrie, water gave the largest drops, and acetic acid the smallest. The instrument used by Dr. G. to measure drops and which was shewn by him to the Society was named by him Stcdagmometer , from the Greek words signifying Drop and Measure. Another paper not less remarkable, although of a different nature, viz. : A memoir on the “ Pou a poche blanche,” by Dr. leery, was presented by the author. It is accompanied with drawings from nature of the insect, magnified by a powerful instrument. It fully deserves the enconiums bes- towred by the Society, both on the author and on Mr. Desjardins who executed the drawings under the direction of Dr. leery. The “ Pou h poche blanche” had already been the subject of examination by Mr. Westwood F. L. S., from specimens forwarded to him by the Secretary. Mr. Westw ood says it be- longs to the genus Coccus, of which the species are very nu- merous. Dr. leery proposed that it should form a new genus to be called G aster alphus, a name which indicates the protu- berance which constitutes the external form of the insect. The Society, through its President, thanked Dr. Guthrie and Dr. Icerv for their papers which were ordered to be prin- ted with the Transactions of the Society for the present year. The Secretary read extracts from a paper published by Dr. Hooker in a number of the “ Natural Historv Review, ” on a subject which is not new’, but to which he attaches great im- portance, viz : the replacing in countries and colonies which are in frequent communication with European or other coun- tries, of certain indigeneous plants by plants from the other countries. “ It must be long, “he says”, 1 efore facts enough to theorize “ upon can Ire collected. Meanwhile, the inquiry appears “ perhaps the most interesting and important in all Biology, “ and as such it is most earnestly to be desired that all that “ are favorably circumstanced to pursue it, will do so both “ systematically and very carefully:” It has been in the power of your Secretary, so far as -Mau- ritius is concerned, to test the correctness of these assertions. He has been able to point out several exotic plants which have taken possession of our soil, and which have grown in such profusion in retired spots, in the borders of our forests and on our mountains, that strangers to the Flora of Mauritius would believe them to be indigeneous. The Secretary has also pointed out the fruit trees, w hich adorn our orchards, some of which such as the guava, the mango, the custard apple, the strawberry and the raspberry are to be seen growing w ild in different parts of the island. On the other hand, several indigeneous plants have become extremely scarce, either through the destruction of the forests, or from other cause. The same remarks mav have suggested themselves to Your Excellency. There Avas formally, say, twenty or twenty-five years ago, to be found in the Kcduit — 2:25 — Cascade, the Eg uise turn elongatum, the only representative in Mauritius of that genus Equisetum, and which is no longer in existence, at least, in that locality. It is the same with some herns mentioned in the Hortus Mauritianus of Bojer. Dr. Hooker mentions not only plants, but also animals, some too that occupy no inferior position in the animal king- dom, and which when introduced under favorable conditions, for their reproduction in a country, become in some measure indigeneous. New insects have increased the number of these in existen- ce in our Island ■ Butterflies from Madagascar are to be found even in the streets of Port-Louis, in greater number than these that are indigeneous. Other insects including the Borer un- voluntarily introduced from Ceylon and the Foil Blanc, have increased with such fearful rapidity as to threaten our prin- cipal agricultural productions, and spread alarm among our planters. As for Birds, Mr. Ed. Newton is of opinion that out of about thirty species which constitute the Ornithological Fauna of Mauritius, 15 have been imported and the remainder are indigeneous. Amoung the latter some as the Merle (1), the Cuisinier (2), the Ferruche (3), the large Rainier (4), the Rainier (5), and the Cateau (6), are becoming scarcer and scarcer every year — without it being possible to ascribe any cause for their diminution, unless it is to be attributed to the destruction of our forests. Two others, the Dutch Pigeon (8) and the Hoopoe (8) which are said to have existed in the Is- land, have entirely disappeared. Among the exotic birds, some are more numerous than others. The Pingo (9) and the Bengali (10) are to be found every where. The partridges (11) are pretty common in many localities. As for the Martins (12), this is what Mr. New- ton says about it : “ The Martin is far the commonest bird, indeed I think it is more numerous than any specie of bird I ever saw. That is to say there are more Martins per acre in Mauritius than any other specie per acre I have ever seen. ” (1) Hypsipetes Olivaceus. (2) Oxynotus Ferruginous. (3) Agapornis Cana. (4) Trocaza Meyeri. (5) Turtur Picturatus. (6) Palaornis Eques. (7) Alectroasnos Nitidissima. — (8) Fregulupus Madagascaricnsis. (9) Munia Punctulata. — (10) Estrelda Astrild. , , . , ( Francolinus Madagascariensis — Perdrix Pintadee. • ' l Francolinus Ponticerianus — Perdrix Bouge. (12) Acridotheres Tristis. — 226 — Mr. F. Dick called the attention of the Society to the active principle which would probably be found in the nest and exu- viae of an insect belonging to the order of Nevropters” and known in every hot quarter of the globe where it commits great ravages, viz : the Caria or white ant Thermes destruc- tor ” of Fabricius. It is well known that a few years ago, it was made use of as an infusion or decoction for the treatment of certain ner- vous affections, particularly epilepsy, and that if no cures were affected, the condition of the patients was improved. Mr Dick drew the inference that the matters extracted from the wood by the Caria itself might contain some principles similar to those which are found in chloroform or other anestctics. Hut, the medical question apart, Mr Dick was desirous that the analysis of the nest should be made, in order to ascertain, what substances arc extracted from the wood,, which might lead to the discovery of a means of arresting the ravages of this destructive insect. Mr Fleurot was requested by the So- ciety to undertake the task ; his analysis has thrown a broad light on the subject, and furnished results very curious and interesting. It has proved tlxc presence in remarkable proportions and in rather considerable quantities, of formic acid iti combina- tion with iron, in the head and mandibles of the insect. Mr Fleurot is of opinion that the sedative effects of the Caria's nest are due to the combination of the iron and formic acid, which produces a formate of iron. The result leaves no doubt as to its value in the treatment of certain nervous affections, and Mr Fleurot considers that it may be ranked as a new therapeutic agent. The anlaysis of the nest and of the insect left no traces of soluble salts or common salt, so generally diffused and which is found in all animal substances. Mr Fleurot draw the infe- rence that the nature of the insect being antipathetical to common salt, it may be combated with that substance. lie traced a circle of salt, in which he enclosed some white ants and they did not dare to cross the barrier. New facts support- ed his assertion . He has been informed that in some damp cellars where the white ants caused great destruction amongst the casks of wine and beer, they had been entirely driven away by strewing a layer of common salt under the barrels, lie al- so ascertained that salt meat casks have never been known to be touched by them. Mr Fleurot has thus established that common salt is the best means hitherto discovered of preservation from the at- tacks of the white ant. Several products of the analysis of the Thermes Destructor , and a magnified drawing of the in- sect were presented to the Society- Mr Fleurot’s paper attracted the lively interest of the mem- bers. It has established two important points : lo. The disco- very of a new therapeutic substance — formate of iron — with which it is hoped to combat with success certain nervous affections that are so common in our enervating climate and 2o. The discovery of an easy mode of driving away the insect. On the other and, Mr Beyts has communicated to -the So- ciety an extract from the “ Gazette of India ” dated 8tli Octo- ber 1864, of a letter by Dr. E. Bonavia, honorary Secretary to the Agricultural and Horticultural Society. “ In the site,” he says”, where the central jail is erected, the white ants exist in unlimited numbers, and they cat through the plaster in or- der to get at the cow-dung, so that the walls require to be constantly re-plastered.” “ Some time ago, Mr Marshall, the jailor, was getting so- me floor made from the fibres of the American aloes (Agave Americana), and he found white ants did not touch mats from this fibre. On the countrary, they always destroyed mats made from other materials. “ I then asked him what use he made of the pulp which is separated from the fibre of the aloe leaves. He said it was thrown away. It struck me that it might be very profitably used for mixing up with the clay and cow-dung used for plas- tering the jail wnlls, as then probably the white ants would not touch the plaster. The experiment was tried and quite answered the purpose. Plaster which was impregnated with juice and pulp of- the aloe leaves has stood for months, and is not yet touched by white ants, while the plaster of walls free from aloe juice becomes covered with white ants, shortly after it is put on.” I crave indulgence for all these 'details, but if we consider how extensive are the ravages of this insect, , and the destruc- tion with which some of our large buildings arc threatened, we cannot lay too much stress upon the means of conquering so formidable an enemy, and should seek every possible remedy. The Society has received through the Colonial Secretary’s office, a circular from the Secretary of State, shewing, in a series of tabulated statements, the decreasing importations into the United Kingdom of rosins and turpentine since the American war. The London Board of Trade have considered the matter to be of sufficient importance to be brought to the notice of the Secretary of State with the view of its being communicated to the different possessions of the British em — 228 — pire, in order to ensure a supply of these articles being received, the want of which is being felt in England. We can hardly, now that our forests once so dense, have been thinned, find a sufficient quantity of rosinous trees to form an article of trade. The Secretary has however pointed out several that yield rosin, for instance : the Colophonia Mauritiana, Marignia obtusifolia, Calophyllum Ratamaka §c. Sir Gabriel Fropier has reminded us that several plants of the genus Eucalyptus have been introduced from Australia. Our former President, Mr. R. W. Rawson, now Governor of Bahamas, being the first to set the exemple. But they are not iu sufficient number to fulfil the ends for which they were introduced into the Island. As to Turpentine, alcohol is known to be a substitute for it. A legislative enactment has even permitted its introduc- tion into England, duty free, but on condition that it should be mixed with a substance Avhich renders its use loathsome. Dr. Guthrie has suggested that spirits of wood should be mixed with the alcohol, but Mr. Fleurot remarked that it would only be obtained by the combustion of a considerable quantity of wood, and that Petroleum oil might be used, which is imported in considerable quantities from America. His Excellency the Governor has also forwarded to the Society a circular from the Society of Acclimatisation of London. A similar Society is in existence in our island. Several of our members belong to it, and overtures have been made to us with a view of placing it in communication with a commission selected from the members of our Society. We must then await a favorable time to furnish our replies to the various questions of the London Society. Similar questions were addressed to the Secretary of our Society during the administration of the late Sir William Stevenson. His reply is dated 28th April 1862. Mr. Constant V ankeirslbick presented au Hygrometer of his own sugestion, a filament or Arista of the seed of Erttlium Gruinum, a plant recently introduced by Mr. Constant V. himself, being substituted for hair. This filament from its elasticity and sensitiveness to atmospheric influences, may serve to determine the state of the ambiant air. It constitutes an instrument as simple as it is ingenious, to indicate, like the hygrometer, the exact state of saturation of the atmosphere. Mr. Fleurot presented specimens of Carbonate of Lime from Diego Suarez. Other specimens of this chalk were also collect- ed by Isidore Legentil, at Rodrigues. It exists, in the opinion of Mr. Fleurot, in sufficient abun- dance iu those Islands to fill the purposes in Mauritius, for which it is imported from Europe ; either as an improvement to the soil in certain localities or for industrial purposes, in the painter’s and glasier’s trade, or for the preparation of carbonic acid which is required in the manufacture of gazeous drinks. Mr. F. Dick called attention to the antiseptic property of the fibrous residue of the Sugar Cane, known under the name of Bagasse. This property was accidentally discovered about a year ago by a physician of George Town who had to perform the “ post mortem ” examination of a man found buried under a heap of Bagasse. His body, instead of being in an advanced state of decomposition, was dried up to a mummy. The result was that the physician carried into practice his discovery. There happened to be at the time a great number of pa- tients suffering from ulcers in the hospital, and a contagious gangrene had declared itself ; the physician caused several tubs containing cane-trash to be placed in the wards, and the supply to be renewed at intervals. In a short time the atmosphere of the hospital Avas purified and the contagion ceased. The Editor of the Standard, number of r the 2nd April 1864, adds a few remarks which seem applicable to Mauritius, and we think the experiment deserving of a trial in our hospitals. “ Thus, it seems, ” says this paper, “ that Nature itself has provided an antidote for the pernicious effects of heat in tropical countries ; the contagious diseases caught by the heat of the sun, may be neutralized by the Sugar Cane, which is brought to maturity by those very rays.” The Secretary was favored by a letter from Mr. Daniel H anbury in London, calling his attention to the Columbo root ( Coccidus palmatus ) and recommending its cultivation in Mauritius as a medicinal plant of a great value. ff The Columbo root of commerce, Mr. H anbury says, is the product of a wild plant growing on the Mozambique Coast, whence it is shipped to Europe by way of Bombay. It is mostly more or less worm eaten and often has been badly dried, so that its bright greenish yellow colour is not well preserved. At the present time, (October 1864) it is remar- kably scarce and dear, and a supply of good quality would be really acceptable in the market.” The Secretary was enabled to procure but a very small quantity of the Columbo root at the Botanical Garden of Pamplemousses. He prepared it according to instructions, vizt : cut it in very thin slices and dried it in the shade It formed part of the collection of medicinal plants forwarded for the Dublin Exhibition. It would be interesting for more than one reason, to extend in this island the cultivation of the Columbo plant, the growth — 230 — of which is very rapid. It could become an article of com- merce in the hands of small proprietors. The following Resident Members were admitted during the year : — PORT LOUIS : 1. Mr. Charles Rustichelli, 2. — Constant Vankeirsbilk, 3. — E. C. Bewsher, 3. — Henry Magny, 4. Dr. Edwards, General Sanitary Inspector. Honorary Member : — Mr. P. Van Shendel, at Brussels. Several books, periodical papers, &c., have been received from the correspondents of the Society or from foreign So- cieties. The Cotton Association of Manchester has forwarded, through our Agent in London, live different varieties of Cot- ton seeds, which have been distributed amongst those of our members who have expressed a wish to cultivate them, name- ly : Mr. James Currie and Mr. Ch. Pitot. The Society has been informed of the death of Mr. Diard, one of its honorary members. He has long been known to the inhabitants of the Mascarenhas Islands. They will remem - qer his essential assistance in facilitating the introduction of certain species of sugar cane, the richness of which has in some measure compensated for the loss of the white cane. One of these canes bears the name of Mr. Diard. The life of that eminent man has been devoted to the progress of Natural Sciences. At first in conjunction with Mr. Duvaucel, they had both been sent out as collectors by the Museum of Paris. Mr. Diard subsequently entered the service of the King of Holland and the Netherlands, and was employed in Java as Superintendant of Agriculture. It was in that capacity that he was enabled to forward to Mauritius a -whole cargo of the Batavian canes, to replace the kind that had been destroy- ed by the malady in 1848 and 1849. They arrived here in 1850, in the Reliance, a ship that had been freighted by a certain number of Planters for the purpose. Such are, Your Excellency and Gentlemen, the results of our labours during the past year. We may have omitted to mention the name of a few members whose contribu- tions were of minor importance, and beg that they will accept our apology. There now remains the grateful task of thanking Your Excellency, not only for honoring this meeting with your presence, but above all, for unceasing marks of interest and the kindness which the Society has met with at your hands.” — 231 — IIis Excellency the Governor then rose for the purpose of moving the adoption of the Report which had just been read, and in so doing said he gladly availed himself of the • opportunity of thanking the Society for the valuable assistance it had afforded to the Government in several matters alluded to therein. The principal of these he need hardly say, had been the superintendance of the preparations for sending spe- cimens to the Dublin Exhibition, which he was happy to learn had been effected on a scale that would do j ustice to the industrial resources of this important Colony. The expe- diency of its being properly represented at all such great congresses of manufacturing skill, could not in his opinion be overrated, and he had readily applied to the Legislature for a grant on the occasion in question, at the instance of the Chamber of Agriculture. Of course Sugar in some shape or other must, as usual, form the great staple of their contribu- tion, but there were minor products referred to in the Report which might prove both useful and remunerative, among these he was glad to find that samples of Colombo root properly prepared had been forwarded ; not long since. Sir William Hooker had written to him to enquire whether this plant, the root of which is now attracting much attention in Europe, as a specific for Dysentery, flourished in this Island. Many of them were aware that this plant the “ Cocculus palmatus,” of Botanists was dioecious, and Mr. Horne had informed him that though both males and females blossom freely, seeds have not yet been produced at the Botanic Garden ; he be- lieved, however, that it could be easily propagated by other means and that its cultivation would ensure a valuable addi- tion to their exports. There was another medicinal plant which he hoped to see included among those exports at no distant date, though hitherto the attempt to introduce it had been attended as stated in tire report with disappointment, and that was the “Cinchona” or “Quinine Bark Tree.” The plants which he had procured had unfortunately arrived in a dead or dying state, and although they had been at once removed to the cooler climate of Reduit and attended to by Mr. Horne., they had never recovered the effects of the voy- age, or more probably of the previous land journey from the Botanical Gardens at Cotacamund through hotter regions of Madras. They ought not however to dispair of success from the failure of one attempt and he had written again to the Madras Government to repeat the experiment, and had only yesterday from his friend, Sir William Denison that another case wonld shortly be sent with all the precautions that have been suggested. There was another matter in which the Society also de- served his acknowledgements and that was for the very suc- cessful Flower Show held under their auspices in the Gardens of Government House. He trusted that its success was suffi- cient to ensure its repetition and he would take the oppor- tunity of reminding them that in that case it w'as not too soon to give public notice to intending exhibitors ; his honorable friend opposite (Mr. Henri Pitot) smiled ; but it was not every one who was ready to enter the lists, like him, at a moment’s notice. He Avould not delay them by referring to other points touched on in the Report ; the original papers contributed, though fevr in number, appeared to have been of a highly practical character and there was one of them con- taining the notes of Mr. Dick and Mr. Fleurot on the \V hite Ant of which he should be glad to get a copy, as enquiries had not long since been addressed to hint as to the best means of checking the ravages of that destructive insect. lie had seen in an English paper, that the impregnation of timber and other substances with Linseed Oil, was recommended for this purpose, but there might be many cases in which com- mon salt or the pulp of aloe leaves might be more suitable or easily procured. He must congratulate the Secretary on having so nearly completed the task of packing up and sending to Kewr the specimens in the Herbarium. They would be returned arran- ged and correctly named after comparaison with those in the collection there which is now the most extensive in the world, and the commencement would thus be made of an accurate catalogue of the contents of the Museum over the way. On the other hand, the examination of the original Types of Bory, Bojer and other eminent Botanists who had labored on these shores could not fail to prove instructive and inter- esting to European Botanists who congregated at Kew from all quarters — De Candolle him self having spent several months there last year. It would moreover enable his venerable friend Sir "William Hooker, to advise how far the materials amass- ed here, together with those he has already acquired at Kew, would justify the publication of a “Flora” of the Co- lony ; for that purpose he would not hesitate to ask the Legislature for the necessary vote of .€300 or £400 when the proper time arrived, and he trusted that the ground-work would be found to have been laid in the manuscripts of a late eminent member of that Society, just presented to Kew by his Widow. He remembered that the late Dr. Ayres in a letter to Dr. Mueller which he saw before leaving Melbourne, stated that he had then completed the desetiption of six hundred species not including the Ferns. It was worth their while to consider likewise whether the publication of a Fauna of Mauritius might not be much facilitated, and the Museum at the same time enriched, by exchanging duplicate speci- mens of Birds, Insects and Fishes with the British Museum and other kindred institutions in Europe. He believed it would be found that much less was known at home than was generally supposed of some of the commonest families in the Island, such as the Lacertse, Crustacea1, Mollusca Src. No doubt a good deal yet remained to be explored also in the Dependencies of Mauritius notwithstanding that, as men- tioned in the Report, advantage had been taken of the recent cruise of II. M. S. Rapid to send a collector from the Museum among them. In a brief visit of only a few hours’ duration to Rodrigues, one of their members, Mr. Edward Newton had not only disintered the fossil bones of what he considered — 234 — a Dodo {JDidus Solitarius) , but bad obtained t ivo species of birds new to Ornithologists ; whilst amongst the Ferns brought from the same Island by Captain Barclay, one had been reco- gnised by Lady Barkly as not previously known to exist either in Africa or India, or indeed anywhere else except Sin- gapore. Such discoveries might appear trival to the unobser- vant mind, but besides the interest they possessed for students of the particular branch of natural history to which they pertained, they furnished facts for those speculations — for he could hardly call them theories — as to the origin and distribu- tion of species, which were now exciting so much interest in the Scientific World, and the importance of which, in every point -of view, could not be disputed. He would detain them no longer, but call upon them to adopt the Report presented. Sir Gabriel F ropier rose and spoke as follows : — Messieurs, Permettez-moi dc remercier en votre nom Son Excellence le Gouverncur d’ avoir bien voulu venir presider votre seance annuel) e. Je me sens toujours tres honore d’ avoir a interpreter vos sentiments dans dcs occasions semblables, mais je suis peine de devoir aujourd’hui cet honneur a des causes regrettables. Je regrette que mon honorable ami et collogue de la Vice Presidence, prefere s’effacer par exces de modestie, quand sa parole, toujours ecoutee avec favour, le serait aussi avec fruit ; je regrette surtout que notre President, PHonorable Rush- worth, se sente encore trop affaibli, par sa recente maladie^ pour vous representer en cettc circonstance. J’espere du moins qubl pourra bientbt reprendre sa place parmi nous, coramc il a dejii repris ses occupations officiellcs. 11 est toujours facile cPexprimer des sentiments de recon- naissance, parce qu’ils sont bien sentis, ct pen de mots suflisent pour dire a Son Excellence que nous sommes touches de la nouvclle marque dbnteret qu’Ellc vent bien donner il notre Societe. Mais je n’oserais pas, sans preparation, me hasarder — 235 — aborder lcs questions que yient de trailer Son Excellence et qui font Fobjet du It ap port de noire infatigable et zele Secre- taire. Je nFexposerais surement h le faire d’une maniere peu digne du sujct et de vous-memes. Yous nFexcuserez done de nFabstenir. Si les encouragements aux arts et aux sciences sont desira- bles et utiles partout, on peut affirmer quails soUt indispensa- bles a Maurice ; et Son Excellence semble Favoir reconnu par les nombreuses preuves d’interet qu’Elle nous donne, et dont son discours de tout-il-Flieure abonde dbm bout a F autre. Ce iFest pas a dire que les habitants de cette colonie ne soient pas enclins an progres, ne soient pas animes du desir de F etude et de la science, ou soient prives de F aptitude et de Fintelligence necessaires pour s’y livrer avec succes. Dieu merci les mauriciens n’ont rien a regretter ou h envier sous ce rapport, et bien des exemples pourraient en faire foi. Mais il faut bien le reoonnaitre, si les progres accomplis dans le monde entier ont cree, pour Fliomme des sources nou- velles de jouissance et de bien etre, ils ont cree par cela memo mille besoins nouveaux et une soif ardente pour les richesses qui offrent seules les moyens de satisfaire ces besoius. Sous ce rapport on peut dire que dans les pays comme le notre, la lutte est peut-etre plus vive, plus incessante que partout ail- leurs. Et, ce qui pourrait etre paradoxal pour ceux qui voient dans les habitants de toutes les colonies des hommes mous et desoeuvres, on peut avancer qu’il n’y a pas de population plus affairee, plus occupee que la ndtre. Les resultats iFen sont ni plus prompts ni plus assures qiFailleurs sans doute ; nous avons a lutter contre des difficultes inconnues en d5autres con- trees ; et si la vie humaine parait trop courte en ces contrecs, pour atteindre le but propose, e’est bien autre chose ici ou le plus grand nombre voudrait accomplir en quelques annees, une tache si ardue pour regagner ses penates ou esperer un repos qui fuit toujours. Aussi ne trouve-t-on de temps pour rien ; et si j’en cxcepte Faccomplissement des devoirs d’un ordre superieur, cliacun sc croit clans l’impossibilite d’enlever un moment it ses aflaires. C’est done nn grand service que nous rend notre Gouver- neur, non seulement en nous encourageant par ses paroles, mais surtout en nous montrant par son exemple qu’on ne peut mieux reposer son esprit des occupations de la vie pu- blique qu’en l’appliquant aux charmes de l’etude. Et, cons- tatons en passant que cette heureuse alliance de l’etude et des aflaires id a pas ete perdue pour Sir Henry Barkly ; et que le temoignage que vient de lui donner la plus influente Societe Scientifique de notre Afetropole est d’autant plus considera- ble qu’il est venu le trouver aux confins du monde. ]Mais (l’ailleurs dans l’interet merae de la lutte que nous soutenons, ne devons-nous pas, comme nos concurrents cl’Eu- rope, demander a la science les moyens d’augmenter et d’a- meliorer nos produits, et de defendre nos recoltes et nos au- tres biens contre les causes de destruction qui les menacent ? — Ne devons-nous pas surtout demander aux Arts et aux Sciences les moyens de proteger notre sante, d’eclairer et d’elever notre esprit, d’augmenter le comfort et le bien-etre de notre existence? Et disons-le hardiment quelques ins- tants cliaque jour, chaque semaiue, cliaque mois meme, con- sacres ce but, nous seraient bientot amplement retribues. Voyez quel vaste champ s’offre it nous : cette annee les principaux travaux des membres de notre Societe ont porte sur des infiniment petits ; et ont produit cependant des resul- tats tres remarquables. AI. Eleurot, notre habile chimiste, sur les intelligentes sug- gestions de AL P. Dick, s’est attaque an caria blanc (Ther- mite Destructeur) cette vieille et tres dangereuse connaissance de nos maisons, de nos meubles, de nos arbres. L’irisecte lui-meme, sa demeure, son nid tout a ete decrit, alambique, analyse ; et bientot il en sortira sans doute des resultats utiles pour la conservation des bois, pour la therapeutique meme. Le Dr. Guthrie porte son attention sur les gouttes des liquidcs, sur les Indies des gaz ; et de cette etude patiente. — 237 complete, il salt tirer des indications propres a iuteresser l’esprit et fertiles en consequences pratiques. Le Dr. leery s' attache it decrire le pou a poche blanche, ce nouvel ennemi de notre industrie sucriere, le plus infime et peut etre le plus terrible, comme si le maitre de toutes choses voulait nous montrer le neant de notre orgueil humain en nous faisant trembler devant les plus chetifs des etres crees. Son etude aussi est complete : les transformations, les moeurs, les habitudes du terrible animal microscopique, tout est minu- tieusement decrit. Et qiPon Pappelle Puceron, Cochenille, Gallinsecte ou Gaster alphas (ainsique le propose le Dr. leery), il faut esperer que cette etude conduira it connaitre les meil- leurs moyens de s’en preserver. Yous le voyez done, rien iPest petit dans la nature. Par son importance, le Createur est toujours grand dans la plus chetive de ses oeuvres, et si je ne fais pas allusion it un autre travail du meme savant membre, plus important encore, si je passe sous silence les autres travaux de notre Societe, e’est pour vous laisser sous cette impression. A P oeuvre done vous tous ouvriers de Pavenir, vous surtout jeunes homines qui avez ete puiser les elements des sciences aux sources vives de Penseignement europeen. Faites profiter votre pays de vos connaissances acquises. Augmentez-enla somme par de nou- velles investigations. Considerez combien il reste it faire dans ces pays que n’ont pas encore explores les maitres de la science. IPhistoire naturelle tout entiere, la physiologie vegetale et animate, la chimie, la therapeutique, etc., etc., vous promettent d’abondantes moissons. Arenez en faire part it nos modestes reunions mensuelles. La timidite, la modestie peuvent-elles vous retenir ? Sans doute P esprit de critique peut s’exercer comme partout ailleurs, dans une petite communaute dont tous les membres se connaissent. Mais l’approbation des honnetes gens, des vrais amis du pays doit vous rassurer. Leur indulgence est acquise it tous ceux qui cherchent le bien, leurs applaudissements recompensent ceux qui y reussissent. Tout nous convie a reunir nos efforts pour rapporter dans — 238 — un an une plus grande somme de travaux au Chef bienveillant qui nous honore de son patronage. Nous ne saurions mieux lui prouver notre reconnaissance, qu’en imitant ses exemples. Et est-il seul a nous les donner ? Aupres de lui, une femme distinguee se livre avec succes a cette attrayante etude de la botanique qui offre a notre admiration les oeuvres les plus delicates de la nature. Yous venez de 1’ entendre, un hommage tout recent lui a ete rendu par la plus illustre autorite bota- nique de notre epoque : Sir William Hooker a donne le nom de Lady Barkly a une fougere (1) reconnuc par elle oomme non-decrite et recueillie dans la visite qui vient d’etre faite aux iles de notre Archipel. Montrons-nous done reconnais- sants par nos efforts comme par le remerciments (pie je repete en votre nom a, Sir Henry Barkly. The Society then proceeded to the election of its Council of Administration for the ensuing year and the following result was obtained : — OFFICIAL MEMBERS : The Hon. E. E. Hush worth, — President The Hon. Sir Gabriel Fropier, The Hon. Ch. W. Wiehe, j A. Desenne, Esq., — Treasurer. L. Bouton, Esq., — Secretary Fredk. M. Dick, Esq., Henry W. Finniss Vice-Presidents. I y c, Esq., - ) liss. Esq., ) Vi ce- Seer eta ries. INOFFICIAL MEMBERS : The Hon. H. Pitot, John Fraser, Esq., L. Ilugues, Esq., The Hon. E. Newton, Doctor Ch. Rcgnaud, „ II. Rogers. auditors : E. Fleurot, Esq. | V. Naz, Esq. (1) Cheilanthes Barklyi. /if ft A mr/iif J f-.-l. (’tek lifft • PRESENTED 1 2 DEC 1351) J A t I «