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THE
ELEMENTS OF AGRICULTURE
GEO. E. WARING, Jk.,
ATTTHOB OF "DRAINING FOE PROFIT AND DRAINING FOE HEALTH,'"
FORMERLY AGRICULTUEAL ENGINEER OF THE CENTRAL
PARK JN NEW YORK.
The effort to extend the dominion of man over nature is the most healthy and
most noble of all ambitions. — Bacon.
SECOND AliTD EEVISED EDITION.
NEW YORK:
THE TRIBUNE ASSOCIATION,
154 NASSAU STREET.
1868,
^^0
Entered according to Act of Congress, in the year 1868, by
GEO. E. WARING, Jr.,
In the Clerk's Office of the District Court of the LTnited States for tho
Southora District of New York.
The New York Printing Company,
8i, 83, a7id 85 Centre Street,
New York.
CONTENTS.
Section iTirst.
CHAPTER I.
PAGE
Introduction 11
CHAPTER II.
The Atmosphere and its Carbon 14
CHAPTER III.
Hydrogen and Oxygen 21
Nitrogen 22
Ammonia 23
CHAPTER IV.
Earthy Matter .27
Alkalies 28
Potash 28
Soda 29
Lime 29
Magnesia 30
Acids — Phosphoric Acid 30
Sulphuric Acid 31
Silicic Acid, or Silica 32
Neutrals — Chlorine 33
Oxide of Iron 33
CHAPTER V.
Growth 34
CHAPTER VI.
Starch, Woody- Fibre, Gluten, etc 39
Animals 42
CHAPTER VII.
Location of the Different Parts, and Variations in the Ashes
of Plants 46
CHAPTER Vin.
Recapitulation 49
IV CONTENTS.
Section Qcconb.
T" H TG SOIL.
CHAPTER I.
PAGE
Formation and Character of the Soil 57
Geology G4
CHAPTER II.
Uses of Atmospheric Matter 66
CHAPTER III.
Uses of Earthy Matter 72
Subsoil 74
Improvement 75
Section ®liir5,
31 ,A. IS^ TJ R, E S .
CHAPTER I.
Character and Varieties of Manures 81
CHAPTER II.
Animal Excrement 84
Digestion and its Products 85
CHAPTER III.
Waste of Manure 88
Evaporation 88
Leaching 93
CHAPTER rV.
Absorbents 95
Charcoal 95
Muck and its Treatment 97
Lime and Salt Mixture 99
Lime 100
Potash 101
CHAPTER V.
Composting Stable Manure 101
Shelter .102
The Floor 103
Tank 1 03
Liquid Manure 110
CHAPTER VI.
Different kinds of Animal Excrement 110
Stable Manure Ill
Recapitulation 112
CONTENTS.
PAGE
Mg-ht SoU 113
Hog Manure ... 115
Poultry-house Manure 116
Sheep Manure 118
Guano 118
CHAPTER YII.
Other Organic Manures 120
Dead animals 120
Bones 121
Fish 121
WooUen Rags, etc 122
Organic Manures of Vegetable Origin 'i2S
Spent Tan-bark 124
Sawdust and Soot 125
Green Crops 126
Absorption of Moisture 128
Distribution of Manures 129
CHAPTER yill.
Mineral Manures 130
CHAPTER IX.
Deficiencies of Soils, Means of Restoration, etc 135
Alkalies — Potash 136
Soda 138
Lime 140
Plaster of Paris 147
Chloride of Lime 147
Magnesia 148
Acids — Sulphuric Acid 148
Phosphoric Acid 150
Bones 153
Super-Phosphate of Lime 156
Silicic Acid 160
Neutrals — Chlorine 160
Oxide of Iron 161
Oxide of Manganese 161
Various other Earthy Manures — Leached Ashes 162
Old Mortar 162
Gas House Lime, etc 163
Soapers' Ley and Bleachers' Ley. ... ^ 164
Irrigation ' 164
Mixing Soils 167
CHAPTER X.
Atmospheric Fertilizers 169
Ammonia 170
Carbonic Acid 178
Oxygen 173
Water 174
VI CONTENTS.
CHAPTER XI.
PAOE
Recapitulation 174
Section iTonrtl).
IMLECHA^lSriC^Ij CTJLTI"VJ^TIO:iSr.
CHAPTER I.
The Mechanical Character of Soils 181
CHAPTER II.
Under-Draining 183
TUe Draining- 184
CHAPTER III.
Advantages of Under-Draining 187
CHAPTER IV.
SuV ioil Plowing 200
CHAPTER V.
Plowing and other Processes for Pulverizing the Soil 206
Plowing 206
The Harrow and Cultivator. 210
CHAPTER VI.
Rolling, Mulching, Weeding, etc 211
Rolling 211
Mulching 212
"Weeding 216
Cultivators 218
Improved Horse-Hoe 219
Section fiftl).
AI^^L YSIS.
Cfll^PTER I.
.Analysis A 225
CHAPTER II.
Tables of Analysis 228
The Practical Farmer '. 245
Explanation op Terms 253
The first edition of this book was written in 1853, when
the writer was full of the enthusiasm that comes with the
first years of study; when a very elementary knowledge
of the subjects of which it treats made the whole plan of
vegetation, cultivation, and manuring seem easy and simple.
In some instances, rather vague fancies were presented as
sound theories; and the perplexing uncertainties which
beset the path of the more thorough student were ignored —
because unknown.
The observation and experience of the intervening years
have sadly clouded some of these fancies, and the veil which
hangs about the true theories of agriculture has grown
harder to penetrate, — the difiiculties in the way of precise
knowledge have not lessened with closer acquaintance.
Notwithstanding its faults, the book received a very cor-
dial welcome at the hands of the public, — more because
such a book was much needed, than because of its real
value, and it ought, long ago, to Ijave been rewritten.
The present edition has been carefully revised, and it is
believed that its doctrines are such as the positive teachings
of chemistry, and the more enlightened practice of farming,
will justify ; still, it is ojQfered with more hesitation than was
its predecessor, and it is only offered at all because there
exists a sad deficiency in this department of our agricul-
tural literature.
The place that it is intended to fill is occupied by no
other work. It is not an agricultural chemistry, nor is it a
hand-book of the processes of every-day farming ; — only an
attempt to translate into common language, for the use of
every-day farmers, that which science has discovered and
has told in its own necessarily technical terms, and which
practical experience has proven to be of practical value.
The facts which it sets forth lie at the very ground- work
of the art of farming, and they are necessary to the business
education of every farmer. On the universal importance of
these facts the book must depend for its success ; and for
their sake, — not because of its own merit, — it is confidently
offered to the young farmers of America, as being worthy
of their most careful study.
Ogden Farm,
Newport, R. /., 1868.
SECTIOI FIRST.
THE PLANT.
SECTION FIRST.
THE PLANT.
CHAPTER I.
INTKODUCTION'.
The object of cultivating the soil is to raise from it
a crop oi plants. In order to cultivate with economy,
we must raise the largest possible quantity with the
least expense^ and without permanent injury to the
soil.
Before this can be done we must study the char-
acter of plants, and learn their exact composition.
They are not created by a mysterious power, they
are merely made up of matters already in existence.
They take up water containing food and other mat-
ters, and discharge from their roots, or their leaves,
or deposit within their pores, those substances that
are not required for their growth. It is necessary
for us to know what kind of matter is required as
food for the plant, and whence it is to be obtained ;
this we can learn only through such means as shall
separate the elements of which plants are composed ;
12 THE PLANT.
in other words, we must take them apart, and exam-
ine the different pieces of which they are made np.
If we burn any vegetable substance it disappears,
except a small quantity of earthy matter, which con-
stitutes the ashes. In this way we make the first
division between the two distinct classes of the con-
stituents of plants. One portion escapes into the
atmosphere, and the other remains as a disorganized
earthy substance.
That part which burns away during combustion
we will call atmospheric matter, because it was de-
rived by the plant from the air ; the ashes which re-
main we will call earthy matter, because they were
derived from the soil. The atmospheric matter has
become air, and it was originally obtained from air.
The earthy matter has become earth, and was ob-
tained from the soil.
This is the first step toward a knowledge of agri-
cultural chemistry. The next will be to examine
each of these two different classes of matter, that we
may learn precisely of what they consist. Then we
must inquire w4iere these substances are found, how
they are taken up by the plant, and how we can best
supply such as nature, unaided, does not always
furnish. This knowledge does not require that farm-
ers become chemists. All that is required is, that
they should know enough of chemistry to understand,
so far as the present state of knowledge makes it
possible, the nature of the materials of which their
crops are composed, and how those materials are to
be used to the best advantage.
THE PLANT-. 13
The elements of this knowledge may be easily ac-
quired, and should be possessed by every person, old
or young, whether actually engaged in the cultivation
of the soil or not. All are dependent on vegetable
productions, not only for food, but for every comfort
and convenience of life. It is the object of this book
to teach young farmers the first principles of agri-
culture : and while it does not contain all tlmt is
absolutely necessary to an understanding of the prac-
tical operations of cultivation, its teachings are such
as the writer found, in his early studies, to be most
necessary as a groundwork for future study and
thought and most useful in practice.
We will first examine the atmospheric part of
plants, or that which is driven away during combus-
tion or burning. This matter, though apparently lost,
is only changed in form.
It consists of one solid substance, carbon (or
charcoal), and three gases, oxygen^ hydrogen and ni-
trogen. These four kinds of matter constitute nearly
the whole of most plants, the ashes forming some-
times less than one part in one hundred of their dry
weight.
When wood is burned in a close vessel, or other-
wise protected from the air, its carbon becomes char-
coal. All plants contain this substance, it forming
usually about one-half of their dry weight. The re-
mainder of their atmospheric part consists of the
three gases named above. By the word gas, we mean
aeriform. Oxygen, hydrogen and nitrogen, when
pure, always exist in the form of air. Oxygen has
14 THE PLANT.
the power of uniting witli many substances, forming
compounds which are different from either of their
constituents alone. Thus : oxygen unites with iron
and forms oxide of iron or iron-rust^ which does not
resemble the grey metallic iron nor the gas oxygen ;
^^ oxygen unites with carbon and forms carbonic acid,
'HSif. which is an invisible gas, but not at all like pure oxy-
gen ; oxygen combines with hydrogen and forms
water. All water, ice, steam, etc., are composed of
these two gases. We know this because we can arti-
ficially decompose, or separate, all water, and obtain
as a result simply oxygen and hydrogen, or we can
combine these two gases and thus form pure water ;
oxygen combines with nitrogen and forms nitric
acid. These chemical changes and combinations
take place only under certain circumstances, which,
so far as they affect our subject, will be considered
in the following pages.
As the atmospheric elements of plants are ob-
tained from matters existing in the atmosphere which
surrounds our globe, we will examine its constitution.
CHAPTER II.
THE ATMOSPHERE AND ITS CAKBON.
Atmosphekic air is composed of oxygen and nitrogen.
Their proportions are, one part of oxygen to four
parts of nitrogen. Oxygen is the active agent in the
combustion, decay, and decomposition of organized
THE PLANT. 15
bodies (those which have possessed animal or vegetable
life, that is, organic matter), and others, — also, in
the breathing of animals. Experiments have proved
that if the atmosphere consisted of pure oxygen every
thing would be speedily destroyed, as the processes of
combustion and decay would be greatly quickened,
and animals would be so stimulated that they would
soon die. One use of the nitrogen in the air is to
dilute the oxygen, and thus reduce the intensity of
its effect.
Besides these two great elements, the atmosphere
contains certain impurities which are of great impor-
tance to vegetable growth ; these are, carbonic acid^
water ^ ammonia^ etc.
CAEBONIO ACID.
Carbonic acid is, in all probability, the only source
of the carbon of plants, and consequently supplies
more material to vegetation than any other single
sort of food. It is a gas, and is not, under natm^al
circumstances, perceptible to our senses. It consti-
tutes about 2-§Vo ^f ^^ atmosphere, and is found in
combination with many substances in nature. Marble,
limestone and chalk, are carbonate of lime, or car-
bonic acid and lime in combination ; and carbonate
of magnesia is a compound of carbonic acid and mag-
nesia. This gas exists in combination with many
other mineral substances, and it is contained in all
water not recently boiled. Its supply, though small,
is sufficient for the purposes of vegetation. It enters
16 THE PLANT.
the plant in two ways — through the roots in the
water which goes to form the sap, and at the leaves,
which absorb it from the air in the form of gas.
The leaf of the plant seems to have three offices :
absorbing carbonic acid from the atmosphere — as-
sisting in the chemical preparation of the sap — and
evaporating its water. If we examine leaves with a
microscope we shall find that some have as many as
170,000 openings, or mouths, in a square inch ; others
have a much less number. Probably the pores on
the under side of the leaf generally absorb the car-
bonic acid. This absorptive power is illustrated
"when we apply the lower side of a cabbage leaf to a
wound, as it draws strongly — the other side of the
leaf has not an equal effect. Young green shoots
and sprouts doubtless have the power of absorbing
and decomposing carbonic acid.
The roots of plants, by their absorbent surfaces, or
through the spongioles at the ends of their roots, ab-
sorb from the soil water, which contains carbonic
acid and other substances required for their nutrition.
How large a proportion of the carbonic acid is ab-
sorbed in this manner is not definitely known. It
probably depends on various circumstances, but is,
no doubt, always important.
Carbonic acid, it will be recollected, consists of
carbon and oxygen^ while it supplies only carbon to
the plant. It is therefore necessary that it be divided,
or decomposed, and that the carbon be retained while
the oxygen is sent off again into the atmosphere, to
perform again its office of uniting with carbon. This
THE PLANT. 17
decomposition takes place in the greenip^Yts of plants
and only under the influence of daylight. It is not
necessary that the sun shine directly on the leaf or
green shoot, but this causes a 7nore rapid decomposi-
tion of carbonic acid, and consequently we find that
plants which are well exposed to the sun's rays make
the most rapid growth.
The fact that light is essential to vegetation ex-
plains the conditions of different latitudes, which, so
far as the assimilation of carbon is concerned, are
much the same. At the Equator the days are but
about twelve hours long. Still, as the growth of
plants is extended over nearly or quite the whole
year, the duration of daylight is sufficient for the re-
quirements of a luxuriant vegetation. At the Poles,
on the contrary, the summer is but two or three
months long ; here, however, it is daylight all sum-
mer, and plants from continual growth develop them-
selves in that short time.
It will be recollected that carbonic acid constitutes
but about 2 s'o o ^^ ^^® ^^^) .7®^? although about one-
half of all the vegetable matter in the world is de-
rived from this source, as well as all of the carbon
required by the growth of plants, its proportion in
the atmosphere is constantly about the same. In
order that we may understand this, it becomes
necessary for us to ^consider the means by which it is
formed. In the act of burning, carbon unites with
oxygen, and always when bodies containing carbon
are burnt with the presence of atmospheric air, the
oxygen of that air unites with the carbon, and forms
18 THE PLANT.
carbonic acid. The same occurs when bodies con-
taining carbon decay^ as this is simply a slower
hurning and produces the same results. In the
breathing of animals the carbon of the blood com-
bines with the oxygen of the air drawn into the
lungs, and their breath, when thrown out, always
contains carbonic acid. From this we see that the
reproduction of this gas is the direct effect of the de-
struction of all organized bodies, whether by fire,
decay, or consumption by animals.
Furnaces are its wholesale manufactories. Every
cottage fire is continually producing a new supply,
and the blue smoke issuing from the cottage-chim-
ney, contains materials for making food for the cot-
tager's tables and new faggots for his fire. The
wick of every burning lamp draws up the carbon
of the oil to be made into carbonic acid in the
fiame. All matters in process of combustion, decay,
fermentation, or putrefaction, are returning to the
atmosphere those constituents, which they obtained
from it. Every living animal, even to the smallest
insect, by respiration, spends its life in the produc-
tion of this material, so necessary to the growth of
plants, and at death gives up its body in part for
such formation by decay.
Thus we see that there is a continual change from
the carbon of plants to air, and from air back to
plants, or through them to animals. As each dollar
in gold that is received into a country permanently
increases its amount of circulating medium, and each
dollar sent out permanently decreases it until re-
THE PLANT. 19
turned, so the carbonic acid sent into the atmosphere
by burning, decay, or respiration, becomes a per-
manent stock of constantly changeable material,
until it shall be locked up for a time, as in a house
which may last for centuries, or in an oak tree
which may stand for thousands of years. Still,
when these decay, the carbon which they contain
must be again resolved into carbonic acid.
The coal-beds of Pennsylvania are mines of car-
bon once abstracted from the atmosphere by plants.
In these coal-beds there are found various forms of
organized matter. These existed as living things
before the great floods, and it is the theory of some
geologists that at the breaking away of the barriers
of the immense lakes, of which our present lakes
were merely the deep holes in their beds, they were
washed away and deposited in masses so great as to
take fire from their chemical changes. It is by
many supposed that this fire acting throughout the
entire mass (^dthout the presence of air to supjply
oxygen except on the surface) caused it to become
melted carbon, and to flow around those bodies
which still retain their shapes, changing them to
coal without destroying their structures. This coal,
so long as it retains its present form, is lost to the
vegetable kingdom, and each ton that is burned, by
being changed into carbonic acid, adds to the ability
of the atmosphere to support vegetation.
Thus w^e see that, in the provisions of nature, car-
bon, the grand basis, on which all organized matter
is founded, is never permanent in any of its forms.
20 THE PLANT.
Oxygen is the carrier wliicli enables it to change its
condition. For instance, let lis snppose that we
have a certain quantity of charcoal ; this is nearly
pure carbon. We ignite it, and it unites with the
oxygen of the air, becomes carbonic acid, and floats
away into the atmosphere. The wind carries it
through a forest, and the leaves of the trees with
their millions of mouths drink it in. By the
assistance of light it is decomposed, the oxygen is
sent off to make more carbonic acid, and the carbon
is retained to form a part of the tree. So long as
that tree exists in the form of wood, the carbon will
remain unaltered, but when the wood decays, or is
burned, it immediately takes the form of carbonic
acid, and mingles with the atmosphere ready to be
again taken up by plants, and have its carbon de-
posited in the form of vegetable matter.
The blood of animals contains carbon derived
from their food. This unites witli the oxygen of the
air drawn into the lungs and forms carbonic acid.
Without this process, animals could not live. Thus,
while by the natural operation of breathing, they
make carbonic acid for the uses of the vegetable
world, plants, in taking up carbon, throw off oxygen to
keep up the life of animals. There is perhaps no way
in which we can better illustrate the chang^es of form
in carbon than by describing a simple experiment.
Take a glass tube filled with oxygen gas, and
put in it a lump of charcoal, cork the ends of the
tube tightly, and pass through the corks the wires
of an electrical battery. By passing a stream of
THE PLANT. 21
electrical fluid over the charcoal it may be ignited,
when it will burn with great brilliancy. In burning
it unites with the oxygen forming carbonic acid, and
disappears. It is no more lost, however, than is the
carbon of wood which is burned in a stove ; al-
though invisible, it is still in the tube, and may be
detected by careful weighing. A more satisfactory
proof of its presence may be obtained by decompos-
ing the carbonic acid by drawing the wires a short
distance apart, and giving a sjpark of electricity.
This immediately separates the oxygen from the car-
bon, which forms a dense black smoke in the tube.
By pushing the corks together we may obtain a
,wafer of charcoal of the same weight as the piece
introduced. In this experiment we have changed
carbon from its solid form to an invisible gas and
back again to a solid, thus fully representing the
continual changes of this substance in the destruc-
tion of organic matter and the growth of plants.
CHAPTEE III.
HTDEOGEN, OXYGEN AND NITEOGEN.
HYDROGEN AND OXYGEN.
Let us now consider the three gases, hydrogen^ oxygen^
and nitrogen^ which constitute the remainder of the
atmospheric part of plants.
22 THE PLANT.
Water is composed of liydrogeii and oxygen, and, if
analyzed, yields simply these two gases. Plants per-
form STicli analysis, and in tliis way are able to obtain
a sufficient supply of these materials, as their sap is
composed chiefly of ^vater. Whenever vegetable
matter is destroyed by burning, decay, or otherwise,
its liydrogen and oxygen unite and form water, which
usually escapes in the form of an invisible vapor.
The atmosphere of course contains greater or less
quantities of watery vapor arising from this cause
and from the evaporation of liquid water. This
vapor condenses, forming rains, etc.
Hydrogen and oxygen are never taken into con-
sideration in manuring lands, as they are so readily
obtained from the w^ater constituting the sap of the
plant, and consequently they need not occupy our
attention in this book.
NITROGEN.
Nitrogen^ the only remaining atmosjpheric constitu-
ent of vegetable matter, is for many reasons worthy
of close attention.
1. It is necessary to the growth and perfection of
all cultivated plants.
2. It is necessary to the formation of all animal
'6. It - ^-tten deficient in the soil.
4. 1l is liable to be easily lost from manures.
Athough about four-fifths of atmospheric air are
pure nitrogen, it is almost certain that plants get no
THE PLANT. 23
nutriment directly from this source. It is all obtained
from some of its compounds, chiefly from the one
called ammonia. Nitric acid is also a source from
which plants may obtain nitrogen, though, to the
farmer, it is of less importance than ammonia.
AMMONIA.
Ammonia is composed of nitrogen and hydrogen.
It has a pungent smell and is famiharly known as
hartshorn. The same odor is often perceptible
around stables and other places where animal matter
is decomposing. All animal muscle, certain parts of
plants and other organized substances, consist of
compounds containing nitrogen. When these com-
pounds undergo combustion, or are in any ixianner
decomposed, the nitrogen which they contain unites
with hydrogen, and forms ammonia. In conse-
quence of this the atmosphere always contains more
or less of this gas, arising from the decay and com-
bustion which are continually going, on all over the
world.
This ammonia in the atmosphere and that which is
contained in the soil (derived from the decomposition
of organic matters within it) is the capital stock to
which all plants, not artificially manured, must look
for their supply of nitrogen. As the} -^'k^^'^rK <=--
monia chiefly if not entirely through thei'l " ':s, we
must discover some means by which it may be con-
veyed from the atmosphere to the soil.
Water may be made to absorb many times its
24 THE PLANT.
bulk of this gas, and water with which it comes in
contact will immediately take it up. Spirits of
hartshorn is merely water through which ammonia
has been passed until it is saturated.* This power
of water has a direct application to agriculture,
because the water constituting rains, dews, etc.,
absorbs the ammonia which the decomposition of
nitrogenous matter had sent into the atmosphere,
and we find that all rain, snow, and dew, contain
ammonia. This fact may be chemically proved in
various ways, and is perceptible in the common
operations of nature. Every person must have
noticed that when a summer's shower falls on the
plants in a flower garden, they commence their
growth with fresh vigor, while the blossoms become
larger and more richly colored. This effect cannot
be produced by watering with spring water, unless
it be previously mixed with ammonia, in which case
the result will be the same.
Although ammonia is a gas and pervades the
atmosphere, few, if any, plants can take it up,- as
they do carbonic acid, through their leaves. It
must all enter through the roots in solution in the
water which goes to form the sap. Although the
amount received from the atmosphere is of great
importance, there are few cases where artificial ap-
plications are not beneficial. The value of farm-yard
and other animal manures, depends largely on the
ammonia which they yield on decomposition. This
* By saturated^ we mean tliat it contains all that it is capable
of holding.
THE PLANT. 25
subject, also the means for retaining in the soil the
ammoniacal parts of fertilizing matters, will be fully
considered in the section on manures.
After ammonia has entered the plant it ma^^ be
decomposed, its hydrogen separated from it, and its
nitrogen retained to answer the purposes of growth ,
The changes which nitrogen undergoes, from plants
to animals, or, by decomposition, to the form of am-
monia in the atmosphere, are as varied as those of
carbon and the constituents of water. The same
little atom of nitrogen may one year form a part of a
plant, and the next become a constituent of an animal,
or, with the decomposed dead animal, may form a
part of the soil. If the animal should fall into the
sea it may become food for fishes, and our atom of
nitrogen may form a part of a fish. That fish may
be eaten by a larger one, or at death may become
food for the whale, through the marine insect on
which it feeds. After the abstraction of the oil from
the whale, the nitrogen may, by the putrefaction of
his remains, be united to hydrogen, form ammonia,
and escape into the atmosphere. From here it may
be brought to the soil by rains, and enter into the
composition of a plant, from which, could its parts
speak as it grows in our garden, it could tell us a
wonderful tale of travels, and assure us that, after
wandering about in all sorts of places, it had returned
to us, the same little atom of nitrogen which we had
owned twenty years before, and which for thousands
of years had been continually going through its
changes.
2
26 THE PLANT.
Liebig says : " All the nitrogen of plants and of
animals is derived from the air. Every fireplace
where coals are burned, the numerous furnaces and
chimneys of the manufacturing towns and districts,
of locomotive engines and steamboats, all the smelt-
ing furnaces of the iron-works — all these are so many
forms of distillatory apparatus which enrich the at-
mosphere with the nitrogenized food of a vegetable
world, belonging to a period long past.
" We. can form some idea of the quantities of am-
monia thus poured into the atmosphere, if we con-
sider that in numerous gas-works many tons of am-
moniacal salts are annually obtained from the coals
distilled for gas." ^
The same is true of any of the atmospheric or
earthy constituents of plants. They are performing
their natural offices, or are lying in the earth, or
floating in the atmosphere, ready to be lent to any
of their legitimate uses, sm-e again to be returned to
their starting point.
Thus no atom of matter is ever lost. It may
change its place, but it remains for ever as a part of
the capital of nature.
* Journal of the Royal Agricultural Society, vol. xvii., p. 289.
THE PLAIfT. 27
CHAPTER lY.
EAETHY MATTER.
We will now examine the ashes left after burning
vegetable substances. This is earthy matter; and it
is obtained from the soil. Atmospheric matter, al-
though forming so large a part of the plant, we
have seen to consist of four different substances.
The earthy portion, on the contrary, although
forming so small a part, consists of no less than nitw
or ten different kinds of matter. These we will
consider in order. In their relations to agriculture
they may be divided into three classes — alkalies^
acids ^ and neutrals ^^
Alkalies and acids are of opposite properties, and
when brought together they unite and neutralize
each other, forming compounds which are neither
alkaline nor acid in their character. Thus, carbonic
acid (a gas) unites with lime — a burning, caustic
substance — and forms marble, which is a hard, taste-
less stone. Alkalies and acids are characterized by
their tendency to unite with each other, and the com-
pounds thus formed have many and various proper-
ties, so that the characters of the constituents give
no indication of the character of the compound.
For instance, lime causes the gases of animal manure
* This classification is not strictly scientific, but it is one which
the learner will find it well to adopt. These bodies are called
neutrals because they have a less decided alkaline or acid charac-
ter than the other.
THE PLANT.
to escape, while sulphate of lime (a compound of
sulphmTc acid and lime) produces an opposite effect,
and prevents their escape.
The substances coming under the signification of
neutrals, are less affected bj the laws of combina-
tion, still they do combine with other substances, and
some of the resultant compounds are of great impor-
tance to apiculture.
ALKALIES.
The alkalies which are found in the ashes of
plants are four in number ; they are jpotash^ soda,
lime, and magnesia.
POTASH.
When we pour water over wood ashes it dissolves
the potash which they contain, and carries it away
in solution. This solution is called ley, and if it
be boiled to dryness it leaves a solid substance
which is chiefly pure potash. Potash left exposed
to the air absorbs carbonic acid and becomes car-
bonate of potash or pearlash / if another atom of car-
bonic acid be added, it becomes super-carbonate of
potash, or saloeratus. Potash has many uses in agri-
culture.
1. It forms a constituent . / early all plants.
2. It unites with silicic ac* -hd tbrms a compound
which water can dissolve ai < carry into the roots of
plants ; thus supplying them with an ingredient
which gives them much of their strength.
THE PLANT. 29
3. It is a strong agent in the decomposition of vege-
table matter, and is thus of much importance in pre-
paring manm-es.
4. It roughens the smooth round particles of sandy
soils, and prevents their compacting, as they are
often liable to do.
5. It is also of use in killing certain kinds of insects,
and, when externally applied, in smoothing the bark
of fruit trees.
The source from which this and the other earthy
matters required are to be obtained, will be more
fully considered in the section on manures.
SODA.
Soda^ one of the alkalies contained in the ashes
of plants, is very much the same as potash in its agri-
cultural character and uses. Soda exists very largely
in nature, as it forms an important part of common
salt, whether in the ocean or in those inland deposits
known as rock salt. When combined with sulphuric
acid it forms sulphate of soda or Glauber's salts.
In combination with carbonic acid, as carbonate of
soda, it forms the common washing soda of the shops.
LIME.
Lime is in many ' ^s important in agriculture :
1. It is a constitut^^^ li plants and animals.
2. It assists in th. decomposition of vegetable
matter in the soil as \\ o as of its minerals.
3. It corrects the acidity* of sour soils,
* Sourness.
30 THE PLANT.
4. Combined with chlorine or sulphuric acid as
chloride or sulphate of lime it is a good fixer of
fertilizing gases.
In nature it exists most largely in the form of car-
bonate of lime ; that is, as marble, limestone, and
chalk — these all being of the same composition. In
manufacturing oaustic (or quick) lime, the carbonate
of lime is burned in a kiln ; by this means the car-
bonic acid is driven off into the atmosphere and the
lime remains in a pure or caustic state.
MAGNESIA.
Magnesia is the remaining alkali of vegetable
ashes. It is well known .as a medicine, both in the
form of calcined magnesia, and, when mixed with
sulphuric acid, as epsom salts.
Although magnesia is a necessary constituent of
plants, it is not an element of which fertile soils are
likely to become exhausted, and it does not receive
attention in special manuring ; the amount returned
to the soil in farm-yard manure, and that supplied
by the decay of roots, being sufficient for the growth
of the most luxuriant crops.
ACID s.
PHOSPHOKiq ACID.
Phosphoric acid is a constituent of the ashes of
plants which is of the greatest value to the farmer ;
it is composed of phosphorus and oxygen. Being an
THE PLANT. 3 J.
acid, this sabstance has the power of combining witli
any of the alkalies. Its most important compound
is formed with lime.
PJiosj)hate of lime forms about 65 per cent, of the
dry weight of the bones of all animals, and it is all
derived from the soil through the medium of plants.
As plants are intended as food for animals, nature
has provided that they shall not 'attain their perfec-
tion without taking up a supply of phosphate of
lime as well as of their other earthy ingredients ;
consequently, there are many soils which will not
produce good crops, simply because they are deficient
in phosphate of lime. It is one of the most impor-
tant ingredients of manures, and its value is depen-
dent on certain conditions which will be hereafter
explained.
Another use of phosphoric acid in the plant is to
supply it with the small amount of phosj)horus,
which seems to be required in the formation of the
seed.
SULPHURIC Acm.
Sulphuri& acid is important to vegetation, and~its
addition to the soil often renders it more fertile. It
is composed of sulphur and oxygen, and is made for
manufacturing purposes, by burning sulphur. With
lime it forms sulphate of lirne^ which is gypsum or
"plaster." In this form it is often found in na-
ture, and is most extensively used in agriculture.
The methods for supplying sulphuric acid will be
described hereafter. It gives to the plant a small
32 THE PLANT.
portion of sulphur^ which is necessary to the forma-
tion of some of its parts.
SILICIC ACID, OR SILICA.
This is common sand. In its pure state it cannot
be dissolved and plants can make no use of it. It
unites with the alkalies and forms compounds, such
as silicate of potash^ silicate of soda^ etc.^ which are
soluble in water, and tlierefore available to plants.
If we roughen a corn stalk with sand-paper we may
sharpen a knife upon it. This is owing to the hard
particles of silica which its outer parts contain.
.Window glass is silicate of potash, rendered insoluble
by additions of arsenic and litharge.
Liebig tells us that there was discovered, between
Manheim and Heidelberg in Germany, a mass of
melted glass where a hay-stack had been struck by
Hghtning. They supposed it to be a meteor, but
chemical analysis showed that it was only the com-
pound of silicic acid and potash which served to
strengthen the grass.
There is always enough silicic acid in the soil, but
it is often necessary to add an alkali to render it
soluble and available. When grain, etc., lodge or
fall down from their own weight, it is probable that
they are unable to obtain from the soil a sufficient
supply of the soluble silicates to support their rapid
growth.
THE PLANT. 33
NEUTRALS .
CHLOEINE.
Chlorine is an important ingredient of vegetable
ashes. It is not found alone in nature, but is always
in combination with other substances. Its most im-
portant compound is with sodium, forming chloride
of sodium (or common salt). Sodium is the base
of soda, and common salt is usually the cheapest
source from which to obtain both soda and chlorine.
Chlorine unites with lime in the formation of chloride
of lime^ which is much nsed to absorb or destroy the
unpleasant odors of decaying matters, and in this
character it is of use in the treatment of manures.
OXID EOF IKON.
Oxide of iron, one of the constituents of ashes, is
common iron rust. Iron itself is naturally of a
greyish color, but when exposed to the atmosphere,
it readily absorbs oxygen and forms a reddish com-
pound. It is in this form that it usually exists in
the soil, and many soils as well as the red sandstones
are colored by it. It is seldom, if ever, necessary to
apply this as a manure, there being usually enough
of it in the soil.
This red oxide of iron, of which we have been
speaking, is called by chemists the peroxide. There
is another compound which contains less oxygen than
this, and is called the protoxide of iron, which is
2*
34
THE PLANT.
poisonous to plants. When it exists in the soil it is
necessary to use such means of cultivation as shall
expose it to the atmosphere and allow it to take up
more oxygen and become the peroxide. The black
scales which ily from hot iron when struck by the
blacksmith's hammer are protoxide of iron.
The peroxide of iron is a very good absorbent of
ammonia, and consequently, as will be hereafter
described, adds to the fertility of the soil.
Oxide of Manganese, though often found in small
quantities in the ashes of cultivated plants, cannot
be considered indispensable.
Having now examined the materials from which
the ashes of plants are formed, we are enabled to
classify them in a simple manner, so that they may
be recollected. They ai'e as follows : —
ALKALIES.
Potash.
Soda.
Lime.
Magnesia.
ACIDS.
Sulphuric acid.
Phosphoric "
Silicic "
NEUTRALS.
Chlorine.
Oxide of Iron.
" Manganese.
CHAPTEK Y.
GROWTH
Having examined the materials of which plants are
made, it becomes necessary to discover how they ai'e
THE PLANT. 35
*
put togetlier in the process of growth. Let us there-
fore suppose a young wheat-plant, for instance, to be
in condition to commence independent growth.
It consists of roots which are located in the soil ;
leaves wdiich are spread in the air, and a stem which
connects the roots and leaves. This stem contains
sap vessels, which may be regarded, for the sake of
simplicity, as tubes extending from the ends of the
roots to the surfaces of the leaves, thus affording a
passage for the sap, and consequently allowing the
matters taken up to be distributed throughout the
plant.
It is necessary that the materials of which plants
are made should be supplied in certain proportions,
at the proper time, and in a suitable condition. For
instance, carbon could not be taken up in large
quantities by the leaves, unless the roots, at the same
time, were receiving from the soil those mineral mat-
ters w^hich are necessary to growth. On the other
hand, no considerable amount of earthy matter could
be appropriated by the roots unless the leaves were
obtaining carbon from the air. This same rule holds
true with regard to all of the constituents required ;
Nature seeming to have made it a law that if one
of the important ingredients of the plant is absent,
the others, though they may be present in sufficient
quantities, cannot be used. Thus, if the soil is de-
ficient in alkalies, and still has sufficient quantities
of all of the other ingredients, the plant cannot take
up these ingredients, because alkalies are necessary
to its life.
36 THE I'LANT.
If a farmer wishes to make a cart lie prepares his
wood and iron, gets them all in the proper condition,
and then can very readily put them together. But
if he has all of the wood necessary and no iron^ he
cannot make his cart, because bolts, nails and screws
are required, and their place cannot be .supplied by
boards. This serves to illustrate the fact that in,
raising plants we must give them everything that
they require, or they wdll not grow at all.
In the case of our young plant the following opera-
tions are going on at about the same time.
The leaves are absorbing carbonic acid from the
atmosphere, and the roots are drinking in water from
the soil.
The manner in which food is taken up by roots,
may be illustrated by the following experiment:
Take a tumbler, filled entirely full with water ; tie
over it a bladder, and on the bladder sprinkle a little
salt. The bladder becomes moist throughout its
entire thickness, and transmits enough moisture to
the salt to dissolve it gradually, and as fast as it is
dissolved, it passes through the bladder into the
water inside of the tumbler. In a long enough time
the water can be made, in this way, to dissolve as
much salt as though it had been stirred into it with-
out the intervention of the bladder. If we keep the
salt soaking wet, as it lies on the outside of the blad-
der, it will pass through much more rapidly, but if
we do not wet it by a direct application of water,
enough water will reach it through the mem])rane to
allow it to pass into the tumbler, as above described.
THE PLANT. 37
The roots of plants contain sap, which is separated
from the plant-food in the soil, by a thin film of
matter, which constitutes its cell-walls. So long as
the water of the sap has the capacity to dissolve
more mineral matter than it already contains, it will
take it through the cell-walls, as the salt is taken
through the bladder. If the plant-food outside of
the roots is in a moist condition, it will be taken up
more rapidly than if too dry. The moistm-e of the
soil itself, containing mineral matter in solution,
passes through the cell- walls to supply the place of
that which has been evaporated at the leaves, the
matters in solution passing through with the w^ater
itself.
In short, there is a constant tendency to supply
the deficiency of water in the root, and to keep it
constantly charged with as much as it can dissolve
of the plant-food, from which it is separated only by
its membranous cell-walls.
Under the influence of daylight, the carbonic acid
is decomposed ; its oxygen returned to the atmos-
phere, and its carbon retained in the plant.
The water taken in by the roots circulates through
the sap vessels of the plant, and is drawn up towards
the leaves, where it is evaporated. This water con-
tains the nitrogen and earthy food required by the
plant and some carbonic acid, while the water itself
consists of hydrogen and oxygen.
Thus we see that the plant obtains its food in the
following manner : —
38 THE PLANT.
Carbon. — In the form of carhoniG acid from the
atmosphere, and from that contained
in the sap, the oxygen being retm^ned
to the air.
o ) From the elements of the water con-
Htdeogen. j stitnting the sap.
NiTKOGEN. — From the soil (chiefly in form of am-
monia). It is carried into the plant
* through the roots in solution in water.
Earthy | From the soil, and only in solution in
Matter, j water.
Many of the chemical changes which take place
in the interior of the plant are well, and some but
imperfectly understood, but they require too much
knowledge of chemistry to be easily comprehended
b}^ the young learner, and it is not absolutely essen-
tial that they should be understood by the scholar
who is merely learning the elements of the science.
It is sufficient to say that the food taken up by
the plant undergoes such changes as are required for
its growth ; as in animals, where the food taken into
the stomach is digested, and is afterward formed
into bone, muscle, fat, hair, etc., so in the plant the
nutritive portions of the sap are resolved into wood,
bark, grain, or other necessary parts.
The results of these changes are of the greatest
importance in agriculture, and no person ought to
be called a thoroughly practical farmer who does
not understand them.
TRE PLANT. 39
CHAPTEE YI.
STARCH, WOODY-FIBKE, GLUTEN, ETC.
"We have liitlierto examined the raw material of
plants. That is, we have looked at each one of the
elements separately, and considered its nse in vege-
table growth.
We will now consider another division of plants.
We know that they consist of various substances, such
as wood, gum, starch, oil, etc., and on examination
we shall discover that these substances are composed
of the various atmospheric and earthy ingredients de-
scribed in the preceding chapters. Thej are made
up almost entirely of atmospheric matter, but their
ashy parts, though very small, are (as we shall pres-
ently see) of great importance.
These compounds may be divided into two classes.
The first class are composed of carhon^ hydrogen^
and oxygen.
The second class contain the same substances and
nitrogen.
The first class (those compounds not containing ni-
trogen) comprise the wood, starch, gum, sugar, and
fatty matter, which constitute the greater part of all
plants, also the acids which are found in sour fruits,
etc. Yarious as are all of these things in their char-
acters, they are entirely composed of the same ingre-
dients (carbon, hydrogen, and oxygen), and usually
combined in about the same proportion. There may
40 THE PLANT.
be a slight difference in the composition of their ashes,
but the organic part derived from the atmosphere is
much the same in every case, so much so, that they can
often be artificially changed from one to the other.
As an instance of this, it may be stated that at the
Fair of the American Institute, in 1834, Prof. Mapes
exhibited samples of excellent sugar made from the
juice of the corn-stalk, from starch, from linen, and
from woody fibre.
In the plant, during its growth, they are constantly
changing. At one time they assume a form in which
they cannot be dissolved by water, and remain fixed
in their places.
At another, the chemical influences on which growth
depends, change them to a soluble form, and they are
carried, by the circulation of the sap, to other parts
of the organism, where they may be again deposited
in other insoluble forms. For example, the turnip
devotes the first season of its growth to storing up
in its root a large amount of starch and pectic acid ;
in the second season, these substances become soluble,
are taken up by the circulation and again deposited
in the form of woody fibre, starch, etc., in the stems,
leaves, seed-vessels, etc., above the ground. If a
turnip root be planted in the spring, in moist cotton,
from which it can get no food, it will simply, by the
transformation of its own substance, form stems,
leaves, flowers and seed.
Those products of vegetation which contain nitro-
gen, are of the greatest importance to the farmer,
being the ones from which animal muscle is made.
THE PLAiCT. 41
The J consist, as will be recollected, of carbon, liy-,
drogen, oxygen and nitrogen^ or of all of the atmos-
j)heriG elements of plants. They are all of much the
same character, though each kind of plant has its
peculiar form of this substance, which is known under
the general name oi protein.
The protein of wheat is called gluten — that of In-
dian corn is zein — that of beans and peas is legumin.
In other plants the protein substances are vegetable
aTbumen^ casein^ etc.
Gluten absorbs large quantities of water, which
causes it to swell to a great size, and become full of
holes. Flour which contains much gluten, makes
light, porous bread, and is preferred by bakers, be-
cause it absorbs so large an amount of water.
The nitrogenous substances are necessary to animal
and vegetable life, and none of our cultivated plants
will attain maturity, (complete their growth,) unless
allowed the materials required for forming them. To
furnish this condition is the chief object of nitrogen
given to plants as manure. If no nitrogen could be
obtained these substances could not be formed, and
the plant must cease to grow.
When, on the contrary, ammonia is given to the
soil, (by rains or otherwise,) it furnishes nitrogen,
while the carbonic acid and water yield the other
constituents of protein, and a healthy growth con-
tinues, jprovided that the soil contains the earthy
matters required in the formation of the ash, in a
condition to be taken up by the roots. •
The wisdom of this provision is evident when we
42 THE PLANT.
recollect that the nitrogenous substances are neces-
sary to the formation of muscle in animals, for if
plants were allowed to complete their growth with-
out a supply of nitrogen, our grain and hay might
not be sufficiently well supplied with it to keep our
oxen and horses in working condition, while under
the existing law, plants must be of nearly a uniform
quality, (in this respect,) and if a field is short of
nitrogen, its crop will not be large, and of a very
poor quality, but the soil will produce good plants
as long as the nitrogen lasts, and then the growth
must cease. ^
ANIMALS.
That this principle may be clearly understood, it
may be well to explain more fully tlie application of
the different constituents of plants in feeding animals.
Animals are composed (like plants) of atmospheric
and earthy matter, and every thing necessary to build
.them up exists in plants. It is one of the offices of
the vegetable world to prepare the gases in the
atmosphere and the minerals in the earth for the
uses of animal life, and, to effect this, plants put
these gases and minerals together in the form of the
various compound substances which we have just
described.
In animals the compounds containing no nitrogen
comprise the fatty substances, parts of the blood,
etc., while the protein compounds, or those which
* It is of course assumed that the soil is fertile in other re-
spects.
THE PLAKT. 43
do contain nitrogen, form the muscle, a^part of the"
bones, the hair, and other portions of the body.
Animals contain a larger proportion of earthy
matter than plants do. Bones contain a large quan-
tity of phosphate of lime, and we find other earthy
compounds performing important ofiices in the sys-
tem.
In order that animals may be perfectly developed,
they must, of course, receive as food all of the mate-
rials required to form their bodies. They cannot
live if fed entirely on one ingredient. Thus, if
starch alone be eaten by the animal, he might be-
come/b^, but his strength would soon fail, because
his food contains nothing to keep up the vigor of his
muscles. If on the contrary the food of an animal
consisted entirely of gluten, he might be very strong
from a superior development of muscle, but would
not become fat. Hence we see, that in order to
keep up the proper proportion of both fat and mus-
cle in our animals, (or in ourselves,) the food must
be such as contains a proper proportion of both
classes of vegetable products.
It is for this reason that grain, wheat for instance,
is so good for food. It contains both classes of
proximates, and furnishes material for the formation
of both fat and muscle. The value of j^6>i^/' depends
very much on the manner in which it is manufac-
tured. This will be explained hereafter.
Apart from the relations between the organic
parts of plants, and those of animals, there exists an
important relation between their ashes or their earthy
4^ THE PLANT.
parts ; and food, in order to satisfy the demands of
animal life, must contain the mineral matter re-
quired for the purposes of that life. Take bones for
instance. If phosphate of lime is not always sup-
plied in sufficient quantities in the food, animals are
prevented from forming healthy bones. This is par-
ticularly to be noticed in teeth. Where food is
deficient of phosphate of lime, we see poor teeth as
a result. Some physicians have supposed that one
of the causes of consumption is the deficiency of
phosphate of lime in food.
The first class of vegetable constituents (starch,
sugar, gum, etc.) perform an important office in the
animal economy aside from their use in making fat.
They constitute they^^^^ which supplies the animal's
fire, and gives him his Keat. The lungs are the
delicate stoves, which supply the whole body with
heat. But let us explain this matter more fully. If
wood, starch, gum, or sugar, be bm^ned in a stove,
they produce heat. These substances consist, as
will be recollected, of carbon, hydrogen, and oxygen,
and when they are destroyed in any way, (provided
they be exposed to the atmosphere,) the hydrogen
and oxygen unite and form water, and the carbon
unites with the oxygen of the air and forms carbonic
acid, as was explained in a preceding chapter. This
process is always accompanied by the production of
Jieat^ and the intensity of this heat depends on the
time occupied in its production. In slow decay, the
chemical changes take place so slowly that the heat,
being conducted away as soon as formed, is not per-
THE PLANT. 45
ceptible to our senses. In combustion (or burning)
the same changes take place with much greater
rapidity, and the same amount of heat, being con-
centrated, or brought out in a far shorter time, it
becomes intense, and therefore apparent. In the
lungs and blood-vessels of animals the same law
holds true. The blood contains matters belonging
to this carbonaceous class, and they undergo, dm^ing
its circulation, the changes which have been de-
scribed under the head of combustion and decay.
Their hydrogen and oxygen unite, and form the
moisture of the breath, while their carbon is com-
bined with the oxygen of the air drawn into the
lungs, and is thrown out as carbonic acid. The
same consequence — heat — results in this, as in the
other cases, and this heat is produced with sufficient
rapidity for the necessities of the animal. When he
exercises violently, his blood circulates with in-
creased rapidity, thus carrying carbon more rapidly
to the lungs. The breath also becomes quicker,
thus supplying increased quantities of oxygen. In
this way the decomposition becomes more rapid,
and the animal is heated in proportion.
Thus we see that food has another function be-
sides that of forming animal matter, namely to sup-
ply heat. When the food does not contain a suffi-
cient quantity of starch, sugar, etc., to answer the
demands of the system, the cmimaVs own fat is car-
ried to the lungs, and there used in the production
of heat. This important fact will be referred to
again.
46
THE PLANT.
CHAPTER YII.
LOCATION OF THE DIFFERENT PARTS, AND VARIATIONS
IN THE ASHES OF PLANTS.
Let us now examine plants with a view to learn-
ing the location of the various parts.
The stem or trunk of the plant or tree consists
very largely of woody fibre / this also forms a large
portion of the other parts except the seeds, and, in
some instances, the roots. The roots of the potato
contain large quantities of starch. Other roots, such
as the carrot and turnip^ contain pectic acid^"^ a
nutritious substance resembling starch.
It is in the seed^ however, that the more nutritive
portions of most plants exist, and here they maintain
certain relative positions which it is well to under-
stand, and which can be best explained by reference
to the following figures, as described by Prof. John-
ston : —
FIG, 1.
" Thus a shows the position of the oil in the outer
* This pectic acid gelatinizes food in" the stomach, and thus
renders it more digestible.
" THE PLANT. 47
part of the seed — it exists in minute drops, inclosed
in six-sided cells, which consist chiefly of gluten ; 5,
the position and comparative quantity of the starch,
which in the heart of the seed is mixed with only a
small proportion of gluten ; c, the germ or chit, which
contains much gluten.""^
The location of the earthy parts of plants is of
much interest, and shows the adaptation of each
part to its particular use. Take a wheat plant, for
instance — the stalk, the leaf, and the grain, show in
their ashes, important difference of composition.
The stalk or straw contains three or four times as
large a proportion of ash as the grain, and a no less
remarkable difference of composition may be noticed
in the ashes of the two parts. In that of the straw,
we find a large proportion of silicic acid and scarcely
any phosphoric acid, while in that of the grain there
is scarcely a trace of silicic acid, although phosphoric
acid constitutes about one half of the entire weight.
The leaves contain a considerable quantity of lime.
This may at first seem an unimportant matter,
but on examination we shall see the use of it. The
straw is intended to support the grain and leaves,
and to convey the sap from the roots to the upper
portions of the plant. To perform these offices,
strength is required, and this is given by the siliciG
acid, and the woody fibre which forms so large a
proportion of the stalk. The silicic acid is combined
with an alkali, and constitutes the glassy coating of
the straw. While the plant is young, this coating is
* See Johnston's Elements, page 41.
48 THE PLANT.
hardly apparent, but as it grows older, as the grain
becomes heavier, (verging towards ripeness,) the
silicious coating of the stalk assumes a more prom-
inent character, and gives to the straw sufficient
strength to support the golden head. The straw is
not the most important part of the plant as/btx^, and
it contains but little phosphoric acid, which is so
necessary to animals.
The grain, on the contrary, is especially intended
as food, and therefore must contain a large propor-
tion of phosphoric acid — this being, as we have al-
ready learned, necessary to the formation of bone —
while, as it has little necessity for strength, and as
silicic acid is not needed by animals, this ingredient
exists in the grain only in a very small proportion.
It may be well to observe that the phosphoric acid
of grain exists most largely in the hard portions near
the shell, or bran. This is one of the reasons why
Graham (or unbolted) flour is more wholesome than
fine flour. It contains all of the nutritive materials
which render the grain valuable as food, while flour
which is very finely bolted* contains only a small
part of the outer portions of the grain (where the
phosphoric acid, protein and fatty matters exist most
largely). The starchy matter in the interior of the
grain, which is the least capable of giving strength
to the animal, is carefully separated, and used as food
for man, while the better portions, not being ground
so finely, are rejected. This one thing alone may be
sufficient to account for the fact, that the lives of
* Sifted through a fine cloth called a bolting cloth.
THE PLANT. 49
men have become shorter and less blessed with
health and strength, than they were in the good old
days when a stone mortar and a coarse sieve made
a respectable flour mill.
Another important fact concerning the ashes of
plants is the difierence of their composition in different
plants. Thus, the most prominent ingredient in the
ash of the potato \^ potash ; of wheat and other grains,
phosphoric acid / of meadow hay, silicic acidj of clo-
ver, liw.e'y of beans, potash^ etc. In grain, potash
(or soda)^ etc., are among the important ingredients.
These differences are of great importance to the
practical farmer, as by understanding what kind of
plants uses the most of one ingredient, and what kind
requires another in large proportion, he can regulate
his crops so as to prevent his soil from being exhaust-
ed more in one ingredient than in the others, and
can also manure his land with reference to the crop
which he intends to grow. The tables of analyses
in the fifth section will point out these differences
approximately. The composition of ashes varies a
little, but not enough to affect the value of the
tables for the uses of the farmer.
CHAPTER YIII.
REOAPITULATIOH-.
We have now learned as much about the plant as is
required for our immediate uses, and we will care-
3
50 THE PLA^T.
fully reconsider the various points with a view to fix-
ing them permanently in the mind.
Plants are composed of atmospheric and earthy
matter.
Atmospheric matter is that which burns away in
the fire. Earthy matter is the ash left after burning.
The organic matter of plants consists of three
gases, oxygen, hydrogen and nitrogen, and one solid
substance, carbon (or charcoal). The mineral parts
consist of potash, soda, lime, magnesia, sulphi^'ic
acid, phosphoric acid, silicic acid, chlorine, oxide of
iron, and oxide of manganese.
Plants obtain their atmospheric food as follows : —
Oxygen and hydrogen from water ; nitrogen from
some compound containing nitrogen (chiefly from
ammonia) ; and carbon from the atmosphere, where
it exists as carbonic acid — a gas.
They obtain their earthy food from the soil.
The water which supplies oxygen and hydrogen
to plants is readily obtained without the assistance
of manures.
Ammonia is obtained from the atmosphere, by be-
ing absorbed by rain and carried into the soil, and it
enters plants through their roots. It may be artifi-
cially supplied in the form of animal manure with
advantage.
Carbonic acid is absorbed from the atmosphere by
leaves, and decomposed in the green parts of plants
under the influence of daylight; the carbon is re-
tained, and the oxygen is returned to the atmos-
phere.
THE PLANT. 61
When plants are destroyed by decay, or burning,
their organic constituents pass away as water, am-
monia, carbonic acid, etc., ready again to be taken
np by other plants.
The earthy matters in the soil can enter the plant
only with the aid of w^ater. Potash^ soda, lime,
and magnesia, are soluble in their pure forms.
Magnesia is injurious when present in too large
quantities.
SulphuriG acid is often used as a manure, and is
usually most available in the form of sulphate
of lime or plaster. It is also valuable in its pure
form to prevent the escape of ammonia from com-
posts.
PhosjyJioric acid is highly important, from its fre-
quent deficiency in worn-out soils. It is most readily
taken up by plants under certain conditions which
will be described in the section on manures.
SilioiG acid is common sand, and must be united
to an alkali before it can be used by the plant, be-
cause it is insoluble except when so united.
Chlorine is a constituent of common salt (chloride
of sodium), and from this source may be obtained in
sufficient quantities for manm-ial purposes.
Oxide of iron is iron rust. There are two oxides
of iron, \hQ peroxide (red) and \h.Q protoxide (black).
The former is advantageous in the soil, and the latter
poisons plants.
Oxide of manganese is often absent from the ashes
of our cultivated plants.
The food of plants, both organic and earthy, must
52 THE PLANT.
be present at the time when it is required and in
sufficient quantity. In the plant, this food under-
goes such chemical changes as are necessary to growth.
The compound substances contained in plants are
of two classes, those not containing nitrogen^ and
those which do contain it.
The first class constitute nearly the whole plant.
The second class, although small in quantity, are
of the greatest importance to the farmer, as from
them all animal muscle is made.
Animals, like plants, are composed of both at-
mospheric and earthy matter, and their bodies are
obtained directly or indirectly from plants.
The first class of compounds in animals comprise
the fat, and like tissues.
The second class form the muscle, hair, gelatine
of the bones, etc.
In order that they may be perfectly developed,
animals must eat nitrogenized and non-nitrogenized
food, and in the proportions required by their
natures.
They require phosphate, of lime and other mineral
food which exists in plants.
Aside from their use in the formation of fat^ sub-
stances of the first class are employed in the lungs
and blood-vessels as fuel to keep up animal heat,
which is produced (as in fire and decay) by their
decomposition.
When the food is insufficient for the purposes of
heat, the animal's own fat is decomposed, and carried
to the lungs as fuel.
THE PLANT. 53
The stems, roots, branches, etc., of most plants
consist principally of woody jihre. '
Their seeds, and sometimes their roots, contain
considerable quantities of starch.
The nitrogenized substances and the oils of most
plants exist most largely in the seeds, therefore seeds
are the most nutritions food for animals, because
they contain the largest proportion of digestible
matter.
The location of the different compounds in the
plant, as well as of its mineral parts, shows a remark-
able reference to the purposes of growth, and to the
wants of the animal world, as is noticed in the
difference between the construction of the straw and
that of the kernel of wheat.
The reason why the fine flour now made is not
so healthfully nutritious as that which contained
more of the coarse portions, is that it is robbed of a
large proportion of protein and phosphate of lime,
while it contains an undue amount of starch, which
is available only to form fat, and to supply fuel to
the lungs.
Different plants have ashes of different composi-
tion. Thus — one may take from the soil large
quantities of potash, another of phosphoric acid, and
another of lime. By understanding these difler-
ences, we shall be able so to regulate our rotations
that the soil may not be called on to supply more of
one ingredient than of another, and thus it may be
kept in balance.
The facts contained in this chapter are the alpha-
5-1: THE PLANT.
het of agriculture^ and the learner should become
perfectly familiar with them, before proceeding
further.
To enter more fully and more scientifically upon
the consideration of the various properties of these
substances, and of their relations to each other,
would, no doubt, be in better accordance with the
demands of accurate knowledge ; but the foregoing
is believed to be a perfectly true, although a very
simple statement of the first principles of the growth
and composition of plants, and is sufficient for the
first steps in agricultural study.
A clear comprehension of what is herein set forth
should have the effect of stimulating a further search,
in which more extended treatises will become neces-
sary.
SECTION SECOID.
THE SOIL
SECTION SECOND.
THE SOIL.
•-«-•
CHAPTEE I.
FOEMATION AND CHARACTER OF THE
SOIL.
In the foregoing section, we have studied the cha-
racter of plants and the laws which govern their
growth. We learned that one necessary condition
for growth is a fertile soil, and we must examine the
nature of different soils, in order that we may under-
stand the relations between them and plants.
The soil is not to be regarded as a mysterious mass
of dirt, whereon crops are produced by a mysterious
process. Well ascertained scientific knowledge has
proved beyond question that all soils, whether in
America or Asia, whether in Maine or California,
have certain fixed properties, which render them
fertile or barren, and their fertility or barrenness de-
pends, first of all, on the presence or absence of those
minerals which constitute the ashes of vegetable pro-
ductions.
3*
58 THE SOIL.
The soil is a great chemical compound, and its
chemical character is ascertained (as in the case of
plants) by analyzing it, or taking it apart.
We first learn that fertile soils contain both at-
mospheric and earthy matter ; but, unlike the plant,
they usually possess much more of the latter than of
the former.
In the plant, the atmospheric matter constitutes
the most considerable portion of the whole. In the
soil, on the contrary, it usually exists in very small
quantities, while the earthy parts constitute nearly
the whole bulk.
The atmospheric or organic part of soils consists of
the same materials that constitute the atmospheric
part of the plants, and is in reality decayed vegetable
and animal matter. It is not necessary that this
organic part of the soil should form any particular
proportion of the whole, and indeed we find it vary-
ing from one and a half to fifty, and sometimes, in
peaty soils, to over seventy per cent. All fertile soils
contain some organic matter, although it seems to
make but little difiference in fertility, whether it be
five or fifty per cent.
The earthy part of soils is derived from the
crumbling of rocks. Some rocks (such as the slates
in Central 'New York) decompose, and crumble rap-
idly on being exposed to the weather ; while granite,
marble, and other rocks, will last for a long time
without perceptible change. The causes of this
crumbling are various, and are important to be un-
derstood by the agriculturist, as by the same process-
THE SOIL. 59
es bj wMcli the soil was originally formed, lie can
increase its depth, or otherwise improve it. This
being the case, we will in a few words explain some
of the principal pulverizing agents.
1. The action of frost. "When water lodges in
the crevices of rocks, and freezes^ it expands, and
bursts the rock, on the same principle that causes
it to break a pitcher in winter. This power is verj
great, and by its assistance large cannon may be
burst. Of course, the action of frost is the same on
a small scale as when applied to large masses of mat-
ter, and, therefore, we find that when water freezes
in the jpores * of rocks or stones, it separates their
particles and causes them to crumble. The same rule
holds true with regard to stiff clay soils. If they are
ridged in autumn, and left with a rough surface ex-
posed to the frosts of winter, they will become much
lighter and finer, and can afterwards be worked with
less difiiculty.
2. The action of water. Many kinds of rock
become so soft on being soaked with water, that they
readily crumble.
3. The chemical changes of the constituents of the
rock. Many kinds of rock are affected by exposure
to the atmosphere, in such a manner, that changes
take place in their chemical character, and cause
them to fall to pieces. The red kellis of J^ew Jer-
sey, (a species of sandstone,) is, when first quarried,
a very hard stone, but on exposure to the influ-
* The spaces between the particles.
60 THE SOIL.
ences of the atmosphere, it becomes so soft that it
may be easily crushed between the thumb and finger.
Other actions, of a less simple kind, exert an in-
fluence on the stubbornness of rocks, and cause them
to be resolved into soils. "^ Of course, the composi-
tion of the soil must be similar to that of the rock
from which it was formed ; and consequently, if we
know the chemical character of the rock, we can tell
Avhether the soil formed from it can be brought under
profitable cultivation. Thus felspar, on being pul-
verized, yields potash ; talcose slate yields magnesia ;
marls yield lime, etc.
The soil formed entirely from rock, contains, of
course, no organic matter. Still, it is capable of
bearing plants of a certain class, and when these die,
they are deposited in the soil, and thus form its or-
ganic portions, rendering it capable of supporting
those plants which furnish food for animals. Thou-
sands of years must have been occupied in prepa-
ring the earth for habitation by man.
As the earthy part of the soil is usually the lar-
gest, we will consider it first.
As we have stated that this portion is formed
from rocks, we will examine their character, with a
view to showing the different qualities of soils.
As a general rale, it may be stated that all rocks
* In very many instances the crevices and seams of rocks are
permeated by roots, wMch, by decaying^ and thus inducing the
growth of other roots, cause these crevices to become filled with
organic matter. This, by the absorption of moisture, may expand
with sufficient power to burst the rock.
THE SOIL. 61
are either sandstones, limestones, or clays / or a mix-
ture of two or inore of these ingredients. Hence we
find that all mineral soils are either sandy, calcareoics
(limej), or clayey / or consist of a mixture of these,
in which one or another usually predominates. Thus,
we speak of a sandy soil, a clay soil, etc. These
distinctions (sandy, clayey, loamy, etc.) are impor-
tant in considering the mechanical character of the
soil, but have little reference to its chemical condi-
tions of fertility.
By mechanical character, we mean those qualities
which affect the ease of cultivation — excess or defi-
ciency of water, ability to withstand drought, etc.
For instance, a heavy clay soil is difiicult to plow,
retains water after rains, and bakes (j^uite hard dur-
ing drought ; while a light sandy soil is plowed with
ease, often allows water to pass through immediately
after rains, and becomes dry and powdery during
drought. Notwithstanding those differences in their
mechanical character, both soils may be very fertile,
or one more so than the other, without reference to
the clay and sand which they contain, and which, to
our observation, form their leading characteristics.
The same facts exist with regard to a loam, a calca-
reous (or limey) soil, or, a vegetable mould. Their
mechanical texture is not necessarily an index to
their fertility, nor to the manures required to enable
them to furnish food to plants. It is true, that each
kind of soil appears to have some general quality of
fertility or barrenness which is well known to prac-
tical men, yet this is not founded on the fact that
02 THE SOIL.
the clay or the sand, or the vegetable matter, enter
more largely into the constitution of plants than they
do when they are not present in so great quantities,
but on certain other facts which will be hereafter
explained.
As the following names are used to denote the
character of soils, in ordinary agricultural descrip-
tion, we will briefly explain their application :
A Sandy soil is, of course, one in which sand
largely predominates.
Clay soil, one where day forms a large proportion
of the soil.
Loamy soil, where sand and clay are more equally
mixed.
Marl contains from five to twenty per cent, of
carbonate of lime.
Calcareous soil more than twenty per cent.
Peaty soils, of course, contain large quantities of
organic matter.*
We will now take under consideration that part
of the soil on which depends its ability to supply
food to the plant. This portion rarely constitutes
more than five or ten per cent, of the entire soil,
often much less — and it has no reference to the sand,
clay, and vegetable matteus which they contain.
From analyses of many fertile soils, and of others
which are barren or of poorer quality, it has been
ascertained that the presence of certain ingre-
dients is necessary to fertility. This may be bet-
* These distinctions are not essential to be learned, but are
often convenient.
THE SOIL.
ter explained by the assistance of tlae following
table :
In one hundred pounds.
Soil fertile
without
manure.
Good
wheat soil.
Barren.
Organic matter
Silicic acid (sand) . . .
Alumina (clay)
Lime
Magnesia
Oxide of iron
Oxide of manganese . . .
Potash
Soda
Chlorine
Sulphuric acid
Phosphoric acid ....
Carbonic acid
Loss during the analysis
9.7
64.8
5.7
5.9
.9
6.1
.1
.3
.4
.2
.2
.4
4.0
1.4
7.0
74.3
5.5
1.4
.7
4.7
1.7
.7
.1
.1
•U
3.6i
4.0
77.8
9.1
8!l
A
100.0
100.0
100.0
The soil represented in the first and second columns
might still be fertile with less organic matter, or with
a larger proportion of clay (alumina), and less sand
(silicic acid). These affect its TneGhanical character ;
but, if we look down the columns, we notice that there
are small quantities of lime, magnesia and the other
constituents of the ashes of plants (except oxide of
manganese). It is not necessary that they should be
present in the soil in the exact quantity named above,
but not one must he entirely absent^ or greatly reduced
in ^proportion. By referring to the third column, we
see that these ingredients are not all present, and the
soil is barren. Even if it were supplied with all but
one or two, potash and soda for instance, it could not
support a crop without the assistance of manures con-
64: THE SOIL.
taining these alkalies. The reason for this must be
readily seen, as we have learned that no plant can arrive
at maturity without the necessary supply of materials
required in the formation of the ash, and these mate-
rials can be obtained only from the soil ; consequent-
ly, when they do not exist there, it must be barren.
The earthy part of soils has two distinct offices to
perform. The claj^ and sand form a mass of material
into which roots can penetrate, and which support
plants in their position. These parts also absorb
heat, air and moisture, to serve the purposes of growth,
as we shall see in a future chapter. The minute
portions of soil, which comprise the acids, alkalies
and neutrals, furnish plants with their ashes, and are
the most necessary to the fertility of the soil.
GEOLOGY.
The relation between the earthy parts of soils and
the rocks from which it was formed, is the foundation
of Agricultural Geology. Geology may be briefly
named the science of the rochs. It would not be ap-
propriate in an elementary work, to introduce much
of this study, and we will therefore simply state that
the same kind of rock is of the same composition all
the world over ; consequently, if we find a soil
in New England formed from any particular rock,
and a soil from the same rock in Asia, their natural
fertility will be the same in both localities. All rocks
consist of a mixture of different kinds of minerals ;
and some, consisting chiefly of one ingredient, are of
THE SOIL. 65
different degrees of Jiardness. Both of these qualities
must affect the character of the soil, but it may be
laid down as a rule that, when the rocks of two loca-
tions are exactly alike, the soils formed from them
will he of the same natural fertility, and in propor-
tion as the chemical character of rocks changes, in
the same proportion will the soils differ in fertility.
In most districts the soil is formed from the rock
on which it lies ; but this is not always the case.
Soils are often formed by deposits of matter brought
by water from other localities. Thus the alluvial
banks of rivers consist of matters brought froln the
country through which the rivers have passed. The
river Xile, in Egypt, yearly overflows its banks, and
deposits large quantities of mud brought from the un-
inhabited upper countries. The prairies of the West
owe their soil chiefly to deposits by water. Swamps
often receive the washings of adjacent hills ; and, in
these cases, their soil is derived from a foreign source.
We might continue to enumerate instances of the
relations between soils and the sources whence they
originated, thus demonstrating more fully the impor-
tance of geology to the farmer ; but it would be be-
yond the scope of this work, and should be investi-
gated by scholars more advanced than those who are
studying merely the elements of agricultural science.
The mind, in its early application to any branch
of study, should not be charged with intricate subjects.
It should master well the rudiments, before investi-
gating those matters which ^ouldi follow such under-
standing.
(IG THE SOIL.
By pursuing the proper course, it is easy to learn
all that is necessary to form a good foundation for a
thorough acquaintance with the subject. If this
foundation is laid thoroughly, the learner will regard
plants and soils as old acquaintances, with whose
formation and properties he is as familiar as with the
construction of a building or a simple machine. A
simple spear of grass will become an object of inter-
est, forming itself into a perfect plant, with full de-
velopment of roots, stems, leaves, and seeds, by pro-
cesses with which he feels acquainted. The soil will
cease to be mere dirt ; it will be viewed as a com-
pound substance, whose composition is a matter of
interest, and whose care may become a source of in-
tellectual pleasure. The commencement of study
in any science must necessarily be wearisome to the
untrained mind, but its more advanced stages amply
repay the trouble of early exertions.
CHAPTEE 11.
USES OF ATMOSPHERIC MATTER.
It will be recollected that, in addition to its mineral
portions, the soil contains atmospheric or organic mat-
ter in varied quantities. It may be fertile with but
one and a half per cent, of atmospheric matter, and
some peaty soils contain more than fifty per cent, or
more than one-half of the whole.
THE SOIL. 07
The precise amount necessary cannot be fixed at
any particular proportion ; probably five parts in a
hundred is better than a smaller amount.
The soil obtains its atmospheric matter in two
ways. First, by the decay of roots and dead plants,
also of leaves, which have been brought to it by
wind, etc. Second, by the application of animal or
vegetable manures.
When a crop of clover is raised, it obtains its car-
bon from the atmosphere; and, if it be plowed
under, and allowed to decay, a portion of this carbon
is deposited in the soil. Carbon constitutes nearly
the whole of the dry weight of the clover, aside from
the constituents of water ; and when we calculate
the immense quantity of hay and roots grown on
an acre of soil in a single season, we shall find that
the amount of carbon thus deposited is immense.
If the clover be removed, and the roots only left to
decay, the amount of carbon deposited would still be
very great. The same is true in all cases where the
crop is removed, and the roots remain to add to the
organic or vegetable part of the soil. While under-
going decomposition, a pi . tion of this matter escapes
in the form of gas, and the remainder chiefly assumes
the form of carbon (or charcoal), in which form, it
will always remain, without loss, unless driven out by
fire. If a bushel of charcoal be mixed with the soil
now, it will be the same bushel of charcoal, neither
more nor less, a thousand years hence, unless some
influence is brought to bear on it aside from the
growth of plants. It is true that, in the case of the
68 ' THE SOIL.
decomposition of organic matter in the soil, certain
compounds are formed, known under the general
names of humus and humic acid, which may, in a
slight degree, affect the growth of plants, but their
practical importance is of too doubtful a character
to justify us in considering them. The application
of manures, containing organic matter, such as peat,
muck, animal manure, etc., supplies the soil with
carbon on the same principle, and the decomposing
matters also generate "^ carbonic acid gas while being
decomposed. The agricultural value of carbon in
the soil depends (as we have stated), not on the fact
that it enters into the composition of plants, but on
certain other important offices which it performs, as
follows : —
1. It makes the soil more retentive of manures.
2. It causes it to appropriate larger quantities of
the fertilizing gases of the atmosphere.
3. It gives it greater power to absorb moisture.
4. It renders it warmer.
1. Carbon (or charcoal) makes the soil retentive
of manures, because it has in itself a strong power
to absorb, and retain fertilizing matters. There is
a simple experiment by which this "power can be
shown.
Ex. — Take two barrels of pure beach sand, and
mix with the sand in one barrel a few handfuls of
charcoal dust, leaving that in the other pure. Pour
a pailful of the brown liquor of the barn-yard
through the pure sand, and it will pass out at the
* Produce.
THE SOIL. 69
bottom unaltered. Pour the same liquor through
the barrel containing the charcoal, and only pure
water will pass through. The reason for this is that
the charcoal retains all of the impurities of the
liquor, and allows only the water to pass through.
Charcoal is often employed to purify water for
drinking, or for manufacturing purposes.
A rich garden-soil contains large quantities of
carbonaceous matter ; and if we bury in such a soil
a piece of tainted meat or a fishy duck, it will, in a
short time, be deprived of its odor, which will be
entirely absorbed by the charcoal and clay in the
soil.
« Carbon absorbs gases, as well as the impurities of
water ; and, if a little charcoal be sprinkled over
manm*e, or any other substance, emitting offensive
odors, the gases escaping will be taken up by the
charcoal, and the odor will be very much modified.
It has also the power of absorbing earthy matters,
which are contained in water. If a quantity of salt
water be filtered through charcoal, the salt will be
retained, and the water will pass through pure.
We are now able to see how carbon renders the
soil retentive of manures.
1st. Manures, which resemble the brown liquor
of barn-yards, have their fertilizing matters taken
out, and retained by it.
2d. The gases arising from the decomposition
{rotting) of manure are absorbed by it.
3d. The soluble earthy portions of manure, which
might in some soils leach down with water, are
70 .THE SOIL.
arrested and retained at a point at which they can be
taken up by the roots of plants.
2. Carbon in the soil causes it to appropriate
larger quantities of the fertilising gases of the atmos-
phere, on account of its power, as just named, to ab-
sorb gases.
The atmosphere contains gases, which have been
produced by the breathing of animals, by the decom-
position of various kinds of organic matter, which
are exposed to atmospheric influences, and by the
burning of wood, coal, etc. These gases are chiefly
ammonia and carbonic acid, both of which are largely
absorbed by water, and consequently are contained
in rain, snow, and dew, which, as they enter the soil,
give up these gases to the carbon, and they there
remain until required by plants. Even the air itself,
in circulating through the soil, gives up fertilizing
gases to the carbon, which it may cbntain.
3. Carbon gives to the soil power to absorb
moisture, because it is itself one of the best absorb-
ents in nature ; and it has been proved by accurate
experiment that peaty soils absorb moisture with
greater rapidity, and part with it more slowly than
any others.
4. Carbon in the soil renders it warmer, because
it darkens its color. Black surfaces absorb more heat
than light ones, and a black coat, when worn in the
sun, is warmer than one of a lighter color. By mix-
ing carbon with the soil, we darken its color, and
render it capable of absorbing a greater amount of
heat from the sun's rays.
THE SOIL. 71
It will be recollected that, when vegetable matter
decomposes in the soil, it produces certain gases (car-
bonic acid, etc.), which either escape into the atmos-
phere, or are retained in the soil for the use of plants.
The production of these gases is always accompanied
by Jieat^ which, though scarcely perceptible to our
senses, is perfectly so to the growing plant, and is of
much practical importance. This will be examined
more fully in speaking of manures.
Another important part of the organic matter in
the soil is that which contains nitrogen. This forms
but a very small portion of the soil, but it is of
very great importance to vegetation. As nitrogen
in food is of absolute necessity to the growth of
animals, so nitrogen in the soil is indispensable to the
growth of cultivated plants. It is obtained by the
soil in the form of ammonia (or nitric acid) from the
atmosphere, or by the application of animal or vege-
table matter. In some cases, manures called nitrates'^
are used; and, in this manner, nitrogen is given to
the soil.
We have now learned that the atmospheric mat-
ter in the soil performs the following offices : —
Organic matter thoroughly decomposed is chiefly
carbon^ and has the various effects ascribed to this
substance on p. 68.
Organic matter in process of decay produces car-
* Mtrates are compounds of nitric acid (whicli consists of ni-
trogen and oxygen) , and alkaline substances. Thus nitrate of
potash (saltpetre), is composed of nitric acid and potash ; nitrate
of soda (cubical nitre or cubic-petre), of nitric acid and soda.
72 THE SOIL.
bonic acid and ammonia in the soil ; its decay also
causes heat.
Organic matters containing nitrogen^ such as ani-
mal substances, etc., furnish ammonia, and other ni-
trogenous substances to the roots of plants.
CHAPTER III.
USES OF EAKTHT MATTER.
The offices performed by the earthy constituents of
the soil are many and important.
These, as well as the different conditions in which
the bodies exist, are necessary to be carefully consid-
ered.
Those parts which constitute the larger proportion
of the soil, namely the clay, sand, and limy portions,
are useful for purposes which have been named in the
first part of this section, w^iile the clay has an addi-
tional efiect in the absorption of ammonia.
For this purpose, it is quite as effectual as charcoal ;
the gases escaping from manures, as well as those ex-
isting in the atmosphere, and in rain-water, being
arrested by clay as well as by charcoal.
The more minute ingredients of the soil — those
which enter into the construction of plants — exist in
conditions which are more or less favorable or in-
jurious to vegetable growth. The principal condi-
THE SOIL. 73
tion necessary to fertility is cwpadty to he dissolved^
it being (so far as we have been able to ascertain) a
fixed rule, as was stated in the first section, that no
mineral substance can enter into the roots of a plant
except it he dissolved in water.
The alkalies potash, soda, lime, and magnesia, are-
in nearly all of their combinations in the soil suffi-
ciently soluble for the purposes of growth.
The acids are, as will be recollected, sulphuric,
silicic, and phosphoric. These exist in the soil in
combination with the alkalies, as sulphates, silicates,
and phosphates, which are more or less soluble under
natural circumstances. Phosphoric acid in combi-
nation with lime as phosphate of lime is but slightly
soluble ; but, when it exists or has existed in the com-
pound known as 5'6^j?6^phosphate of lime, it is much
more soluble, and consequently enters into the com-
position of plants with much greater facility. This
matter will be more fully explained in the section on
manures. Silicic acid exists in the soil usually in the
form of sand^ in which it is, as is well known, per-
fectly insoluble ; and, before it can be used by plants,
which often require it in large quantities, it must be
made soluble, by combination with an alkali.
For instance, if there is a deficiency of soluble
silicic acid in the soil, the application of an alkali,
such as potash, which will unite with the sand, and
form the silicate of potash, will give it the ability to
be dissolved and carried into the roots of plants.
Chlorine in the soil is probably always in an
available condition.
4
74 THE SOIL.
Oxide of iron exists, as has been previously stated,
usually in the form of the peroxide (or red oxide).
Sometimes, however, it is found in the form of the
j>rotoxide (or black oxide), which is soluble and is
poisonous to plants, and renders the soil unfertile.
By loosening the soil in such a manner as to admit
the air, and by removing stagnant water by draining,
this compound takes up more oxygen, which renders
it a peroxide, and makes it insoluble except in the
slight degree required for plants. The oxide of
manganese is probably of little consequence.
The usefulness of all of these matters in the soil
depends largely on their exposure to the action of
roots and of the circulating water in the soil ; if
they are in the interior of particles, they cannot be
made use of; while, if the particles are so pulverized
that their constituents are exposed on their sin-faces,
they become available, because water can immediate-
ly attack to dissolve them and roots can absorb them.
This is one of the great offices of plowing, harrow-
ing, cultivating, and hoeing ; the lumps of soil being
thereby more broken up and exposed to the action
of atmospheric influences, which are often necessary
to produce a fertile condition of soil.
SUBSOIL.
The subsoil is usually of a different character from
the surface soil, but this difference is more often the
result of cultivation and the effect of vegetation than
of ,a different original formation. The surface soil,
THE SOIL. 75
from having been long cultivated, has been more
opened to the influences of the air than is the case
with the subsoil, which has never been disturbed so
as to allow the same action. Again the growth of
plants has supplied the surface soil with roots, which
bj decaying have given it organic matter, thus dark-
ening its color, rendering it warmer, and giving it
greater ability to absorb heat and moisture, and to
retain manures. All of these effects render the sur-
face soil more fertile than it was before vegetable
growth commenced, unless, by the removal of crops,
its earthy plant-food has been too much reduced ;
and, where frequent cultivation and manures have
been applied, a still greater benefit has resulted. In
most instances the subsoil may, by the same means,
be gradually improved in condition until it equals
the surface soil in fertility. The means of produc-
ing this result, also further accounts of its advan-
tages, will be given under the head of Cultivation
(Sec. lY.).
IMPEOVEMENT.
From what has now been said of the character of
the soil, it must be evident that, as we know the
causes of fertility and barrenness, we may by the
proper means inprove the character of all soils
which are not now in the highest state of fertility.
Chemical analysis of the soil cannot give us any
reliable indication of its fertility or barrenness ; so
much depends on the state of solubility of the min-
eral plant-food, on the uniformity of its distribution
76 THE SOIL.
through the soil, on the extent to which it is exposed
on the surface of particles, and probably on other
conditions concerning which we are in doubt, or of
which we are entirely ignorant, that the mere weigh-
ing and measuring of the laboratory, has very little,
if any, value to the practical farmer.
We can learn something of the capacities of the
soil from the character of the plants which grow
naturally upon it, and much more from its ability
to produce larger crops of one kind than of another ;
something from the effect of different mineral ma-
nures upoD plants growing on it.
The best use to which the farmer can apply the
teachings of chemistry is in making such improve-
ments as the foregoing indications show to be neces-
sary, and, above all, in giving to the soil for each
crop, or for each rotation of crops, the full equiva-
lent of the minerals that they take away.
An examination, such as any farmer may make,
will show us its deficiencies in inechanical character,
and we may apply the proper treatment to increase
fertility. In some instances the soil may contain
everything that is required, but not in the proper
condition. For instance, in some parts of Massachu-
setts, there are nearly harren soils which show by
analysis precisely the same chemical composition as
the soil of the Miami valley of Ohio, one of the most
fertile in the world. The cause of this great differ-
ence in their agricultural capabilities, is that the
Miami soil has its particles finely pulverized ; while
in the Massachusetts soil the ingredients are com-
THE SOIL. 77
billed within particles (such as pebbles, etc.), where
they are out of the reach of roots.
In other cases, we find two soils, which are equal-
ly well pulverized, which are of the same color and
texture, and which appear to be of the same char-
acter, yet having very different power to support
crops. Chemical analysis, could it accurately show,
not only the kinds and quantities of plant food con-
tained in these soils, but the condition in which it
exists as to solubility, etc., would undoubtedly in-
dicate a very great difference between them.
All of these differences may be overcome by the
use of the proper means. Sometimes it could be
done at an expense which would be justified by the
result ; and at others, it might require too large an
outlay to be profitable. It becomes a question of
economy, not of ability, and science is able to estimate
the cost.
A soil cannot be cultivated understandingly until
it has been rigidly subjected to such examinations as
will tell us, as nearly as any examination can tell it,
what is necessary to render it fertile. Even after
fertility is perfectly restored it requires thought and
care to maintain it. The different ingredients of
the soil must be returned in the form of manures as
largely as they are removed by the crop, or the sup-
ply will eventually become too small for the purposes
of vegetation.
SECTION THIRD.
MANURES
SECTIOI THIRD.
MANURES
CHAPTEK I.
CHARACTER A^B VARIETIES OF MA-
NURES.
The study of the science of manures is one of the
most important branches of the practical education
of a farmer. ISTo baker would be called a good prac-
tical baker, who kept his flour exposed to the sun and
rain. 'No shoemaker would be called a good practi-
cal shoemaker, who used morocco for the soles of his
shoes, and heavy leather for the uppers. No car-
penter would be called a good practical carpenter,
who tried to build a house without nails, or other
fastenings. So with the farmer. He cannot be
called a good practical farmer if he keeps the ma-
terials, from which he is to make plants, in such a
condition, that they will have then' value destroyed,
uses them in the wrong places, or tries to put them
82 MANURES.
together without having everything present that is
necessary. Before he can work to the best advan-
tage, he must know what manures are composed of,
how they are to be preserved, where they are needed,
and what kinds are required. True, he may from
observation and experience, guess at results, but he
cannot know that he is right, and that he gets his re-
sults in the cheapest and most economical way, until
he has learned the facts above named. In this section
of our work, we shall endeavor to convey some of the
information necessary to this branch of practical
farming.
We shall adopt a classification of the subject some-
what different from that found in most works on
manures, but the facts are the same. The action of
manures is either mechanical or chemical^ or a com-
bination of both. For instance : some kinds of ma-
nure improve the mechanical character of the soil,
such as those which loosen stiff clay soils, or others
which render light sandy soils compact — these are
called TYiechaiiical manures. Some again furnish food
for plants — these are called chemical manures.
Many mechanical manures produce their effects
by means of chemical action. T\i\x^ potash combines
chemically with sand in the soil. In so doing, it
roughens the surfaces of the particles of sand, and
renders the soil less liable to be compacted by rains.
In this manner, it acts as a mechanical manure. The
compound of sand and potash,^ as well as the potash
alone, may enter into the composition of plants, and
* Silicate of potash.
MANURES. 83
hence it is a chemical manure. In other words, pot-
ash belongs to both classes described.
It is important that this distinction shonld be well
understood by the learner, as the words " mechani-
cal " and " chemical " in connection with manures
will be made use of through the following pages.
There is another class of manures which we shall
call absorbents. These comprise those substances
which have the power of taking up fertilizing mat-
ters, and retaining them for the use of plants. For
instance, charcoal is an absorbent. As was stated
in the section on soils, this substance is a retainer
of all fertilizing gases and of many minerals.
Other matters made use of in agriculture have the
same effect. These absorbents will be spoken of
more fully in their proper places.
TABLE.
Mechanical Manures are those which improve
the mechanical conditions of
Chemical " soils are those which serve as
food for plants.
MANURES.
Absorbents are those substances which absorb and
retain fertilizing matters.
Manure may be divided into three classes, viz. :
organic^ mineral^ and atnnospheric.
84 MANURES.
Organic manures comprise all animal and vege-
tahle matters which are used to fertilize the soil, such
as dung, swamp-muck, etc.
MmEKAL manures are those which are of a purely
mineral character, such as lime, ashes, etc.
Atmospheric manures consist of those organic
manures which exist in the form of gases in the at-
mosphere, and which are absorbed by rains and car-
ried to the soil. These are of the greatest impor-
tance. The ammonia and carbonic acid in the air
are atmospheric manures.
CHAPTEK II.
ANIMAL EXCREMENT
The first organic manure which we shall examine,
is animal excrement.
This is composed of those matters which have
been eaten by the animal as food, and have been
thrown off as solid or liquid manure. In order that
we may know of what they consist, we must refer to
the composition of food and examine the process of
digestion.
The food of animals, we have seen to consist of
both atmospheric and earthy matters. The atmos-
pheric part may be divided into two classes, i. e.^
that portion which contains nitrogen — such as glu-
ma:ntjres. 85
ten, albumen, etc., and that which does not contain
nitrogen — such as starch, sugar, oil, etc.
The earthy part of food may also be divided into
soluble matter and insoluble matter.*
DIGESTION AND ITS PKODUCTS.
Let us suppose that we have a fall-grown ox,
which is not increasing in any of his parts, but only
consumes food to keep up his respiration, and to sup-
ply the natural wastes of his body. To this ox we
will feed a ton of hay which contains organic mat-
ter, with and without nitrogen, and soluble and
insoluble earthy substances. E^ow let us try to fol-
low the food through its changes in the animal, and
see what becomes of it. Liebig compares the con-
sumption of food by animals to the imperfect burning
of wood in a stove, where a portion of the fuel is resolv-
ed into gases and ashes (that is, it is completely burn-
ed), and another portion, which is not thoroughly burn-
ed, passes oif as soot. In the animal action in ques-
tion, the food undergoes changes which are similar
to this burning of wood. A part of the food is di-
gested and taken up by the blood, while another por-
tion remains undigested, and passes the bowels as
solid dung — corresponding to the soot of combus-
tion. This part of the dung, then, we see is merely
so much of the food as passes through the system
* No part of animal manure is permanently and entirely insol-
uble. It would perhaps be better to classify these substances as
(1) those which are readily soluble, and (2) those which are but
slowly soluble.
86 MAINUEES.
without being materially qjianged. Its nature is
easily understood. It contains organic and mineral
matters in nearly the condition in which they existed
in the hay. They have been rendered finer and softer,
but their cheinical character (their composition) is not
materially altered. The dung also contains small
quantities of nitrogenous matter, which has leaked
out, as it were, from the stomach and intestines.
The digested food, however, undergoes further
changes which affect its character, and it escapes
from the body in three ways — i. e., through the
lungs and skin, through the bladder, and through
the bowels. It will be recollected from the first
section of this book, p. 20, that the carbon in the
blood of animals unites with the oxygen of the air
drawn into the lungs, and is thrown off in the
breath as carbonic acid. The hydrogen and oxygen
unite to form a part of the water which constitutes
the moisture of the breath.
That portion of the atmospheric part of the hay
which has been taken up by the blood of the ox, and
which does not contain nitrogen, is emitted through
the lungs. It consists, as will be recollected, of car-
bon, hydrogen, and oxygen, and these assume, in res-
piration, the form of carbonic acid and water.
The atmospheric matter of the digested hay, in
the blood, which does contain nitrogen, goes to the
'bladder, where it assumes the form of urea — a consti-
tuent of urine or liquid manure.
We have now disposed of the imperfectly digested
food (the dung), and of the atinospheric matter which
MANURES. - 87
was taken up by the blood. All that remains to be
examined is the earthy matter in the blood, which
would have become ashes ^ if the hay had been
burned. The readily soluble part of this earthy mat-
ter passes into the bladder, and forms the eartJiy
parts of urine. The more insoluble part passes the
bowels, in connection with the dung.
If any of the food taken up by the blood is not
returned as above stated, it goes to form fat, muscle,
hair, b©nes, or some other part of the animal, and as
he is not growing (not increasing in weight) an
equivalent amount of the body of the animal goes to
the manure to take the place of the part retained.*
We now have our subject in a form to be readily
understood. We learn that when food is given to
animals it is not jput out of existence^ but is merely
changed in form / and that in the impurities of the
breath, we have a large portion of those parts of the
food which plants obtain from air and from water ;
while the solid and liquid excrements contain all that
was taken by the plants from the soil andfrom manures.
The Solid Dung contains the undigested parts of the
food, the more insoluble
parts of the ash, and the
nitrogenous matters which
have escaped from the di-
gestive organs.
* This account of dig-estion is not, perhaps, strictly accurate in
a physiological point of view, but it is sufficiently so to give an
elementary understanding' of the character of excrement as
manure.
88 MANURES.
The Liquid Manure contains the nitrogenous parts of
the digested food, and the
soluble parts of the ash.
The Breath contains those parts of the fully di-
gested food which contain
carbon, hydrogen, and oxy-
gen, but no nitrogen, or at
least a very inconsiderable
quantity of it.
CHAPTER III.
WASTE or MANURE.
The loss of manure is a subject which demands most
serious attention. Until within comparatively few
years, little was known of the true character of
manures, and consequently of the importance of
protecting them against loss.
The chief causes of waste are evaporation and
leaching.
evaporation.
Evaporation is the changing of a solid or liquid
body to a vapory form. Thus common smelling
salts, a solid, if left exposed, passes into the- atmos-
phere in the form of a gas or vapor. Water, a liquid,
evaporates, and becomes a vapor in the atmosphere.
MANURES. 89
This is tlie case with very many substances in or-
ganic nature, both solid and liquid : they are liable
to assume a gaseous form, and become mixed with
the atmosphere. They are not destroyed, but are
changed in form.
As an instance of this action, suppose an animal
to die and to decay on the surface of the earth.
After a time, the flesh will entirely disappear, but is
not lost. It no longer exists as the flesh of an ani-
mal, but its carbon, hydrogen, oxygen, and nitrogen,
still exist in the air. They have been liberated from
the attractions which held them together, and have
passed away ; but (as we already know from what
has been said in a former section) they are ready to
be again taken up by plants, and pressed into the
service of life.
The evaporation of liquids may take place without
the aid of anything but heat ; but, in the case of
solids, it is often assisted by decay and combustion,
which break up the bonds that hold the constituents
of bodies together, and thus enable them to return
to the atmosphere, from which they were originally
derived.
It must be recollected that everything which has
an odoT (or can be smelled) is evaporating. The
odor is caused by parts of the body floating in the
air, and acting on the nerves of the nose. This is
an invariable rule ; and when we perceive an odor,
we may be sure that parts of the material from which
it emanates are escaping. If we perceive the odor
of an apple, it is because parts of the volatile oils of
90 MANTJKES.
the apple enter the nose. The same is true when we
smell hartshorn, cologne, etc.
The intensity of these odors bears no relation to
the amount of the substance passing into the air ; for
instance, a grain of musk will continue to give off
a strong odor for many years, while gum camphor,
with a much less intense odor, wastes away very
rapidly. Ammonia escapes rapidly.
Manures made by animals have an offensive odor,
simply because volatile parts of the decomposing
manure escape into the air, and are therefore made
perceptible. All organic parts in turn may become
volatile, assuming a gaseous form as they decom-
pose.
We do not see the gases rising, but there are many
ways by which we can detect them. If we wave a
feather over a manure heap, from which ammonia is
escaping, the feather having been recently dipped in
muriatic acid, white fumes will appear around the
feather, being the muriate of ammonia formed by the
union of the escaping gas with the acid. JSTot only
ammonia, but also carbonic acid, and other gases
which are useful to vegetation escape, and are given
to the winds. Indeed it may be stated in few words
that all of the organic part oi plants (all that was ob-
tained from the air, from water, and from ammonia),
constituting more than nine-tenths of their dry weight,
may be evaporated by the assistance of decay or
combustion. The atmospheric parts oi manures may
be lost in the same manner ; and, if the process of
decomposition be continued long enough, nothing
MAJSTIEES. 91
but a mass of earthy matter will remain, except a
small quantity of carbon which has not been resolved
into carbonic acid.
The proportion of solid manure lost by evaporation
(made volatile by the assistance of decay) may be a
very large part of the whole. Manure cannot be kept
a single day in its natural state without losing some-
thing. It commences to give out an offensive odor
immediately, and this odor is often accompanied, as
was before stated, by the loss of some of its fertiliz-
ing parts.
Animal manure contains, as will be seen by refer-
ence to p. 86, all of the substances contained in
plants, though not always in the correct relative pro-
portions to each other. When decomposition com-
mences, the carbon unites with the oxygen of the
air, and passes off as carbonic acid ; the hydrogen
and oxygen combine to form water (which evapo-
rates), and the nitrogen is mostly resolved into am-
monia, wJiich escapes into the atmosphere, unless ab-
sorbed by substances artificially applied for the pur-
pose, or retained by the carbon, organic acids, or
other products of decomposition with which it may
become united.
If manure is thrown into heaps, it often ferments
so rapidly as to produce sufficien #heat to set fire to
some parts of the manure, and cause its gases to be
thrown off with greater rapidity. This may be observ-
ed in nearly all heaps of animal excrement. When
they have lain for some time in mild weather, gray
streaks of ashes are often to be seen in the centre of
92 MANURES;
the pile. The organic part of the manure having
been humed away, nothing but the ash remains, —
this is called fire-fanging.
Manures kept in cellars without being mixed with
refuse matter are subject to some loss by evaporation
unless they are so situated as to absorb the urine,
when they are less likely to become injuriously heated.
When kept in the yard, they are much more liable
to loss from excessive evaporation. They are here
often saturated with the water of rains, which, in its
evaporation, carries away ammonia and carbonic acid
w^hich it has obtained from the rotting mass. The
evaporation of the water is rapidly carried on, on
account of the great extent of surface. The whole
mass is spongy, and soaks the liquids up from below
(through hollow straws, etc.), to be evaporated at the
surface on the same principle as causes the wick of a
lamp to draw up the oil to supply fuel for the flame.
Liquid Manuee containing large quantities of
nitrogen, and forming much ammonia, is also liable
to lose all of its organic parts from evaporation (and
fermentation), so that it is rendered as much less
valuable as is the solid dung.
From these remarks, it may be justly inferred that
a very large portion of the value of soKd and liquid
manure may be lost by evaporation in a sufficient
length of time, depending on circumstances, whether
it be a few months or several years. The wasting
commences as soon as the manure is dropped, and
continues, except in very cold weather, until the
destruction is complete. Hence we see that true
MANURES. 93
economy requires that tlie manures of the stable,
sty, and poultry-house, should be protected (as will
be hereafter described) as soon as possible after they
are made.
LEACHING.
The subject of leaching is even more important
in considering the earthy parts of manures than
evaporation is to the atmospheric, while leaching also
affects the atmospheric products of decay, they being
absorbed by water to a great degree.
A good illustration of leaching is found in the
manufacture of potash. When water is poured over
wood-ashes, it dissolves their potash which it carries
through in solution, making ley. If ley is boiled to
dryness, it leaves the potash in a solid form, proving
that this substance had been dissolved by the water
and removed from the insoluble parts of the ashes.
In the same way, water in passing through ma-
nures takes up their soluble portions as fast as liberated
by decomposition, and carries them to waste, and they
are lost to the manure. There is but a small quan-
tity of ash exposed for leaching in fresh dung ;
but, as the decomposition of the atmospheric part
proceeds, it continues to develop it more and more
(in the same manner as burning would do, only more
slowly), thus preparing fresh supplies to be carried
off with each shower. In this way, while manure
may be largely injured by evaporation, the soluble
parts may be removed by water until but a small
remnant of its original fertilizing properties remains.
94 MANUitES.
It is a singular fact concerning leaching, that
water is able to carry no part of the organic con-
stituents of vegetables to any considerable depth
below the surface in a fertile soil. They would
probably be carried to an unlimited distance in pure
sand, as it contains nothing which is capable of ar-
resting them ; but, in most soils, the clay and car-
bon which they contain retain all of the ammonia ;
also nearly all of the matters which go to form the
ashes of plants very near the surface of the soil. If
such were not the case, the fertility of the earth
must soon be destroyed, as all of those elements
which the soil must supply to growing plants would
be carried down out of the reach of roots, and leave
the world a barren waste, its surface having lost its
elements of fertility, while the downward filtration
of these would render the water of wells and springs
unfit for our use. Now, however, they are all re-
tained near the surface of the soil, and the water
issues from springs comparatively pure.
Evaporation removes from manure —
Carbon, in the form of carbonic acid.
Hydrogen and oxygen, in the form of
water.
Nitrogen, in the form of ammonia.
Leaching removes from manure—
The soluble and most valuable parts of
the ash in solution in water, besides
carrying away some of the above-
named forms of organic matter.
H
MANURES. 95
CHAPTEE lY.
ABSORBEN^rS.
Before considering further the subject of animal
excrement, it is necessary to examine a class of ma-
nures known as absorbents. These comprise all mat-
ters which have the power of absorbing (or soaking
up) the gases which arise from the evaporation of
solid and liquid manures, and retaining them until
required by plants.
The most important of these is undoubtedly clay,
which forms a large part of nearly all fertile soils.
The use of this in connection with manure will be
spoken of in describing the treatment of night-soil.
For ordinary use one of the most valuable absorb-
ents is charcoal.
CHARCOAL.
Cha/rcoalj in an agricultual sense, means all forms
of carbon, whether as peat, muck, charcoal dust from
the spark-catchers of locomotives, charcoal hearths,
river and swamp deposits, leaf mould, decomposed
spent tanbark or sawdust, etc. In short, if any veg-
etable matter is decomposed with the partial exclu-
sion of air (so that there shall not be oxygen enough
supplied to unite with all of the carbon), a portion
of its carbon remains in the exact condition to per-
form the best agricultural offices of charcoal.
The operation of carbonaceous matter in the soil
96 MANUKES.
was explained in a former section (Sec. 2), and we
will now examine merely its action with regard to
manures. When properly applied to manures, in
compost, it has the following effects :
1. It absorbs and retains the fertilizing gases evap-
orating from decomposing matters.
2. It acts as a divisor, thereby reducing the
strength (or intensity) of powerful manures — thus
rendering them less likely to injure the roots of
plants ; and also increases their bulk, so as to pre-
vent fire-fanging in composts.
3. It in part prevents the leaching out of the solu-
ble parts of the ash.
4. It keeps the compost moist.
The first-named office of charcoal, i. e., absorbing
and retaining gases, is one of the utmost importance.
It is this quality that gives to it so high a position
in the opinion of all who have used it. As was
stated in the section on soils, carbonaceous matter
seems to be capable of absorbing everything which
may be of use to vegetation. It is a grand purifier,
and while it prevents offensive odors from escaping,
it is at the same time storing its pores with food for
the nourishment of plants.
2d. In its capacity as a divisor for manures, char-
coal is excellent in all cases, especially to use with
strongly concentrated (or heating) animal manures.
These, when applied in their natural state to the soil,
are very apt to injure young roots by the violence
of their action. When mixed with a divisor, such
manures are diluted, made less active, and conse-
MANUKES. 97
quentlj less likely to be injurious. In composts,
manures are liable, as has been before stated, to be-
come burned by the resultant heat of decomposi-
tion ; this process of combustion is prevented by the
liberal use of divisors, because, by increasing the
bulk, the heat, being diffused through a larger mass,
becomes less intense. The same principle is exhibit-
ed in the fact that it takes more fire to boil a caul-
dron of water than a tea-kettlefulL
3d. Charcoal has much power to arrest the
passage of mineral matters in solution ; so much so,
that compost heaps, well supplied with muck, are
less affected by rains than those not so supplied.
All composts, however, and all organic manures
should be kept under cover until spread upon the
land.
4th. Charcoal keeps the compost moist, from the
ease with which it absorbs water, and its ability to
retain it.
With these advantages before us, we must see the
importance of an understanding of the modes for
obtaining charcoal. Many farmers are so situated
that they can obtain sufficient quantities of charcoal
dust. Others have not the same facilities. Nearly all,
however, can obtain muck or leaf mould, and to this
we will now turn our attention.
MUCK AND ITS TREATMENT.
By muck^ we mean the vegetable deposits of
swamps and rivers. It consists of decayed organic
98 MANURES.
substances, mixed with more or less earth. Its prin-
cipal constituent is carbon^ in different degrees of
development, which has remained after the decom-
position of vegetable matter. Muck varies largely
in its quality according to the amount of carbon
which it contains, and the completeness of its decom-
position. The best muck is usually found in compa-
ratively dry locations, where the water which once
caused the deposit has been removed. Muck which has
been long in this condition, is usually better decom-
posed than that which is saturated with water. The
muck from swamps, however, may soon be brought
to the best condition. It should be thrown out if
possible at least a year before it is required for use,
and left in small heaps or ridges, exposed to the
action of the weather, which will assist in pulveriz-
ing it, while, from having its water removed, its
decomposition goes on more rapidly.
After the muck has remained in this condition a
sufficient length of time, it may be removed to the
barn-yard and composted with a mixture of lime and
salt (described on page 99 in the proportion of one
cord of muck to four bushels of the mixture, or with
slaked lime, or wood-ashes. At the end of a month
or more, the muck in the compost will have been re-
duced to a fine pulverulent mass, the decomposition
being hastened and made more complete by repeated
turnings — nearly as valuable as charcoal dust for
application to animal excrement. "When in this
condition it is 0.2}^^^ jprepared muck, by which name
it will be designated in the following pages.
MANUEES. 99
Muck had better not be used immediately after
being taken from the swamp, as it is then almost
always sour. Its sourness is due to acids which it
contains, and these must be rectified by the applica-
tion of an alkali, or by long exposure to the weather,
before the muck is suitable for use.
LIME A^T> SALT MrXTUEE.
The mixture, lime and salt, used in the decompo-
sition of muck, is made in the following manner :
Recipe. — Take three bushels of shell lime, hot
from the Tciln, or as fresh as possible, and slake it
with water in which one bushel of salt has been dis-
solved.
Care must be taken to use only so much water as
is necessary to dissolve the salt, as it is difficult to
induce the lime to absorb even so large a quantity.
In dissolving the salt, it is well to hang it in a
basket in the upper part of the water, as the salt
water will immediately settle towards the bottom
(being heavier), and allow the freshest water to be
nearest to the salt. In this way the salt may be all
dissolved, and thus make the brine used to slake the
lime. It will be necessary to apply the brine at
intervals of a day or two, and to stir the mass often,
as the amount of water is too great to be readily ab-
sorbed.
This mixture should be made under cover, as, if
exposed, it would obtain moisture from rain or dew,
which would prevent the use of all the brine.
100 MANURES.
Another objection to its exposure to the weather
is its liability to be washed away by rains. It
should be at least ten days old before being used,
and would be improved by an age of three or four
months, as the chemical changes it undergoes will
require some time to be completed.
The character of this mixture is not very clearly
understood. Its principal constituents are lime,
carbonic acid, chlorine, and soda. The salt is
undoubtedly decomposed in part or entirely, and
various compounds, containing the above substances
in different proportions and in different forms of
combination, are formed. Probably the extent of
the decomposition of the salt and the character of the
new combinations depend on various circumstances,
and vary considerably.
These compounds are much better agents in the
composition of muck than pure salt and lime.
When shell lime cannot be obtained, Thomaston,
or any other very pure lime, will answer ; but care
must be taken that it do not contain much magnesia.
LIME.
Muck may be decomposed by the aid of other
materials. Lime is very efficient, though not so
much so as when combined with salt. The action of
lime, when applied to the muck, depends very much
on its condition. Air-slaked lime (carbonate of lime)
has less effect than hydrate of lime (lime simply slaked
with water), because it is less caustic in its character.
MANURES. 101
POTASH.
Potash is a very active agent in decomposing
vegetable matter, and may be used with great ad-
vantage, especially where the soil which is to be
manured is deficient in potash.
Unleached wood-a^hes are generally the best source
from which to obtain this, and from live to twenty-
five bushels of the&e mixed with one cord of muck
will have a capital efifect.*
The sparlings (or refuse) of potash warehouses may
often be purchased at sufiiciently low rates to be used
for this purpose, and answer an excellent end. They
may be applied at the rate of from twenty to one
hundred pounds to each cord of muck.
By any of the foregoing methods, muck may be
jprejpared for use in composting.
CHAPTEE Y.
COMPOSTINa STABLE MANTJEE.
In composting stable manure in the most economical
manner, the evaporation of the gases which result
from its decomposition, and the leaching out of the
ashy (and other) portions which decomposition has
* Leached ashes will not supply the place of these, as the leach-
ing has deprived them of most of their potash.
102 MANURES.
set free must be avoided, while the mass is kept in
such condition as to admit of the perfect decomposi-
tion of the manure.
Solid manures in their fresh state are of but very lit-
tle use to plants. It is only as they are decomposed,
and have their nitrogen turned into ammonia, and
their other ingredients prepared to be taken up again
by plants, that they are of much value as fertilizers,
although there are of course certain advantages
resulting from their fermentation in the ground,
while there is no better way to avoid loss than by
plowing fresh manure directly into the soil. We have
seen that, if decomposition takes place without
pi-oper precautions being taken, the most valuable
parts of the manure would be lost. ISTor is it advisa-
ble, when an immediate effect is wanted, to keep
manures from decomposing until they are applied to
the soil, for then they are not immediately ready for
use, and time is lost. By composting, we aim to
save everything while we prepare the manures for
immediate use.
SHELTER.
The first consideration in preparing for compost-
ing is to provide proper shelter. This may be done
either by means of a shed or by arranging a cellar
under the stables, or in any other manner that may
be dictated by circumstances. It is no doubt better
to have the manure shed enclosed so as to make it an
effectual protection ; this, however, is not absolutely
necessary if the roof project far enough over the
MiJSTJEES. 103
compost to shelter it from the sun's rajs and from
driving rains.
The importance of some protection of this kind
is evident from what has ah-eady been said, and in-
deed it is impossible to make an economical use of
manures without it. The trifling cost of building a
shed, or preparing a cellar, is amply repaid in the
benefit resulting from their uses. If an open shed is
used, care should be taken to so arrange the slope of
the ground that no surface water can reach the
manm^e.
THE FLOOE.
The floor or foundation on which to build the
compost deserves some consideration. It may be of
plank tightly fitted, a hard bed of clay, or better, a
cemented surface. Whatever material is used in its
construction (and stiff clay mixed with water and
beaten compactly down answers an excellent purpose),
the floor must have such an inclination as will cause
it to discharge water only at one point. That is, one
part of the edge must be lower than the rest of the
floor, which must be so shaped that water wiU run
towards this point from every part of it ; then — the
floor being water-tight — aU the liquids of the com-
post may be collected in a
TANK.
This t(m\ used to collect the liquids of the manure,
may be made by sinking a barrel or hogshead (ac-
104
MANUEES.
cording to the size of the heap) in the ground at the
point where it is required, or in any other conveni-
ent manner.
In the tank a pump of cheap construction may be
placed, to raise the liquid to a sufficient height to be
conveyed by a trough to the centre of the heap,
and there distributed by means of a perforated board
Fig. 2.
a, tank ; 5, pump ; c and g\ perforated board ; d, muck ; e, ma-
nure ; /, floor.
with raised edges, and long enough to reach across
the heap in any direction. By altering the position
of this board, the liquid may be carried evenly over
the whole mass.
MANURES. 105
The appearance of the apparatus required for com-
posting, and the compost laid up, may be better
shown by the foregoing figure.
The compost is made by laying on the floor ten or
twelve inches of muck, and on that a few inches of
manure, then another heavy layer of muck, and an-
other of manure, continuing in this manner until the
heap is raised to the required height, always having
a thick layer of muck at the top.
After laying up the heap, the tank should be filled
with liquid manure from the stables, slops from the
house, soap-suds, or other water containing fertilizing
matter, to be pumped over the mass. There should
be enough of the liquid to saturate the heap and
filter through to fill the tank once or twice a week,
at which intervals it should be again pumped up,
thus continually being passed through the manure.
This liquid should not be changed, as it contains
much soluble manure. Should the liquid manures
named above not be sufiicient, the quantity may be
increased by the use of rain-water. That falling
during the first ten minutes of a shower is the best,
as it contains the most ammonia.
The effects produced by frequently watering the
compost constitute one of the greatest advantages of
this system.
The soluble portions of the manure are equally
diffused through every part of the heap.
Should the heat of fermentation be too great, the
watering will reduce it.
When the compost is saturated with water, the
5*
106 - MANURES.
air is driven out ; and, as the water subsides, fresh
air enters and takes its place. The fresh air con-
tains oxygen, which assists in the decomposition of
the manure.
In short, the watering does all the work of fork-
ing over by hand much better and much more cheaply.
At the end of a month or more, this compost will
be ready for use. The layers in the manure will
have disappeared, the whole mass having become of
a uniform character, highly fertilizing, and ready to
be immediately used by plants.
It may be applied to the soil, either as a top-dress-
ing, or otherwise, without fear of loss, as the muck
will retain all of the gases which would otherwise
evaporate.
The cost and trouble of the foregoing system of
composting are trifling compared with its advantages.
The quantity of the manure is much increased, and
its quality improved. The health of the animals is
secured by the retention of those gases, which, when
allowed to escape, render impure the air that they
have to breathe.
The cleanliness of the stable and yard is much im-
proved, as the effete matters, which would otherwise
litter them, are carefully removed to the compost.
The system of composting described above is the
most complete that has yet been suggested for mak-
ing use of solid manures. Many other methods may
be adopted when circumstances will not admit of
so much attention. It is a common and excellent
practice to throw prepared muck into the cellar under
MANUilES. 107
the stables, to be mixed and turned over with the
manure by swine. In other cases the manures are
kept in the yard, and are covered with a thin layer
of muck every morning. The principle which ren-
ders these systems beneficial is that of the absorbent
power of charcoal.
The composting of stable manure, although al-
ways advantageous, frequently requires more labor,
and more expensive accommodations than can be
given to it. There is no doubt that, where proper fa-
cilities can be obtained for carrying out the foregoing
directions, they will be found profitable. Those who
are obliged to use their stable manure with the least
possibly amount of handling, or who cannot procure
muck or other organic matter to add to it, should at
least manage to keep it entirely sheltered from the rain
until it is hauled out on to the land. Manure kept
under a shed, necessarily loses some ammonia ; but
the amount of this loss has been found to be very
small, for the reason that, during the decomposition
of the straw and coarser vegetable parts, certain
organic acids and other compounds are produced,
which combine with or absorb most of the ammonia
as it is generated.
The loss of ammonia, and of the soluble constitu-
ents of the ash, is greater when the decomposition
takes place without protection from the rain.
The best plan is, undoubtedly, to have a cellar
under the stable to receive the manure as soon as
dropped, and to protect it, as far as possible, from all
atmospheric influences.
108 MANURES.
For a long time one of the strongest recommenda-
tions of "book farming" was directed against the
practice of spreading manure upon the land more
than a day or two before it could be plowed under.
But on this point, practice has gained a triumph
over a crude theory. There is no doubt that manure
so spread is subject to some waste ; but that which
is not wasted is so much better incorporated with
the soil by the water of rains, which distributes its
soluble parts evenly among all of its particles, that
the effect produced is better than if the raw manure
had been immediately plowed under, necessarily
somewhat irregularly and in spots. In this latter
case there would be no loss of material, but some
parts of the soil would receive more than was neces-
sary, while others would be deprived of any material
benefit, and the land would be less fertile than if
every root were sure to find, in every part of the
soil, its due proportion of the food. Ammonia is
formed only during decomposition ; and, especially
during cold weather, there is very little decomposi-
tion going on in manure which is thinly spread upon
the surface of the land ; hence the loss from this
cause is not great.
In the case of very heavy manuring, especially
with undecomposed manure on clay land, there is a
great benefit arising from the fermentation of the
dung in the soil, — a chemical action producing a
mechanical effect, — ^but ordinarily it is at least a ques-
tion whether it is not best to spread the manure
on the surface as long as possible before plowing,
MANURES. 109
unless in the case of land whicli is to be plowed in
the fall for spring crops, when it is well to spread
the manure after plowing, to be harrowed in in
the spring.
This practice is of course not admissible on steep
hill-sides or other surfaces where the manure would
be subjected to the danger of being washed away by
water flowing over the surface in winter or spring.
Different circumstances necessarily require a dif-
ferent treatment of manure ; but the following prin-
ciples are applicable to all cases :
1. All organic manures are much improved by
being thoroughly decomposed before being applied
to the land.
2. It is always advantageous (though not always
advisable) that their fermentation take place in the
compost heap, where they give a part of their value
to muck or other refuse organic matter, which pre-
vents all waste of fertilizing gases.
3. All animal manures should be carefully pro-
tected against sun, rain, and wind, from the time they
are dropped until they are spread upon the land.
4. The solid dung should always be so kept that
it will absorb the urine.
5. For the mecfianical improvement of the soil,
raw manure should be deeply mixed with it.
6. For immediate fertilizing effect, well-rotted
manure should be applied to, and harrowed in near
the sm^face.
tlO MANURES.
LIQUID MANURE.
Liquid maiiure from animals may, also, be made
useful bj the assistance of prepared muck. Where
a tank is used in composting, the liquids from the
stable may all be employed to supply moisture to the
heap ; but where any system is adopted, not requir-
ing liquids, the urine may be applied to muck heaps,
and there allowed to ferment. Fermentation is ne-
cessary in urine as well as in solid dung, before it is
very active as a manure, although its decomposition
is much more rapid than that of the dung. Urine,
as will be recollected, contains nitrogen and forms
ammonia on fermentation.
The urine should never be allowed to stand in
pools to become mixed with rain-water, nor to run
to waste ; but should always be immediately ab-
sorbed either by the dung or by muck, or other refuse
matter provided for the purpose.
By referring to the analysis of liquid and solid
manure in Section Y., their relative value may be
seen.
CHAPTEK YI.
DIFFERENT K I ND S O F AN I M A L EXCREMENT.
The manures of different animals are, of course, of
different value as fertilizers, varying according to
the food, the age of the animals, etc.
MANURES. Ill
Yet the difference is not so great as would be sup-
posed. The quality of manure depends very much
more upon the food from which it is made than upon
the animal by which it is made. Linseed meal or
cotton-seed meal, which contains much nitrogen, and
is rich in phosphates, makes manure worth infinitely
more than that from straw and turnips. Whether
these articles of food have passed through an ox or
a hog, makes very little difference; though, as ex-
plained below, it does make some difference.
STABLE MANUKE.
By stable manure we mean, usually, that of the
horse, and that of horned cattle. The case described
in Chapter II. (of this Section) was one where the
animal was not increasing in any of its parts, but
returned in the form of manure, and otherwise, the
equivalent of everything eaten. This case is one of
the most simple kind, and is subject to many modifi-
cations.
The growing animal is increasing in size, and as
he derives his increase from his food, he does not re-
turn in the form of manure so much as he eats. If
his bones are growing, he is taking from his food
phosphate of lime and nitrogenous matter ; conse-
quently, the manure will be poorer in these ingre-
dients. The same may be said of the formation of
the muscles, in relation to nitrogen.
ThQ fattening animal, if full grown, makes manure
which is as good as that from animals that are not
112 ' MANURES.
increasing in size, because the fat is taken from
those parts of the food which are obtained by plants
from the atmosphere, and from water {i. e. from the
substances containing no nitrogen). Fat contains
no nitrogen, and, consequently, does not lessen the
amount of this ingredient in the manure.
Milch Cows use a part of their food for the forma-
tion of milk, and consequently they produce manure
of reduced value.
The solid manure of the horse is better than that
of the ox, while the liquid manure of the ox is com-
paratively better than that of the horse. The cause of
this is, that the horse has less perfect digestive organs
than the ox, and consequently passes more of the
valuable parts of his food, in an undigested form, as
dung ; while the ox, from chewing the cud and hav-
ing more perfect digestion, turns more of his food in-
to urine than does the horse.
RECAPITIJLATION.
Full Grown animals not '
producing milk, and
full grown animals fat-
tening
The Growing of Animals reduces the value of their
manure, portions of their food being taken to form
their bodies.
Milch Cows reduce the value of their manure by
changing a part of their food into milk.
► make the best manure.
MANURES. 113
The Ox makes poor dung and rich urine.*
The Hokse makes rich dung and poor urine.*
NIGHT SOIL.
The hest manure within the reach of the farmer is
night soil, or human excrement. The manure of
man consists (as does that of any other animal) of
those parts of his food which are not retained in the
increase of his body. If he be growing, his manure
is poorer, as in the case of the ox ; and it is subject
to all the other modifications named in the early
part'of this chapter. His food is usually of a varied
character, and is rich in nitrogen, the phosphates,
and other inorganic constituents ; consequently, his
manure is made valuable by containing large quan-
tities of these matters. As is the case with the ox,
the dung contains the undigested food, the secretions
(or leakings) of the digestive organs, and the insoluble
parts of the ash of the digested food. The urine, in
like manner, contains a large proportion of the nitro-
gen and the soluble inorganic parts of the digested
food. When we consider how much richer ihefood
of man is than that of horned cattle, we shall under-
stand the superior value of his excrement.
Night soil has been used as a manure, for ages, in
China and Japan ; and herein lies, undoubtedly, the
great secret of their success in supporting a dense
population, for almost countless ages, without im-
poverishing the soil.
* Comparatively.
Hi: MAi^UKES.
Some have supposed that manuring with night
soil would give disagreeable properties to plants :
this is not the case ; their quality is invariably im-
proved. The color and odor ot the rose are made
richer and more delicate by the use of the most of-
fensive night soil as manure.
It is evident that this is the case from the fact
that plants have it for their dh'ect object to make
over and put together the refuse organic matter and
the gases and the minerals found in nature, for the
us« of animals. If there were no natural means of
rendering the excrement of animals available to
plants, the earth must soon be shorn of its fertility,
as the elements of growth when once consumed
would be essentially destroyed, and no soil could
survive the exhaustion. There is no reason why the
manure of man should be rejected by vegetation
more than that of any other animal ; and indeed it
is not, — ample experience has proved that there is
no better manure in existence.
A single experiment will suffice to show that
night soil may be so kept that there shall be no loss
of its valuable gases, and consequently no offensive
odor arising from it, while it may be removed and
applied to crops without unpleasantness. All that is
necessary to effect this wonderful change in night
soil, and to turn it from its disagreeable character to
one entirely inoffensive, is to mix with it a little char-
coal dust, prepared muck, dry earth, or any other good
absorbent — thus making what is called poudrette.
The mode of doing this must depend on circumstances.
MANURES. 115
'^ Several plans have recently been devised which
have for their object the improvement of privy ac-
commodations of detached houses. One of these,
the ' Earth Closet,' of the Rev. Henry Moule, an
English clergyman, is at once so cheap, so simple,
and so perfect in its operation, that it should receive
general attention. Its action is based on the power
of soils which contain clay or organic matter (loam
or mould) to absorb all offensive effluvia. This
power is so great that not only will a pint of sifted
and air-dried earth completely deodorize the matters
of a single evacuation, but if dried in the air after
each use, the same pint of earth may be used over
and over again — losing, apparently, none of its
power of absorption— until it finally becomes as
powerful a manure as Peruvian guano — although
entirely inoffensive to the sight and smell." *
The manure thus made is of the most valuable
character, and may be used under any circumstances
with a certainty of obtaining a good crop.
For an analysis of human manure, see Section Y.
HOa MANURE.
Hog manure is very valuable, but it must be used
with care. It is very liable to make cabbages clumjp-
footed^ and to induce a disease in turnips called (mi-
hury (or fingers and toes). It is so violent in its
action that, when applied to crops in a pure state, it
* From an article on Sewers and Eartli Closets, in the Amen-
can Agricultural Annual, for 1868, by Geo. E. Waring, Jr.
116 MANURES.
often produces injurious results. The only precau-
tion necessary is to supply the sty with prepared
muck, charcoal-dust, leaf-mould, earth, or any ab-
sorbent in plentiful quantities, often adding fresh
supplies. The hogs will work this over with the
manure ; and, when required for use, it will be found
an excellent fertilizer. The absorbent will have over-
come its injurious tendency, and it may be safely
applied to any crop, except cabbages and the smooth-
leaved turnips — such as the rutabaga. From the
variety and rich character of the food of this animal,
his manure is of a superior quality.
Butchers' hogpen manure is one of the best fer-
tilizers known. It is made by animals that live
chiefly on blood and other animal refuse, and is very
rich in nitrogen and the phosphates. It should be
mixed with prepared muck, or its substitute, to pre-
vent the loss of its ammonia, and as a protection
against its injurious effect on plants.
POULTRY-HOTJSE MANURE.
Next in value to night soil, among domestic ma-
nures, are the excrements of poultry, pigeons, etc.
Birds live on the nice bits of creation, seeds, insects,
etc., and they discharge their solid and liquid excre-
ments together. Poultry-dung is nearly equal in
value to Peruvian guano (except that it contains
more water), and it deserves to be carefully pre-
served and judiciously used. It is as well worth one
dollar per bushel as guano is worth seventy-five dol-
lars a ton.
MANUEES. 117
Poultry-manure is liable to as much injury from
evaporation and leaching as is any other manure,
and equal care should be taken (by the same means)
to prevent such loss. Good shelter over the roosts,
and frequent sprinkling with prepared muck or char-
coal-dust, will be amply repaid by the increased value
of the manure, and its better action and greater
durability in the soil. The principle upon which
Moule's Earth Closet is based may be very effective-
ly applied to the poultry-house. All that is neces-
sary is to dig or fork up the earth floor of their lodg-
ing-room as often as may be necessary (say once a
week), and to rake it daily so as to mix the fresh
droppings with the loose earth. In this manner the.
floor of the poultry-house, for a depth of eight or ten
inches, may be made to absorb the droppings of a
whole summer so as to entirely prevent offensive
smells or disease, while the earth for that depth
will be worth many times what it has cost.
The value of this manure should be taken into
consideration in calculating the profit of keeping
poultry (as indeed with all other stock). It has been
observed by a gentleman of much experience, in
poultry raising, that the yearly manure of a hundred
fowls applied to previously unmanured land would
produce extra corn enough to keep them for a year.
This is probably a large estimate, but it serves to
show that this fertilizer is very valuable, and also
that poultry may be kept with great profit, if their
excrements are properly secured.
118 MA]STJBES.
The manure of pigeons has been a favorite fertil-
izer in some countries for more than 2,000 years.
Market gardeners in England attach much value
to rabbit- manure.
SHEEP MANURE.
The manure of sheep is less valuable than it would
be if so large a quantity of the nitrogen and mineral
parts of the food were not employed in the forma-
tion of wool. This has an effect on the richness of
the excrements, but they are still of very great value
as a fertilizer, and should be protected from loss in
the same way as stable-manure.
GUANO.
Guano as a manure has become world renowned.
The worn-out tobacco lands of Virginia, and other
fields in many parts of the country, which seemed to
have yielded to the effect of an ignorant course of
cultivation, and to have sunk to their final repose,
have in many cases been revived to the production of
excellent crops, and have had their value multiplied
many fold by the use of guano. Although an ex-
cellent manm'e, it should not cause us to lose sight of
•those valuable materials which exist on almost every
farm. Every ton of guano imported into the United
States is an addition to our national wealth, but
every ton of stable-manure, or poultry-dung, or night
soil evaporated or carried away in rivers, is equally
a deduction from our riches. If the imported ma-
nure is to really benefit us, we must not allow it to
MANUEES. 119
occasion the neglect and consequent loss of our do-
mestic fertilizers.
The Peruvian guano (which is considered the
best) is brought from islands off the coast of Peru.
The birds which frequent these islands live almost
entirely on fish, and drop their excrements here in
a climate where rain is unknown, and where, from
the dryness of the air, there is but little loss sustained
by the manure. It is brought to this country in
large quantities, and is an excellent fertilizer, supe-
rior even to night soil.
Injudiciously used, Peruvian guano may become
a curse to a country instead of a blessing. It stimu-
lates crops to an inordinate growth and causes them,
on the poorer soils, to seek out the last available atom
of some mineral which it does not in itself supply
in sufficient quantity. When this last atom has
been sold off in the crop, the power of the guano to
produce a crop, to which that mineral is largely
necessary, has ceased. It is not the guano, but the
crop that has exhausted the land. If all its mineral
constituents had been judiciously returned, the soil
would not be made poorer, — on the contrary, it
would be made better by the decomposition of the
roots left in the soil. The best way to use guano,
is to compost it with other manures or to mix it
with fine earth or muck. In either case, its lumps
should be crushed to powder, so that it may be evenly
distributed through the soil.
The composition of various kinds of guano may
be found in the Section on Analysis.
120 MANURES.
CHAPTEK YIl.
OTHER ORGANIC MANURES.
The number of organic manures is almost countless.
The most common of these have been described in
the previous chapters on the excrements of animals.
The more prominent of the remaining ones will now be
considered. As a universal rule, it may be stated that
all organic matter (everything which has had vegeta-
ble or animal life) is capable of feeding plants.
DEAD ANIMALS.
The bodies of animals contain much nitrogen^ as
well as large quantities of the phosphates and other
inorganic materials required in the growth of plants.
On their decay, the nitrogen is resolved into amtno-
nia^ and the mineral matters become valuable as food
for the inorganic parts of plants.
If the decomposition of animal bodies takes place
in exposed situations, and without proper precautions,
the ammonia escapes into the atmosphere, and much
of the mineral portion is leached out by rains. The
use of absorbents, such as charcoal-dust, prepared
muck, earth, etc., will entirely prevent the evapora-
tion, and will in a great measure serve as a protection
against leaching.
If a dead horse be cut in pieces and mixed with
ten loads of muck, the whole mass will, in a single
season, become a valuable compost. Small animals,
such as dogs, cats, etc., may be with advantage
MANURES. 121
bnried by the roots of grape-vines, or trees, or com-
posted as above.
BONES.
The hones of animals contain phosphate of lime
and gelatine. The gelatine is a nitrogenous sub-
stance, and produces ammonia on its decomposition.
This subject will be treated more fully under the
head of " phosphate of lime " in the chapter on min-
eral manures, where the treatment of bones is con-
sidered more directly with reference to the fertilizing
value of their earthy parts.
FISH.
In many localities near the sea-shore large quanti-
ties of fish are caught and applied directly to the soil.
These make excellent manure. They contain much
nitrogen, which renders them strongly ammoniacal
on decomposition. Their bones consist of phosphate
and carbonate of lime; and, being natm^ally soft, they
decompose in the soil with great facility, and become
available to plants. The scales of fish contain valu-
able quantities of nitrogen, etc., all of which are
highly useful.
Refuse fishy matters from markets and from the
house are well worth saving. These and fish caught
for manure may be made into compost with prepared
muck, or earth, etc. ; and as they putrefy rapidly, they
soon become ready for use. They may be added to
the compost of stable manure with great advantage.
122 MANURES,
Fisli (like all other nitrogenous manures) should
never be applied as a top dressing, unless previously
mixed with a good absorbent of ammonia ; but should,
when used alone, be immediately plowed under to
considerable depth, to prevent the evaporation — and
consequent loss — of their fertilizing gases.
Within the past few years the manufacture of oil from
fish has become a very extensive industry, especially
along the coast of New England. The fish are caught
in immense quantities and delivered to the factories,
where they are first cooked by steaming and then
subjected to very heavy pressure, which removes their
oil. The solid matter which is left behind, contain-
ing the bones, scales, and muscular tissues, is run
through a " picker," and sold for manure. It con-
tains all of the fish that is of value for this purpose,
in a very concentrated form, and it is easy of applica-
tion to the soil. It is now sold for about one-third
of the value of Peruvian guano, at which price it is
a much more economical fertilizer.
WOOLLEN KAGS, ETC.
Woollen rags^ hair, waste of woollen factories, etc.,
contain both nitrogen and phosphate of lime ; and, like
all other matters containing these ingredients, are
excellent manures, but they must be used in such a
way as to prevent the escape of their fertilizing gases.
They decompose slowly, and are therefore considered
a lasting manure. Like all lasting manures, how-
ever, they are slow in their effects, and the most ad-
MAI^UKES. 123
vantageous way to use them is to compost them with
stable manure, or with some other rapidly fermenting
substance, which will hasten their decomposition and
render them sooner available.
Rags, hair, etc., thns treated, will in a short time
be reduced to such a condition that they may be
more immediately used by plants instead of lying in
the soil to be slowly taken up. It is better in all
cases to have manures act quicJdy and give an im-
mediate retm-n for their cost, than to lie for a long
time in the soil before their influence is felt.
Old leather should not be thrown away. It de-
composes very slowly, and consequently is of but
little value ; but, if put at the roots of young trees,
it will in time produce appreciable effects.
Tanners' and curriers' refuse^ and all other animal
offal, including that of the slaughter-house, are well
worth attention, as they contain more or less of those
two most important ingredients of manures, nitrogen
and phosphate of lime.
It is unnecessary to add that, in common with all
other animal manm-es, these substances must be either
composted, or immediately plowed under the soil.
Horn piths, and horn shavings, if decomposed in com-
post with substances which ferment rapidly, make very
good manure, and are worth fully the price charged
for them.
ORGANIC MANURES OF TEGETABLE OKIGIN.
Muck^ the most important of the purely vegeta-
ble manures, has been already sufficiently described.
124 aiANURES.
It should be particularly borne in mind that, when
first taken from the swamp, it is often sour^ or cold ;
but that if exposed for a long time to the air, or if
well treated with lime, uiileached ashes, the lime
and salt mixture, or any other alkali, its acids will
be neutralized (or overcome), and it becomes a good
application to any soil, except peat or other soils
already containing large quantities of organic mat-
ter.
SPENT TAN-BAHK.
S^ent tan-harJc, if previously decomposed by the
use of alkalies, answers all the purposes of prepared
muck, but is more difficult of decomposition.
The bark of trees contains a larger proportion of
earthy matter than the wood, and much of this,
on the decomposition of the bark, becomes available
as manure. The chemical effect on the bark, of
using it in the tanning of leather, is such as to ren-
der it difficult to be rotted by the ordinary means ;
but by the use of alkalies it may be reduced to the
finest condition, and becomes a most excellent ma-
nure. Unless tan-bark be composted with lime, or
some other alkali, it may produce injurious effects
from the tanniG acid which it still contains. Alka-
line substances will neutralize this acid, and prevent
it from being injurious.
One great benefit resulting from the use of spent
tan-bark, is due to its power of absorbing moisture
from the atmosphere. For this reason it is very val-
MANURES. 125
liable for mulching * young trees and plants wlien
first set out.
SAWDUST AND SOOT,
Sawdust in its natural state is of very little value
to tlie land, but when decomposed, as may be done
by the same method as was described for tan-bark,
it is of some importance, on account of the carbon
that it contains. Its ash, too, which becomes avail-
able, contains soluble earthy matter, and in this
way it acts as a direct manure. So far as concerns
the value of the ash, however, bark is superior to
sawdust. Sawdust may be partially rotted by mix-
ing it with strong manure (such as that of the hog-
pen), while it acts as a divisor, and prevents its too
rapid action when applied to the soil. Some kinds
of sawdust, such as that from beech-wood, form acetic
acid on their decomposition, and these should be treat-
ed with, at least, a sufficient quantity of lime to cor-
rect the acid.
Soot is a good manure. It contains much carbon,
and has, thus far, all of the beneficial efiects of char-
coal dust. The sulphur, which is one of its consti-
tuents, not only serves as food for plants, but, from
its odor, afibrds a good protection against some in-
sects. A handful of soot thrown over a melon vine,
or young cabbage plant, will keep away many in-
sects.
Soot contains some ammonia, and as this is in
the form of a sulphate, it is not volatile, and conse-
* See the glossary at the end of the book.
126 MAJTCIRES.
quentlj does not evaporate when the soot is applied
as a top dressing, which is the almost universal cus-
tom.
GREEN CROPS.
Green crops, to plough under, are in many places
largely raised, and are always beneficial. The
plants most used for this purpose, in this country, are
clover, buckwheat, and peas. These plants have
very long roots, which they send deep in the soil to
draw up mineral matter for their support. This
mineral matter is deposited in the plant. The
leaves and roots receive carbonic acid very largely
from the air, and from the water in the soil. In this
manner they obtain their carbon. When the crop is
turned under the soil, it decomposes, and the car-
bon, as well as the mineral ingredients obtained
from the subsoil, are deposited in the surface soil,
and become of use to succeeding crops. The hol-
low stalks of the buckwheat and pea help to loosen
the soil.
Although green crops are of great benefit, and
require but little labor, they do require, as usually
managed, that the use of the land and the expense
of seeding and cultivation be entirely devoted to the
advantage of future crops.
Yery nearly the same benefit, especially in the
case of clover, would result from the roots alone
of a crop which has been cut for hay and again for
seed. This at least is the opinion of many who have
had much experience, and who believe that, by the
decomposition of the roots only of a heavy crop
MANURES. 127
of clover, the soil may be brought to the highest
state of fertility of which it is capable. The crop-
ping of the plant causes an increased growth of
the roots, and these, when ploughed np, and allowed
to decompose in the soil, constitute an excellent
manure, acting both chemically and mechanically,
and permanently increasing the value of the land.
If the system of cultivation adopted on the farm
does not admit of the use of green crops, its condi-
tion may be improved, though more expensively
and less completely, by the application of swamp
muck or leaf mould, and by the use of the subsoil
plough, to loosen the lower soil. Except, however, in
these comparatively rare cases, where all the land is
needed for use every year, and where extensive
manuring is adopted, the liberal use of green crops
is always to be recommended.
Before closing this chapter, it may be well to re-
mark that there are various other fertilizers, such as
the a/inmoniacal liquor of gas-Jiouses^ soapers^ wastes,
'bleachers' lye, lees of old oil-cashs, etc, which we
have not space to consider at length, but which are
all valuable as additions to the compost heap, or as
applications, in a liquid form, to the soil.
In many cases (when heavy manuring is prac-
tised) it may be well to apply organic manures to
the soil in a green state, turn them under, and allow
them to undergo decomposition in the ground. The
advantages of this system are, that the heat result-
ing from the chemical changes, will hasten the
growth of plants by making the soil warmer ; the
128 MAKUEES.
carbonic acid formed will have a beneficial chemical
action in the soil, and will be directly presented to
the roots instead of escaping into the atmosphere ;
and if the soil be heavy, the decomposing matters
will tend to loosen it, and leave it more porous. As
a general rule, however, in ordinary farming, where
the amount of manure applied is only sufficient for
the supply of food to the crop, it is undoubtedly bet-
ter to have it previously decomposed, — cooked as it
were, for the nses of the plants, — as they can then
obtain the required amount of nutriment as fast as
need-ed.
ABSORPTION OF MOISTURE.
It is often convenient to know the relative power
of different manures to absorb moisture from the at-
mosphere, especially when we wish to manure lands
that suffer from drought. The following results are
given by C. W. Johnson, in his essay on salt (pp. 8
and 19). In these experiments the animal manures
were employed without any admixture of straw.
PARTS.
1000 parts of horse-dung, dried in a tempera-
ture of 100°, absorbed by expo-
sure for three hours to air saturated
with moisture, of the temperature of
62° 145
1000 parts of cow-dung, under the same cir-
cumstances, absorbed 130
1000 parts pig-dung 120
1000 " sheep " 81
MAITUBES. 129
PAETS.
1000 parts pigeon-dung 50
1000 '' rich alluvial soil 14
1000 " fresh tanner's bark 115
1000 " putrefied " 145
1000 " refuse marine salt sold as manure. . 49^
1000 " soot 36
1000 " burnt clay 29
1000 " coal-ashes 14
1000 " lime 11
1000 " sediment from salt-pans 10
1000 " crushed rock salt 10
1000 " gypsum 9
1000 " salt 4
Muck is a most excellent absorbent of moisture,
when thoroughly decomposed.
DISTRIBUTION OF MANURES.
The following table, from Johnson on Manures,
will be found convenient in the distribution of ma-
nures.
By its assistance the farmer will know how
many loads of manure he requires, dividing each
load into a stated number of heaps, and placing
them at certain distances. In this manner manure
may be applied evenly, and calculation may be made
as to the amount, per acre, which a certain quantity
will supply.
6*
130
MANURES.
DISTANCE
OF
THE HEAPS.
3 yards. .
3^ do. . .
4 do. . .
4^L do. . .
5 do. . .
5^ do. . .
6 do. . .
6^ do. . .
7 do. . .
7,L do. . .
8 do. . .
8^ do. . .
9 do. . .
9i do. . .
10 do. . .
NUMBER OF HEAPS IN A LOAD.
538
395
303
239
194
160
131
115
99
86
75i
67
60
53i
48i
168
151
120
97
80
67
57i
49i
43
37f
33i
30
26f
24i
179
132
101
79i
53i
44f
38i
33
28f
25i
22i
20
18
m
134 1108
99 79
75i' 60i
60 I 47f
48i| 38f
40 32
33i
281
24f
21i
19
161
15
13i
12
27
23
19f
m
15f
13i
12
lOf
9f
50i
39f
32i
26
22i
19
16i
14i
12^
Hi
10
9
77
56i
43i
34i
27f
2.2f
19i
14
12i
lOf
9i
8i
7f
7
8 9 10
67
49i
37f
30
24i
20
16f
14i
12i
lOf
9i
8i
7f
61
6
60
44
33i
26i
21i
17f
15
12f
11
9i
8^
7i
6f
6
54
39i
30i
24
19i
16
13i
10
8^
7i
6f
6
5i
4f
Example 1. — Required the number of loads necessary to ma-
nure an acre of ground, dividing- eacli load into six heaps, and
placing them at a distance of 4 J yards from each other. The an-
swer by the table is 39f .
Example 2. — A farmer has a field containing- 5^ acres, over
which he wishes to spread 82 loads of dung. Now 82 divided by
5^^, gives 15 loads per acre ; and by referring to the table, it will
be seen that the desired object may be accomplished by making
4 heaps of a load, and placing them 9 yards apart, or by 9 heaps
at 6 yards, as may be thought advisable.
CHAPTEK YIII.
MINERAL MANURES
The second class of manures named in tlie general
division of the subject, in the early part of this
section, comprises those of a mineral character.
MANURES. 13.1
These manures have four modes of action when
applied to the soil.
1st. They furnish food for the mineral part of
plants.
2d. They prepare matters already in the soil for
assimilation by roots.
3d. They improve the mechanical condition of the
soil.
4th. They absorb ammonia.
Some of the mineral manures produce in the soil
only one of these effects, and others are efficient in
two or more of them.
The principles to be considered in the use of
mineral manures are essentially given in the first
two sections of this book. It may be well, however,
to repeat them briefly in this connection, and to give
the reasons why any of these manures are needed, —
from which we may learn what rules are to be ob-
served in their application.
1st. Those which are used as food by plants. It
will be recollected that the ash left after burning
plants, and which formed a part of their structures,
has a certain chemical composition ; that is, it con-
sists of alkalies, acids, and neutrals. It was also
stated that the ashes of plants of the same kind are
always of about the same composition, while the
ashes of different kinds of plants may vary niate-
rially. Different parts of the same plant too, as we
learned, are supplied with different kinds of ash.
For instance, clover, on being burned, leaves an
ash containing Urns, as one of its principal ingre-
132 MANUKES.
dients, while the ash of potatoes contains more of
potash than of anything else.
In the second section, (on soils,) we learned that
some soils contain everything necessary to make the
ashes of all plants, and in sufficient quantity to sup-
ply what is required, while other soils are either
entirely deficient in one or more ingredients, or con-
tain so little of them in an available condition, that
they are unfertile for certain plants."^
The different requirements of different plants is
the foundation of the theory of sj^ecial manuring y
* In all cases in whicli tlie constituents of tlie soil are spoken of
in this book, it should be understood as applying- not so much to
its absolute chemical composition as to the availability of its
plant-feeding parts. An atom of potash may be locked up ia the
inside of a pebble, and be of no more use to the roots of a plant
than if it were a hundred miles away, yet a careful chemical
analysis would destroy the pebble and weigh its atom of potash.
The food of plants in the soil must exist iu what Lie big calls " a
state of physical combination," that is, coatiag the outside of its
particles ; attached to them by a feeble attraction which is suffi-
cient to prevent their beiag washed away by the water of raius,
but which yields to the feeding action of roots. It is his belief,
and the opinion seems well founded, that it is only, or chiefly
from materials so placed, that plants derive their food ; and that
the constituents of the soil, before they are taken up by roots,
must be separated from their firmer relations and exposed on
the surfaces of particles, as above stated.
In like manner those elements of manures which are taken up
by the plant are first dissolved ia water, from which they are ab-
sorbed by the particles of the soU, — spread over its interior sur-
faces, exposed to the action of roots.
Even the ammonia brought from the atmosphere in falling rain,
attaches itself in the same way to the interior surfaces of the
soil,
MAITIJEES. 133
whicli is that on a soil of tolerable fertility we can
grow large crops of any particular plant by using
such manures as are chiefly required for its ashes, as
phosphoric acid for a crop of wheat, for instance,
or potash for potatoes or tobacco.
As a universal rule, it may be stated that to ren-
der a soil fertile for any particular plant, we must
supply it (unless it already contains them) with those
matters which are necessary to make the ash of that
plant ; and, if we would render it capable of pro-
ducing all kinds of plants, it must be furnished with
the materials required in the formation of all hinds
of vegetable ashes.
To carry out this system, however, with much
nicety or certainty, would require a more thorough
knowledge of the composition of the soil and of the
feeding of plants than we yet possess. The only
safe rule is, by the use of manures and of thorough cul-
tivation, to make the soil fertile for all crops ; and
then to keep it fertile by the return of all mineral
matters removed in its produce.
A long acquaintance with any field will show
its strong and its weak points, and the greatest skill
of the farmer should be applied to strengthening its
weaker ones and preventing its stronger ones from
becoming weaker. In this way the soil may be raised
to its highest state of fertility, and be fully maintained
in its productive powers.
2d. Those manures which render available the
matters already contained in the soil.
Silicic acid, (or sand,) it will be recollected, exists
134: MANTTEES.
in all soils ; but, in its pure state, is not capable of
being dissolved, and therefore cannot be used by
plants. The alkalies (as has been stated) have the
power of combining with it, making compounds, which
are called silicates. These are readily dissolved by
water, and are available in vegetable growth. I^ow,
if a soil is deficient in these soluble silicates, it is well
known that grain, etc., grown on it, not being able
to obtain the material which gives them strength,
will fall down or lodge; but, if such measures
be taken as will render the sand soluble, the other
conditions of fertility being present, the straw will be
strong and healthy. Alkalies used for this purpose,
come under the head of those manures which de-
velop the natural resources of the soil.
Again, much of the mineral matter in the soil is
combined within particles, and is therefore out of the
reach of roots. Lime, among other things, has the
eifect of causing these particles to crumble and ex-
pose their constituents to the demand of roots. There-
fore, lime has for one of its offices the development
of the fertilizing ingredients of the soil.
3d. Those manures which improve the mechanical
condition of the soil.
The alkalies, in combining with sand, commence
their action on the surfaces of the particles, and
roughen them — rust them, as it were. This roughen-
ing of particles of some soils prevents them from
moving among each other as easily as they do when
they are smooth, and thus keeps the ground from being
compacted by heavy rains, as it is liable to be in its
MAI^HRES. 135
natural condition. In this way, the mechanical tex-
ture of the soil is improved.
It has just been said that Z^'m^ causes the pulveriza-
tion of the particles of the soil ; and thus, by making
it finer, it improves its mechanical condition.
Some mineral manures, such as plaster and salt,
have the power of absorbing moisture from the at-
mosphere ; and this is a mechanical improvement to
dry soils.
4th. Those mineral manures which have the
power of absorbing ammonia.
Plaster^ chloride of lime^ cilumina iclay)^ etc., are
large absorbents of ammonia, whether arising from
the fermentation of animal manures or washed down
from the atmosphere by rains.
Having now explained the reasons why mineral
manures are necessary, and the manner in which
they produce their effects, we will proceed to examine
the various deficiencies of soils and the character of
various kinds of this class of fertilizers.
CHAPTEE IX.
MEANS OF EESTOEATION, ETC
As will be seen by referring to the analyses of soils
on p. 63, they may be deficient in certain ingre-
dients, which it is the object of mineral manures to
supply. These we will take up in order, and endea-
136 MANURES.
vor to show in a simple manner the best means of
managing them in practical farming.
ALK ALIE S .
POTASH. ^
Potash is often deficient in the soil. Its de-
ficiency may have been caused in two ways. Either
it may not have existed largely in the rock from
which the soil was formed,- and consequently is
equally absent from the soil itself, or it may have
once been present in sufiicient quantities, and been
carried away in crops, without being returned to the
soil in the form of manure, until too little remains in
an available form for the requirements of fertility.
In either case the deficiency must be made up ; it
may be supplied by the farmer in various ways.
Potash, as well as all the other mineral manures, is
contained in the excrements of animals, but not (as
is also the case with the others) in sufiicient quantities
to restore the proper balance to soils where it is
largely deficient, nor even to make up for what is
yearly removed with each crop, unless that crop (or
its equivalent) has been fed to such animals as
return all of the fertilizing constituents of their food
in the form of manure, and this to be all carefully
preserved and applied to the soil. In all other cases,
it is necessary to apply more potash than is contain-
ed in the excrements of the animals of the farm.
Wood ashes is generally the most available source
MAKTIRES. 13T
from which to obtain this alkali. The ashes of all
kinds of wood contain potash (more or less, according
to the kind — see analyses, Section Y.) If the ashes
are leached^ much of the potash is removed; and
hence, for the purpose of supplying it, they are less
valuable than unleached ashes. The latter may be
made into compost with muck, as directed in a pre-
vious chapter, or applied directly to the soil. In
either case the potash is available directly to the
plant, or is capable of uniting with the silica in the
soil to form silicate of potash. Leached ashes con-
tain too little potash to be valuable in the compost,
but, from their imperfect leaching, they do contain
enough to make them valuable as manure. J^either
potash nor any other alkali should ever be applied to
animal manures unless in compost with an absorbent,
as they cause the ammonia to be thrown off and lost.
Potash sparlings^ or the refuse- of potash ware-
houses, is an excellent manure for lands deficient in
this constituent.
Feldspar^ haolin^ and other minerals containing
potash, are, in some localities, to be obtained in suf-
ficient quantities to be used for manurial purposes.
Within a comparatively few years, a new fer-
tilizer— of great value to all regions within carrying
distance of its place of deposit — has been brought
to the notice of farmers near the seaboard. This is
the Green Sand Marl of ^JsTew Jersey, which under-
lies a wide belt extending from the Atlantic Ocean to
the Delaware River, having an area of about 900
square miles. It is very largely used in South Jersey,
133 MAmjRES.
where it has given great value to land that was pre-
viously not fit for cultivation. Quite recently, com-
panies have been formed for its shipment to other
places near the coast, and it promises to become
of great importance wherever it can be cheaply
procured.
An analysis of this manure is given in Section Y
SODA.
Soda^ the requirement of which is occasioned by
the same causes as create a deficiency of potash,
and all of the other ingredients of vegetable ashes,
may be very readily supplied by the use of common
salt (chloride of sodimn), which is about one-half
sodium (the base of soda). The best way to use
salt is in the lime and salt mixture, previously
described, or as a direct application to the soil. If
too much salt be given to the soil it will kill any
plant. In small quantities, however, it is highly bene-
ficial, and if six iushels per acre be sown broadcast
over the land, to be carried in by rains and dews, it
will not only destroy many insects (grubs and worms),
but will prove an excellent manure. Salt acts direct-
ly in the nutrition of plants, as a source of necessary
chlorine and soda. There is little doubt, however,
that its chief value as a manure in most instances arises
from the fact that it renders other plant foods more
soluble, and assists in pre23armg them for use. Salt,
even in quantities large enough to denude the soil of
all vegetation, is uqyqy jpermanently injurious. After
MAOTJRES. 139
a time it seems to have tlie effect of increasing
fertility. One peck of salt in each cord of compost
will not only hasten the decomposition of the ma-
nures, but will kill seeds and all grubs — a very desira-
ble effect. While small quantities of salt in a com-
post heap are beneficial, too much (as when applied
to the soil) is positively injurious, as it arrests de-
composition, fairly J?^c&5 the manures, and prevents
them from rotting.
For asj>aragus, which is a marine plant, salt is an
excellent manure, and may be applied in almost un-
limited quantities, while the ^plants are growing ; if
used after they have gone to top, it is injurious.
Salt has been applied to asparagus beds in such
quantities as to completely cover them, and with
apparent benefit to the plants. Of course large doses
of salt kill all weeds, and thus save labor, and avoid
the injury to the asparagus buds which would result
from their removal by hoeing. Salt may be used
advantageously in any of the foregoing manners, but
should always be applied with care. For ordinary
farm purposes, it is undoubtedly most profitable to
use the salt with lime, and make it perform the
double duty of assisting in the decomposition of
vegetable matter, and fertilizing the soil.
Soda unites with the silica in the soil, and forms
the valuable silicate of soda.
Nitrate of soda ^ or cubical nitre, which is found in
South America, is composed of soda and nitric acid.
It furnishes both soda and nitrogen to plants, and is
an excellent manure.
140 MAJSrUBES.
LIME.
The subject of lime is one of most vital impor-
tance to the farmer ; indeed, so varied are its modes
of action and its effects, that some writers have given
it credit for everything good in the way of farming,
and have gone so far as to say that all permanent
improvement of agriculture must depend on the use
of lime. Although this is far in excess of the truth
(as lime cannot plough, nor drain, nor supply anything
but lime to the soil), its many beneficial eflects de-
mand for it the closest attention.
As food for plants, lime is of considerable impor-
tance. All plants contain it — some of them in
large quantities. It is an important constituent of
straw, meadow hay, leaves of fruit-trees, peas, beans,
and turnips. It constitutes more than one-third of
the ash of red clover. Most soils contain lime
enough for the use of plants ; in others it is deficient,
and must be supplied artificially before they can pro-
duce good crops of those plants of which lime is an
important ingredient. The amount required for the
mere feeding of plants is not large (much less than one
per cent.), but lime is often necessary for other pur-
poses ; and setting aside, for the present, its feeding
action, we will examine its various efi*ects on the
mechanical and chemical condition of the soil.
1. It corrects acidity (sourness).
2. It hastens the decomposition of the organic
matter in the soil.
3. It causes tlie mineral particles of the soil to
crumble.
4. By producing the above effects, it prepares the
constituents of the soil for assimilation by plants.
5. It is said to exhaust the soil ; but as it does so
through its beneficial action in producing larger
crops, and only in this way, it is only necessary to
return to the soil the other earthy ingredients that
the larger crops remove from it.
1. The decomposition of organic matter in the soil,
especially if too wet, often produces acids which
make the land sour^ and cause it to produce sorrel
and other weeds, and which interfere with the
healthy growth of crops. Lime is an alkali, and if
applied to soils suffering from sourness, it will unite
with the acids, and neutralize them, so that they will
no longer be injurious.
2. We have before stated that lime is a decompo-
sing agent, and hastens the rotting of muck and
other organic matter. It has the same effect on the
organic parts of the soil, and causes them to be re-
solved into the gases and minerals of which they are
formed. It has this effect, especially, on organic
matters containing nitrogen, causing them to pro-
duce ammonia; consequently, it liberates this gas
from the animal manures in the soil.
3. Yarious earthy compounds in the soil are so
affected by Hme that they lose their power of holding
together, and crumble, or are reduced to finer par-
ticles, while some of their constituents are ren-
dered soluble. This crumbling effect improves the
142 MANUKES.
mechanical as well as the chemical condition of the
soil.
4. We are now enabled to see how lime prepares
the constituents of the soil for the use of plants.
By its action on the roots, buried stubble, and other
organic matter in the soil, it causes them to be decom-
posed, and to give up their constituents for the use
of roots. In this manner the organic matter is
prepared for use more rapidly than it would be, if
there were no lime present to hasten its decomposi-
tion.
By the decomposing action of lime on the mineral
parts of the soil (3), they also are placed more rapidly
in a useful condition than would be the case, if their
preparation depended on the slow action of atmo-
spheric influences.
Thus we see that lime, aside from its use directly
as food for plants, exerts a beneficial influence on
both the organic and inorganic parts of the soil.
5. Many farmers assert that lime exhausts the soil.
If we examine the manner in which it does so, we
shall see that this is no argument against its use.
It exhausts the organic parts of the soil by decom-
posing them, and resolving them into the gases and
minerals of which they are composed. The gases
arising from the organic matter cannot escape ; be-
cause there is in all arable soils a sufficient amount
of clay and carbonaceous matter present to cause
these gases to be retained until required by the roots
of plants. Hence, although the organic matter of
manure and vegetable substances may be altered in
MANURES. 143
form by the use of lime, it can escape (except in
very poor soils) only as it is taken up by roots to feed
the crop, and such exhaustion is certainly profitable?
and, so far as the organic parts are concerned, the
fertility of the soil will be fully maintained by the
decomposition of new roots and of organic manures.
The only way in which lime can exhaust the earthy
parts of the soil is, by alteringtheir condition, so that
plants can use them more readily. That is, it exposes
it to the action of roots. We have seen that fertili-
zing matter cannot be leached out of a good soil, in
any material quantity, nor can it be carried down to
any considerable depth. Hence, there can be no
loss m this direction; and, as mineral matter
cannot evaporate from the soil, the only way
in which it can escape is through the structure of
plants.
If lime is applied to the soil, and increases the
amount of crops grown by preparing for use a larger
supply of earthy matter, of course, the removal of
earthy substances from the soil will be more rapid
than when only a small crop is grown, and the soil
will be sooner exhausted,— not by the lime, but by
the plants. In order to make up for this exhaustion
it i& necessary that a sufficient amount of inorganic
matter be supplied to compensate for the increased
quantity taken away by plants.
Thus we see that it is hardly fair to accuse the
lime of exhausting the soil, when it only improves its
character, and increases the yield. It is the crop
that takes away the fertility of the soil (the same as
144: MANTJKES.
would be the case if no lime were used, only faster,
because the crop is larger), and in all judicious culti-
vation this loss will be fully compensated by the
application of manures, thereby preventing the ex-
haustion of the soil.
Kind of lime to he used. The first consideration
in procuring lime for manuring land, is to select that
which contains but little, if any, magnesia. JS'early
all stone lime contains more or less of this, but some
kinds contain more than others. When magnesia
is applied to the soil in too large quantities, it is
positively injurious to plants, and care is necessary
in making selection. As a general rule, it may be
stated, that the best plastering lime makes the best
manure. Such kinds only should be used as are
known from experiment not to be injurious.
Shell lime is undoubtedly the best of all, for it
contains no magnesia, and it does contain a small
quantity of phosphate of lime. In the vicinity of
the sea-coast, and near the lines of railroads, oyster
shells, clam shells, etc., can be cheaply procured.
These may be prepared for use in the same manner
as stone lime.
The preparation of the lime is done by first burn-
ing and then slaking, or by putting it directly on
the land, in an unslaked condition, after its having
been burned. Shells are sometimes ground^ and
used without burning; this is hardly advisable, as
they cannot be made so fine as by burning and sla-
king. As was stated in the first section of this book,
lime usually exists in nature, in the form of carbo-
MANURES. 145
nate of lime, as limestone, chalk, or marble (being
lime and carbonic acid combined), and when this is
burned the carbonic acid is thrown off, leaving the
lime in a ptire or caustic form. This is called burn-
ed lime, quick-lime, lime-shells, hot lime, etc. If
the proper quantity of water be poured on it, it is
immediately taken up by the lime, which falls into
a dry powder, called slaked lime. If quick-lime were
left exposed to the weather it would absorb moisture
from the atmosphere, and become what is termed
air-slaked.
When slaked lime (consisting of lime and water)
is exposed to the atmosphere, it absorbs carbonic acid)
and becomes carbonate of lime again ; but it is now
in the form of a very fine powder, and is much more
useful than when in the stone, or even when finely
ground.
If quick-lime is applied directly to the soil, it
absorbs first moisture, and then carbonic acid, becom-
ing finally a powdered carbonate of lime.
One ton of carbonate of lime contains 11:|- cwt.
of lime ; the remainder is carbonic acid. One ton
qf slaked lime contains about 15 cwt. of lime ; the
remainder is water.
Hence we see that lime should be burned, and not
slaked, before being transported, as it would be un-
profitable to transport the large quantity of carbonic
acid and water contained in carbonate of lime and
slaked lime. The quick-lime may be slaked and
carbonated after reaching its destination, either be-
fore or after being applied to the land.
7
146 MANUKES.
As has been before stated, nmch is gained by sla-
king lime with salt water. Indeed, in many cases it
will be found profitable to use all lime in this way.
Where a direct action on the inorganic matters
contained in the soil is desired, it may be well to ap-
ply the lime directly in the form of quick-lime ; but,
where the decomposition of the vegetable and animal
constituents of the soil is desired, the correction of
sourness, or the supplying of lime to the crop, the
mixture with salt would be advisable.
The amount of lime required hy jplants is, as was
before observed, usually small compared with the
whole amount contained in the soil ; still it is not un-
important.
25 bus. of wheat contain about
25
u
barley
25
a
oats
2
tons of turnips
2
<c
potatoes
2
u
red clover
2
^«
red grass
OF LIME.
13
lbs.
lOi
a
11
u
12
u
5
a
77
u
30
u *
The amount of lime required at each application,
and the frequency of those aj)plications, must depend
on the chemical and mechanical condition of the soil.
No exact rule can be given, but probably the custom
of each district — regulated by long experience — is
the best guide.
Lime sinks in the soil; and therefore, when
* The straw producing the grain, and tlie turnip and potato
tops, contain more lime than the grain and roots.
MANURES. 147
used alone, should always be applied as a top dressing
to be carried into the soil by rains. The tendency of
lime to settle is so great that, when cutting drains,
it may often be observed in a whitish streak on the
top of the subsoil. After heavy doses of lime have
been given to the soil, and have settled so as to have
apparently ceased from their action, they may be
brought up and mixed with the soil by deeper plowing.
Lime should never he mixed with animal manures,
unless in compost with muck or some other good
absorbent, as it causes the escape of their ammonia.
PLASTER OF PARIS.
Plaster of Paris or Gypsum (sulphate of lime)
is composed of sulphuric acid and lime in combina-
tion.
It is a constituent of many plants. It also fur-
nishes them with sulphuric acid, and with the sulphur
of which a small quantity is contained in seeds, etc.
It is an excellent absorbent of ammonia, and is
very useful to sprinkle in stables, poultry houses,
pig-styes, and privies, wdiere it absorbs the escap-
ing gases, saving them for the use of plants, and
purifying the air — rendering stables, etc., more
healthy than when not so supplied.
CHLORIDE OF LIME.
Chloride of lime contains lime and chlorine. It
furnishes both of these constituents to plants, and is
148 MANURES.
an excellent absorbent of ammonia and other gases
arising from decomposition — ^hence its usefulness in
destroying bad odors, and in preserving fertilizing
matters for the use of crops.
It may be used like plaster, or in the decomposi-
tion of organic matters, where it not only hastens
decay, but absorbs and retains the escaping gases.
Lime in combination with phosphoric acid forms
the Ydlvi?^\Q phosphate oflime^ of which so large a
portion of the "ash of grain, and the bones of animals,
is formed. This will be spoken of more at length
under the head of " phosphoric acid."
MAGNESIA.
Magnesia is a constituent of vegetable ashes, and
is almost always present in the soil in sufficient
quantities.
ACIDS.
8IJLPHTJKIC ACID.
Sulphuric acid is a very important constituent
of veo:etable ashes. It is sometimes deficient in the
soil, particularly where potatoes have been long culti-
vated. One of the reasons whj plaster (sulphate of
lim§) is so beneficial to the potato crop is probably
that it supplies it with sulpTiuric acid.
Sulphuric acid is commonly known by the name
of all vitriol, and may be purchased for agricultural
purposes at a low price. It may be added in a very
MANURES. 14:9
dilute form (weakened by mixing it with a large
quantity of water) to the compost heap, where it will
change the ammonia to a sulphate as soon as formed,
and thus prevent its loss, as the sulphate of ammonia
is not volatile ; and, being soluble in water, is useful
to plants. Some idea of the value of this compound
may be formed from the fact that manufacturers of
manures pay a high price for sulphate of ammonia,
to insure the success of their fertilizers. Notwith-
standing this, many farmers persist in throwing away
hundreds of pounds of ammonia every year, as a tax
for their ignorance (or negligence), while a small tax
in money — not more valuable nor more necessary to
their success — for the support of common schools,
and the better education of the young, is too often
unwillingly paid.
If a tumbler full of sulphuric acid (costing a few
cents) be thrown into the tank of the compost heap
once a month, the benefit to the manure would be
very great.
Care is necessary that too miich sulphuric acid be
not used, as it would prevent the proper decomposi-
tion of the manure.
In many instances it will be found profitable to
use sulphuric acid in the manufacture of super-
phosphate of lime (as directed under the head of
"phosphoric acid"), thus making it perform the
double purpose of preparing an available form of
phosphate, and of supplying sulphur and sulphuric
acid to the plant.
150 MANURES.
PHOSPHORIC ACID.
We come now to the consideration of one of the
most important of all subjects connected with agri-
culture.
Phosphoric acid^ which forms about one-half of
the ashes of wheat, rye, corn, buck- wheat, and oats ;
nearly the same proportion of those of barley, peas,
beans, and linseed ; an important part of the ashes
of potatoes and turnips ; one-quarter of the ash
of milk, and a very large proportion of the bones of
animals, often exists in the soil in the proportion of
only about one or two pounds in a thousand, and
but a very small part even of this amount is in a con-
dition to be taken up by roots. The cultivation of
our whole country has been such, as to take away
the phosphoric acid from the soil without returning
it, except in very minute quantities. Every hundred
bushels of wheat sold contains (and removes perma-
nently from the soil) about sixty pounds of phospho-
ric acid. Other grains, as well as the root crops and
grasses, remove, likewise, a large quantity of it. It
has been said by a contemporary writer, that for each
cow kept on a pasture through the summer, there is
carried off in veal, butter, and cheese, not less than
fifty lbs. of phosphate of lime (bone-earth) on an
average. This would be one thousand lbs. for twenty
cows ; and it shows clearly why old dairy pastures
become so exhausted of this substance, that they will
often no longer produce those nutritious grasses
which are favorable to butter and cheese making.
MAI^UEES. 151
That this removal of one of the most valuable con-
stituents of the soil has been the cause of more ex-
haustion of farms, and more emigration, in search
of fertile districts, than any other single effect of
injudicious farming, is a fact which multiplied in-
stances most clearly prove.
It is stated that the Genesee and Mohawk valleys,
which once produced an average of thirty -five or
forty hushels of wheat per acre, have since been
reduced, in their average production, less than twen-
ty bushels. Hundreds of similar cases might be
stated ; and in a large majority of these, could the
cause of the impoverishment be ascertained, it would
be found to be the removal of the phosphoric acid
from the soil.
The evident tendency of cultivation being to con-
tinue this ruinous system, and to prey upon the vital
strength of the country, it is necessary to take such
measm-es as will arrest the outflow of this valuable
material. This can never be fully accomplished
until the laws which regulate the nutrition of plants
are generally understood and appreciated by the
people at large. The enormous waste of the most
valuable manures, taking place not only in every
city, but about every residence in the laild, can only
be arrested when the importance of restoring to the
soil a full equivalent for what is taken from it is
universally realized. China and Japan, the most
densely peopled countries in the world, have been
cultivated for thousands of years with no diminution
of their fertility. Japan is about as large and about
152 MAKURE8.
as densely peopled as Great Britain, yet while Great
Britain imports immense quantities of grain, guano,
bones, and other fertilizers, and pours its immense
volumes of manure into the sea, Japan neither
wastes nor imports. The bread of its people is raised
on its fields, which have been cultivated for un-
counted ages, while every scrap of fertilizing matter
is saved with scrupulous care.
It is true that the processes by which manure is
saved and applied in China and Japan are not nice,
but it is saved, nevertheless, and the fact that our
chemical knowledge enables us to accomplish the
same result in an inoffensive manner, should make
us all the more earnest in mending our ways.
Many suppose tliat soils which produce good crops,
year after year, are inexhaustible, but time invariably
proves the contrary. They may possess a suffi-
ciently large stock of phosphoric acid, and other plant
constituents, to last a long time, but when that stock
becomes so reduced that there is not enough left for
the uses of full crops, the productive power of the
soil will yearly decrease, until it becomes worthless.
It may last a long time — a century, or even more —
but as long as the system is to remote everything^
and return nothing ^ the fate of the most fertile soil
is certain.
As has been stated already, the constituent of the
soil which is most likely to become deficient i^ phos-
phoric acid. One principal source from which this
can be obtained is foimd in the bones of animals.
These contain a large proportion of phosphate of
MANUKES. 153
lime. They are the receptacles which collect nearly
all of the phosphates in crops which are fed to ani-
mals, and are not returned in their excrements. For
the grain, etc., sent out of the country, there is no
way to be repaid except by the importation of this
material ; but nearly all that is fed to animals may,
if a proper use be made of their excrement, and of
their bones after death, be returned to the soil. "With
the treatment of animal excrements we are already
familiar, and we will now turn our attention to the
subject of
BONES.
Bones consist, when dried, of about one-third or-
ganic matter, and two-thirds earthj matter.
The organic matter consists chiefly of gelatine — a
compound containing nitrogen.
The earthy part is chiefly jphosjp^hate of lime.
Hence we see that bones are excellent, both as or-
ganic and as mineral manure. The organic part, con-
taining nitrogen, forms amm^onia^ and the inorganic
part supplies the much-needed phosphoric acid to the
soil.
Liebig says that, as a producer of ammonia, 100
lbs. of dry bones are equivalent to 250 lbs. of human
urine.
. Bones are applied to the soil in almost every con-
ceivable form. Whole hones are often used in very
large quantities ; their action, however, is extremely
slow, and it is never advisable to use them in this
form.
154 MANURES.
Ten bushels of bones, finely ground, will produce
larger results, during the ten years after application,
than would one hundred bushels merely broken ; not
because the dust contains more fertilizing matter than
the whole bones, but because that which it does con-
tain is in a much more available condition. It fer-
ments readily, and produces ammonia, while the
ashy parts are exposed to the action of roots.
It is a rule which is applicable to all manures, that
the more finely they are pulverized or divided, the
more valuable they become. Not only do they ex-
pose much more surface to the feeding action of
roots, but from their fine division they can be much
more evenly distributed through the soil. If it is
true, as seems probable, that the absorptive power
of fertile soils is so strong as to prevent dissolved
plant food from being carried beyond the point with
which it first comes in contact, until the soil about
that point has taken up all that it is capable of hold-
ing, then the more widely we spread a manure before
it is dissolved, the more uniformly rich will be the
soil. By sowing coarsely crushed bones, we fertilize
the soil in spots. By crushing each lump we not
only make all of its constituents immediately availa-
ble, but we make it reach every part of the surface
between the spots above referred to. Even Peruvian
guano, soluble as it is in water, is much more effec-
tive when finely ground before being spread upon
the land.
Bone-hlack. If bones are burned in retorts, or
otherwise protected from the atmosphere, their or-
MANURES. 155
ganic matter will all be driven off except the carbon,
which not being supplied with oxygen cannot escape.
In this form bones are "called wory hlack^ or hone
hlack ; and they contain all of the earthy matter
and carbon of the bones. The nitrogen having been
expelled, it can make no ammonia ; and thus far the
original value of bones is reduced by burning — that
is, a ton of bones contains more fertilizing matter
before, than after, burning. This means of pulveriz-
ing bones is not to be recommended for the use of
farmers, who should not lose the ammonia forming a
part of bones, more than that of other manure.
Composting hones with ashes is a good means of
securing their decomposition. They should be placed
in a water-tight vessel (such as a cask) ; first, three
or. four inches of bones, then the same quantity of
strong unleached wood ashes, continuing these alter-
nate layers until the cask is full, and keeping them
always wet. If they become too dry they will throw
off an offensive odor, accompanied by the escape of
ammonia, and consequent loss of value. In about
one year, the whole mass of bones (except, perhaps,
those at the top) will be softened, so that they may
be easily crushed, and they are in a good condition
for application to the land. The ashes are, in them-
selves, valuable, and this compost is excellent for
many crops, particularly for Indian corn. A little
dilute sulphm'ic acid, occasionally sprinkled on the
upper part of the matter in the cask, will prevent
the escape of the ammonia.
Boiling hones under jjyressiire^ whereby their gela-
150 MANURES.
tine is dissolved away, and the earthy matter left
in an available condition, from its softness, is a very
good way of rendering them useful ; but it requires
the use of a steam boiler, and other expensive appa-
ratus.
SUPER-PHOSPHATE OF LIME.
Super-phosphate of lime is made by treating phos-
phate of lime, or the ashes of bones, with sulphurio
acid.
Phosphate of lime, as it exists in bones, consists
of one equivalent of phosphoric acid and three equi-
valents of lime.
The word " equivalent " is here used to represent
what in chemistry is known as the combining pro-
portion of each element of a compound body — that
is, one pound of one substance combines with one
and one-half pounds of another, and these propor-
tions are invariable.
In bone earth, or phosphate of lime, one equiva-
lent, or 72 lbs. of phosphoric acid combines with three
equivalents (of 28 lbs. each), or 84 lbs. of lime.
IS'ow, by adding to this compound one equivalent
(or 40 lbs.) of' sulphuric acid, we cause one equiva-
lent (28 lbs.) of the lime to be taken away, leaving
the 72 lbs. of phosphoric acid combined with only
56 lbs. of lime. By using two equivalents of sul-
phuric acid (or 80 lbs.) we cause the removal of
56 lbs. of lime, leaving only 28 lbs. combined with
the 72 lbs. of phosphoric acid. This is super-phos-
phaf e of lime, which is readilj^ soluble in water. It
MAinJRES. , 157
is united with 80 lbs. of snipliuric acid and 56 lbs.
of lime in combination with each other, forming
136 lbs. of sulphate of lime, or plaster-of-paris.
The whole compound contains :
Phosphoric acid 72 lbs.
Sulphm-ic acid 80 "
Lime 84 "
In all. . . , 236 "
— or, ^^^^ per cent, of phosphoric acid.
The phosphoric acid, now in combination with
only one equivalent of lime, is readily dissolved in
water, and will be evenly distributed in the soil ; but
it will take the earliest opportunity to combine with
two more equivalents of lime in the soil, and will
again become insoluble. It may well be asked,
What is the advantage of making it soluble if it is
so soon again to become insoluble ?
The answer to this question is clearly stated in
the following quotation from Prof. S. W. Johnson's
Essays on Manures ; —
" This white cloud is precipitated bone-phosphate
of lime, and does not essentially diifer from the
original bone-phosphate, except that it is inconceiv-
ably finer than can be obtained by any mechanical
means. The particles of the finest bone-dust will
not average smaller than one-hundredth of an inch,
while those of the precipitated phosphate are not
more than one twenty-thousandth of an inch in di-
ameter. Since the particles of the precipitated phos-
phate are so tery much smaller than those of the
158 MAKUEES.
finest bone-dust, we can understand that their action
as a manure would be correspondingly more rapid."
In saying that the phosphate of lime is insoluble,
it is meant that it is insoluble in pure water. Water
which contains either carbonic acid, ammonia, or
common salt (and all soil water contains one or
more of these), has the power of dissolving it, and
making it available to roots. The action is slow,
but it is sufficient, and it is the more rapid the finer
the pulverization of the phosphate. The fine pre-
cipitated phosphate exposes much more surface to
the action of the water, and can consequently be
taken up much more rapidly.
Super-phosphate of lime may be made from whole
bones, bone-dust, bone-black, or from the pure ashes
of bones, or from phosphatic guano.
TTie reason why super-phosphate of lime is letter
than phosphate^ is therefore easily explained. The
phosphate is very slowly soluble in water, and conse-
quently furnishes food to plants slowly. A piece
of bone as large as a pea may lie in the soil for years
without being all consumed ; consequently, it will be
years before its value is returned, and it pays no in-
terest on its cost while lying there. The super-phos-
phate is very rapidly dissolved, and if evenly spread
is diftused by the water of rains throughout the soil, —
coating its absorbent particles with a nutriment held
in a state of physical combination, ready to be
yielded to the action of roots; hence its much
greater value as a manure.
It is true that the phosphate is a more lasting
MAiq^UKES. 159
manure than tlie super-phosphate — in the same way
that gold buried in a pot in the garden is more last-
ing than if used in labor and manure for its cultiva-
tion. I desire, once for all, to caution farmers
against attaching too much imporance to the lasting
qualities of a manure. Generally they are lasting
only in proportion as they are lazy. In manuring,
as in other things, a nimble sixpence is better than a
slow shilling.
Of course it is not to be understood that all ma-
nures used had better exert their full effect on the
first year's crop, but the more rapidly it can be made
available consistently with the course of cultivation
adopted (the rotation, etc.), the less we shall lose in
the item of interest. A hundred pounds of coarsely
ground bones may give an extra crop of 250 lbs. of
hay per year for ten years. The same quantity
finely ground and evenly spread might add a thou-
sand lbs. to the first year's crop, and if the hay is
consumed on the farm, and its constituents returned
in the form of manure, the same increase might be
received year after year. Therefore, in considering
the value of manure, more attention should be given
to the rapidity of its action than to the time that it
will last. Many farmers who have the proper facili-
ties, may find it expedient to purchase bones or
bone-dust and sulphuric acid, and to manufacture
their own super-phosphate of lime ; others will prefer
to purchase the prepared manure. Such purchases
should be made with great care, and only from per-
sons of established reputation, for nothing is easier
160 MANURES.
than the adulteration of this material. It is best,
always, to stipulate that the manure shall contain a
certain percentage of soluble and insoluble phospho-
ric acid, — and to withhold payment until an average
sample of the manure received has been tested by a
competent chemist.
SILICIC ACID.
Silicic acid (or sand) always exists in the soil in
sufficient quantities for the supply of food for plants ;
but not always in the proper condition. This subject
has been so often explained to the reader of this
book, that it is only necessary to repeat here, that
when the weakness of the straw or stalk of plants
grown on any soil indicates an inability in that soil
to supply the silicic acid required for strength, not
more sand should be added, but alkalies^ to combine
with the sand already contained in it, and make
soluble silicates which are available to roots.
Sand is often necessary to stiff clays, as a mechani-
cal manure, to loosen their texture and render them
easier of cultivation, and more favorable to the dis-
tribution of roots, and to the circulation of air and
water, and in this capacity it is often very important.
In my own practice I find it profitable to haul it
three miles to use on heavy clay land.
NEUTE ALS.
CHLORINE.
Chlorine^ a necessary constituent of plants, and
sometimes, though not usually, deficient in the soil,
MAI^URES. 161
may be applied in the form of salt (chloride of so-
dium), or chloride of lime. The former may be dis-
solved in the water nsed to slake lime, and the latter
may, with much advantage, be sprinkled around
stables and other places where fertilizing gases are
escaping, and, after being saturated with ammonia,
applied to the soil, thus serving a double purpose.
On a stock farm, a very good way to return to the
soil the chlorine contained in the produce sold, is to
give it freely to the animals.
OXEDE OF mON.
Probably all soils contain sufficient quantities of
oxide of iron, or iron rust, so that this substance can
hardly be required as a manure.
Some soils, however, contain the ^<9toxide of iron
in such quantities as to be injurious to plants, — see
page 74. When this is the case, it is necessary to
plow the soil thoroughly, and use such other me-
chanical means as shall open it to the admission of
air. The^6>toxide of iron will then take up more
oxygen, and become the^^/'oxide — which is not only
inoffensive, but is conducive to fertility.
OXIDE OF MAKaANESE.
This can hardly be called an essential constituent
of plants, and is never taken into consideration in
manuring lands.
162 MANURES.
VARIOUS OTHER EARTHY MANURES.
LEACHED ASHES.
Among the earthy manures which have not yet
been mentioned, — not coming strictly under any of
the preceding heads, — is the one known as leached
ashes.
These are, of course, much less valuable than ashes
from which the potash has not been leached out ; still,
as potash is generally made, the leaching is not very
complete, and a considerable quantity of this sub-
stance, available to plants, is left in them. In addi-
tion to this, they contain some phosphoric acid and
silicic acid, which add to their value. Practically,
they are held in high esteem in all localities where
they can be obtained at a moderate cost of transport-
ation. Care, however, should be taken, not to pur-
chase ashes which have been made in lime-kilns, as
these generally contain a large quantity of lime,
which is not worth so high a price as the ashes.
OLD MORTAR.
Old mortar is a valuable manure, because it con-
tains not only lime, but compounds of nitric acid
with alkalies, — called nitrates.
These are slowly formed in the mortar by the
changing of the nitrogen of the hair (in the mortar)
and of the ammonia received from the atmosphere
into nitric acid, and the union of this with the
MANURES. 163
lime of the plaster, or with other alkalies which it
may contain in minute quantities.
The lime contained in the mortar may be useful
in the soil for the many purposes accomplished by
other lime, and is generally more valuable than that
fresh from the kiln.
GAS HOUSE LIME, ETC.
The refuse lime of gas works, where it can be
cheaply obtained, may be advantageously used as a
manure. It consists, chiefly, of various compounds
of sulphur and lime. It should be composted with
earth or refuse matter, so as to expose it to the action
of air. It should never be used fresh from the gas
house. In a few months the sulphur will have
united with the oxygen of the air, and become sul-
phuric acid, which unites with the lime and makes
sulphate of lime (plaster,) which form it must as-
sume, before it is of much value. Having been
used to purify gas made from coal, it contains a
small quantity of ammonia, which adds to its value.
It is considered a profitable manure in England, at
the price there paid for it (forty cents a cartload),
and, if of good quality, it may be worth more than
that, especially for soils deficient in sulphuric acid
or lime, or for such crops as are much benefited by
plaster. Its price must, of course, be regulated some-
what by the price of lime, which constitutes a large
proportion of its fertilizing parts. The offensive
odor of this compound renders it a good protection
164 MAiniRES.
against many insects, wlien used in its fresh state :
but in this state it should be very cautiously ap-
plied.
The refuse liquor of gas works contains enough
ammonia to make it a valuable manure. It should
be filtered through earth or muck, which will retain
its valuable parts, and will be enriched by them.
The refuse ley of soap factories and bleaching es-
tablishments contains greater or less quantities of
soluble silicates and alkalies (especially soda and pot-
ash,) and is a good addition to the tank of the com-
post heap, or it may be used directly as a liquid
application to the soil, or, better, filtered as above
described. The soapers' ley, especially, will be found
a good manure for lands on which grain lodges.
Much of the benefit of this manure arises from the
soluble silicates it contains, while its nitrogenous
matter obtained from those parts of the fatty matters
which cannot be converted into soap, and conse-
quently remain in this sohition, forms a valuable
addition. Heaps of soil saturated with this liquid
in autumn, and subjected to the freezings of winter,
form an admirable manure for spring use.
IRRIGATION.
Irrigation^ strictly speaking, should not be con-
sidered under the head of earthy manures alone, as it
MAinJRES. 165
often supplies ammonia and other organic matters to
the soil. Its chief value, however, in most cases,
must depend on the amount of mineral matter which
it furnishes.
The word "irrigation" means simply the act of
watering. In many districts water is in various
ways made to overflow the land, and is removed or
withheld when necessary for the pm^poses of cultiva-
tion. All river and spring water contains some im-
purities, many of which are beneficial to vegetation.
These are derived from the earth over, or through,
which the water has passed. Ammonia also is ab-
sorbed by the water from the atmosphere. When
water is made to cover the earth, especially if its
rapid motion be arrested, much of this fertilizing
matter settles, and is deposited on or absorbed by the
soil. The water which sinks into the soil carries its
impurities to be retained for the uses of plants.
When, by the aid of under-drains, or the open texture
of the land, the water passes through the soil, its im-
purities are arrested, and become available in vege-
table growth. It is, of course, impossible to say
exactly what kind of mineral matter is supplied by
the water of irrigation, as that depends on the kind
of rock or soil from which the impurities are derived ;
but, whatever it may be, it is generally soluble and
ready for immediate use by plants, and is distributed
in the most uniform manner possible.
Water which has run over the surface of the earth
contains both ammonia and mineral matter, while
that which has arisen out of the earth, contains
166 MANUBES.
usually only mineral matter. The direct effect of
the water of irrigation as a solvent and distributer
of the mineral ingredients of the soil, constitutes one
of its main benefits.
To describe the many modes of irrigation would
be too long a task for our limited space. It may be
applied in any way in which it is possible to cover
the land with water, at stated times. Care is neces-
sary, however, that it does not wash more fertilizing
matter away from the soil than it deposits upon it, as
would often be the case, if a strong current of water
were run over it. Brooks may be dammed up, and
thus made to cover a large quantity of land. In
such a case the rapid current would be destroye(l,
and the fertilizing matter would settle ; but, if the
course of the brook were turned, so that it would run
in a current over any part of the soil, it might carry
away more than it deposited, and thus prove injuri-
ous. Small streams turned on to land, from the
washing of roads, or from elevated springs, are good
means of irrigation, and produce increased fertility,
except where the soil is of such a character as to pre-
vent the water from passing away, in which case it
must first be under-drained.
Irrigation was one of the oldest sources of fertility
used by man, and still continues in great favor wher-
ever its effects have been witnessed. In England
and Scotland, much attention is now being paid to
the question of liquid manure irrigation, and an at-
tempt is being made to employ the vast discharges
of the London sewers. For this purpose it is in con-
MAi!f[JRES. 167
templation to build an aqueduct forty miles long and
nine feet in diameter for its distribution. In the
experiments made with this manure during the sum-
mer of 1867, fifty-three tons of Italian rye-grass were
grown on a single acre, nine tons being grown in
twenty-two days.
On the farm of the celebrated Mr. Mechi at Tip-
tree Hall, the system was, many years ago, adopted
of converting all the manure of the stables into a
liquid, and distributing it over the farm by means of
uuder-ground pipes and movable hose. Mr. Mechi
still continues the practice and considers it profit-
able.
This subject is mentioned in this connection, not
as affording an example which can be profitably fol-
lowed here, so much as because it shows how much
expense may be profitably applied to the distribution
of manm-e in a liquid form.
MIXING SOILS.
The mixing of soils is often all that is necessary
to render them fertile, and to improve their mechan-
ical condition. For instance, soils deficient in pot-
ash, or any other constituent, may have that deficiency
supplied, by mixing with them soil containing this
constituent in excess.
It is very frequently the case, that such means of
improvement are easily availed of. While these
chemical effects are being produced, there may be an
equal improvement in the mechanical character of
168 MANURES.
the soil. Thus stiff clay soils are rendered lighter,
and more easily workable, by an admixture of sand,
while light blowy sands are compacted, and made
more retentive of manure, by a dressing of clay or
of muck. Of course, this cannot be depended on as
a sure means of chemical improvement, but in a
majority of cases the land will be benefited by mix-
ing with it soil of a different character. It is not
always necessary to go to other locations to procure
the earth to be applied, as the sub-soil is often very
different from the surface soil, and simple deep plow-
ing will suffice, in such cases, to produce the required
admixture, by bringing up the earth from below to
mingle it with that of a different character at the sur-
face.
Until it is demonstrated that a large admixture of
the sub-soil will not lessen the fertility of the surface
(and in a large majority of cases it will not), it is
safest to deepen the plowing inch by inch. This
subject is worthy of the consideration of all farmers,
for there are very few cases in which the arable sur-
face will not be improved by the addition of matters
contained in the sub-soil. Even the earth thrown
from the bottom of deep ditches sometimes has an
astonishing effect on the fertility of the soil, and it
would be well to try the experiment of digging a
deep pit, spreading the earth taken, from it on the
surface of the land. If this is found to have a good
effect, it will offer a ready means of improving the
soil.
MANUKES. 160
In the foregoing remarks on the subject of mineral
manm'es, I have endeavored to point out such a
course as would result in the " greatest good to the
greatest number," and consequently, have neglected
much which might discourage the farmer with the
idea, that the whole system of scientific agriculture
is too expensive for his adoption. Still, while I have
confined my remarks to the more simple improve-
ments on the present system of management, I
would say briefly, that no manuring can he strictly
economical that is not hased on a hnowledge of the re-
quirements of the soil o/nd of the crops^ and of the
hest means of supplying them, together with the most
scrupulous care of every ounce of evaporating or sol-
uble manure made on the farm, a/rid a return of the
earthy matters sold off in produce.
CHAPTEE X.
ATMOSPHERIC FEETILIZEES.
It is not common to regard the gases in the at-
mosphere in the light of manures, but they are the
most important manures we have, as they are the
original source of more than nine-tenths of the entire
production of our fields. Indeed, they are almost the
only organic manure ever received by the uncultiva-
ted parts of the earth, as well as by a large portion of
8
170 MAJfTJKES.
that which is occupied in the production of food for
man.
If these gases were not manures ; if there were no
means by which they could be used by plants, the
fertility of the soil would long since have ceased, and
the earth would be unfertile. That this must be
true, will be shown by a few moments' reflection on
the facts stated in the first part of this book. The
fertilizing gases in the atmosphere being composed
of the constituents of decayed plants and animals, it
is as necessary that they should be again returned to
the form of organized matter, as it is that constitu-
ents taken from the soil should not be put out of
existence.
AMMONIA.
The ammonia in the atmosphere probably cannot
be appropriated by the leaves of plants, and must,
therefore, enter the soil to be assimilated by roots.
It reaches the soil in two ways. It is either arrested
from the air circulating through the soil, or it is ab-
sorbed by rains in the atmosphere, and thus carried
to the earth, where it is retained by its clay and car-
bon, for the uses of plants. In the soil, ammonia is
the most important of all organic manures. In fact,
the value of the organic parts of manure may be
estimated, either by the amount of ammonia which
they will yield, or by their power of absorbing am-
monia from other sources.
The most important use of ammonia in the soil is
MANURES. 171
to supply nitrogen to plants ; but it has other offices
which are of consequence. It assists in some of the
chemical changes necessary to prepare the matters
in the soil for assimilation, and gives to the water in
which it is dissolved an increased power to dissolve
mineral plant food.
Although, in the course of nature, the atmospheric
fertilizers are largely supplied to the soil, without
the immediate attention of the farmer, it is not be-
yond his power to cause their absorption in still
greater quantity. The means for doing this have
been repeatedly given in the preceding pages, but it
may be well to name them again in this chapter.
The condition of the soil is the main point to be
considered. It must be such as to absorb and retain
ammonia — to allow water to pass through it, and be
discharged helow the depth to which the roots of
crops are searching for food — and to admit of a free
circulation of air.
The power of absorbing and retaining ammonia is
not possessed by sand, but it is a prominent property
of clay, charcoal, and some other matters named as
absorbents. Hence, if the soil consist of pure sand,
it will not make use of the ammonia brought to it
from the atmosphere, but will allow it to evaporate
immediately after a shower, or to be washed through
it by rains. Soils in this condition require additions
of absorbent matters, to enable them to use the am-
monia received from the atmosphere. Soils already
containing a sufficient amount of clay or charcoal, are
thus far prepared to receive benefit from this source.
172 MANURES.
The next point is to cause tlie water of rains to
pass through the soil. If it lies on the surface, or
runs off without entering the soil, it is not probable
that the fertilizing matters which it contains will all be
abstracted. Some of them will undoubtedly return
to the atmosphere on the evaporation of the water ;
but, if the soil contains a sufficient supply of absorb-
ents, and will allow all rain water to pass through it,
the fertilizing gases will all be retained. They will
be filtered out of the water, which will pass out ot
the drains almost pure.
This subject will be more fully treated in Section
lY., in connection with under-draining.
Besides the properties just described, the soil
ought to possess the power of admitting a free cir-
culation of air. To effect this, the soil should be
well pulverized to a great depth. If, in addition to
-this, it be of such a character as to allow water to
pass through it, it will facilitate such a circulation of
air as is best calculated to give the greatest supply
of ammonia.
CAEBONIC ACID .
Carbonic acid is received from the atmosphere,
both by the leaves and by the roots of plants.
It is absorbed by the water in the soil, and greatly
increases its power of dissolving earthy plant food.
This use is one of very great importance, as it is
equivalent to making the minerals themselves more
soluble. Water dissolves carbonate of lime, etc.,
MANURES. 173
exactly in proportion to the amount of carbonic acid
which it contains. We shonld, therefore, strive to
have as much carbonic acid as possible in the water
in the soil. One way, in which to effect this, is to
admit to the soil the largest possible quantity of at-
mospheric air, which contains this gas.
The condition of soil necessary for this, is the same
as is required for the deposit of ammonia by the same
circulation of air.
OXYGEN.
Oxygen^ though not taken up by plants as food
in its pure form, may justly be classed among ma-
nures, if we consider its effects both chemical and
mechanical in the soil.
1. By oxidizing or rusting some of the constit-
uents of the soil, it prepares them for the uses of
plants.
2. It unites with the ^r<9toxide of iron, and
changes it to the j^^roxide.
3. If there are acids in the soil, which make it
sour and unfertile, it may be opened to the circula-
tion of the air, and the oxygen will prepare some of
the mineral matters contained in the soil to unite
with the acids and neutralize them.
4. Oxygen combines with the carbon of organic
matters in the soil, and causes them to decay. The
combination produces carbonic acid.
5. It undoubtedly affects in some way the matter
which is thrown out from the roots of plants. This,
174 MANUKES.
if allowed to accumulate, and remain unchanged, is
supposed to be injurious to plants ; but, probably,
the oxygen and carbonic acid of the air in the soil
change it to an inoffensive form, and even make it
again useful to the plant.
6. It may also improve the mechanical condition
of the soil, as it causes its particles to crumble, thus
making it finer ; and it roughens the surfaces of par-
ticles, making them less likely to become too com-
pact.
These properties of oxygen claim for it a high
place among the atmospheric fertilizers.
WATER.
Water may be considered an atmospheric ma-
nure, as its chief supply to vegetation is received
from the air in the form of rain or dew. Its many
effects are already too well known to need further
comment.
Supplying water to the soil by the deposit of dew
will be considered in Section lY.
CHAPTEK XI.
RECAPITULATION.
Manures have two distinct classes of action in the
soil, namely, chemical and mechanical.
MAJS^UEES. 176
Chemical manures are those which enter into the
construction of plants, or produce such chemical
effects on matters already contained in the soil as
shall prepare them for use.
Mechanical manures are those which improve the
mechanical condition of the soil, such as* loosening
stiff clays, compacting light sands, pulverizing large
particles, etc. Many manures act both chemically
and mechanically.
Manures may be classified under three distinct
heads, namely. Organic^ mineral^ and atmospheric.
Organic manures comprise all vegetable and ani-
mal matters (except ashes) which are used to fer-
tilize the soil. Yegetable manures supply carbonic
acid, some ammonia, and earthy matter to plants.
Animal manures supply the same substances and
much more ammonia.
Mineral manures comprise ashes, salt, phosphate
of lime, plaster, etc. They supply plants with earthy
matter. Their usefulness depends in great degree on
their solubility.
Many of the organic and mineral manures have
the power of absorbing ammonia arising from the de-
composition of animal manures, as well as that which
is brought to the soil by rains^these are called ab-
sorhents.
Atmospheric manures consist of ammonia, car-
bonic acid, oxygen and water. Their greatest use-
fulness requires the soil to allow the water of rains to
pass through it, to admit of a free circulation of air
among its particles, and to contain a sufficient
176 MAKTKES.
amount of absorbent matter to arrest and retain all
ammonia and carbonic acid presented to it.
Manures should be applied to the soil with due
regard to its requirements.
Ammonia and carbon are always useful, but
mineral manures become mere dirt when applied to
soils already containing them in abundance.
Organic manures must be protected against the
escape of their ammonia, and especially against the
leaching out of their soluble parts. One cord of
stable manure properly preserved, is worth ten cords
w^hich have lost all of their ammonia by evaporation,
and their soluble parts by leaching — as is the case
with much of the manure kept exposed in open
barn-yards.
Atmospheric manures cost nothing, and are of
great value when properly employed. In conse-
quence of this, the soil which is enabled to make the
largest appropriation of the atmospheric fertilizers,
is worth many times as much as that which allows
them to escape.
In fact, it may be considered to be the object of all
cultivation, to use the advantages which the soil and
manures offer for the purpose of consolidating and
giving a useful form to the carbonic acid, ammonia
and water, which are freely offered to all seekers.
Liebig says : — " A certain mass of gold and silver
circulates in the world, and the art of becoming
rich consists in knowing the way to divert from
the main stream an additional brook to one's own
house. In like manner there circulates, in the air
MANURES. 177
and in the soil, a relatively inexhaustible quantity
of the food of plants ; and the art of the farmer con-
sists in knowing and using the means of rendering
this food available for his* crops. The more he is
able to divert from the moving stream (the air) to
the immovable promoter of his production (the
soil of his fields), the more will the sum of his
wealth and his products increase."
8*
SECTION FOURTH.
MECHANICAL CULTIVATION,
SECTION FOURTH.
MECHANICAL CULTIVATION,
CHAPTEE I.
THE MECHANICAL CHARACTER OF SOILS.
The meclianical character of the soil has been
sufficiently explained in the preceding remarks, and
the learner knows that it has many offices to perform
aside from the feeding of plants.
1. It admits the roots of plants, and holds them in
their position.
2. By a sponge-like action, it holds water for the
uses of the plant.
3. It absorbs moisture from the atmosphere to
supply the demands of the plants.
4. It absorbs heat from the sun's rays to assist in
the processes of growth.
4. It admits air to circulate among roots, and sup-
ply them with a part of their food, while the oxygen
182 CULTIVATION.
of that air renders available the minerals of the soil ;
and its carbonic acid, being absorbed by the water in
the soil, gives it the power of dissolving and supply-
ing to roots more earthy matter than would be dis-
solved by purer water.
All of these actions the soil must be capable of
performing, before it can be in its highest state of
fertility. There are comparatively few soils now in
this condition, but there are also few which could
not be profitably rendered so, by a judicious appli-
cation of the various modes of cultivation.
The three great objects to be accomplished are : —
1. To adopt such a system of drainage as will
cause as much as possible of the water of rains to
pass through the soil, instead of evaporating from the
surface.
2. To pulverize the soil to a considerable depth.
3. To darken its color, and to render it capable of
absorbing atmospheric fertilizers.
The means used to secure these effects are under-
draining^ sub-soil and surface-jplowing^ digging^ ap-
plying muok^ etc.
CHAPTEK II.
UNDEK-DRAINING.
All soils which are cultivated should be thorough-
ly underdrained, either naturally or artificially.
CULTIVATION. 183
All lands which are made wet by springs or
through which the water of rains does not readily
settle away, must be drained artificially before they
can be cultivated to the best advantage.
The advantages of under-drains over qpen-drsdns
are very great.
When open drains are used, much water passes
into them immediately from the surface, and carries
with it fertilizing parts of the soil, while their beds
are often puddled by the running water and baked
by the heat of the sun, so that they become water
tight, and do not admit water from the lower parts
of the soil.
The sides of these drains are often covered with
weeds, which spread their seeds throughout the whole
field. Open drains are not only a great obstruction
to the proper cultivation of the land, but they cause
much waste of room, as we can rarely plow nearer
than within six or eight feet of them.
There are none of these objections to the use of
under-drains, as these are completely covered, and do
not at all interfere with the cultivation of the sur-
face.
Under-drains may be made with brush, stones, or
tiles. Brush is a very poor material, and its use is
hardly to be recommended, except when a better
material cannot be afforded. Small stones are bet-
ter, and if these be placed in the bottom of the
trenches, to a depth of eight or ten inches, and cov-
ered with a little litter, having the earth packed well
down on them, they make very good drains. But
184
CULTTVATION.
thej are very much more costly than tile drains, and
are not so permanent.
* TILE DKAINESra.
The best nnder-drains are those made with tiles,
or burnt clay pipes. The first form of these used
was that called the horse-shoe tile^ which has the
form of an arch, leaving the unprotected ground for
the water to flow over ; this was superseded by the
round pvpe^ and the sole tile.
" Experience in both public and private works in this
country, and the cumulative testimony of English and
French engineers, have demonstrated that the only
tile which it is economical to use, is the hest that can
be found, and that the best, — much the best, — thus
far invented, is the pipe, or round tile, (Mid collar ;
Fig. 3.— Round Tile and Collar.
and these are unhesitatingly recommended for use in
all cases. Round tiles of small sizes should not be laid
without collars, as the ability to use these constitutes
their chief advantage; holding them perfectly in
place, preventing the rattling in of loose dirt in lay-
ing, and giving twice the space for the entrance of
water at the joints. A chief advantage of the
larger sizes is, that they may be laid on any side and
thus made to fit closely. The usual sizes of these
CTTLTIYATION. 185
tiles are IJ inches, ^i inches, and 3|- inches in inte-
rior diameter. Sections of the 2J inch make collars
for the 1^ inch, and sections of the 3^ inch make
collars for the 2 J inch. The S^- inch does not need
collars, as it is easily secured in place, and is only
used when the flow of water wonld be sufficient to
wash out the slight quantity of foreign matters that
might enter at the joints." ^
Fig. 4— Sole TUe.
This tile is made (like the horse-shoe and pipe tile)
of common brick clay, and is burned the same as
bricks. It is about one half or three quarters of an
inch thick. The orifice through which the water
passes is egg-shaped, having its smallest curve at the
bottom. This shape is the one most easily kept clear,
as any particles of dirt which get into the drain
must fall immediately to the point where even the
smallest stream of water runs, and are thus removed.
An orifice of about two inches rise is sufficient for the
smaller drains, while the main drains require larger
tiles.
These tiles are so laid that their ends will touch
each other, on the bottoms of the trenches, and are
kept in position by having the earth tightly packed
* Draining for Profit and Draining for Healtli, by Gr. E. Waring,
Jr,^ page 81.
186
CULTIVATION.
around tliem. Care must be taken that no space is
left between the ends of the tiles, as dirt would be
liable to get in and choke the drain. This may be
best prevented by the use of collars / but if sole tiles
are used, as collars cannot be fitted to them, it is well
to cover the top of the joint with a very small rope
of twisted grass, secured by a stone or lump of clay
on each end, or to lay on the joint a saddle of bent
tin, zinc, or galvanized iron, which may be obtained
at little cost from a tinsmith, cut from pieces in the
waste-heap.
The ditches for tile draining may be narrowed in,
at the bottom, to a width barely sufficient for the
workman's foot. In filling-in, after the tile is laid,
care should be taken that no stones large enough to
break the tile be allowed to fall upon them. After
the tiles are covered to a depth of a foot or eighteen
inches, the filling should be trodden, or pounded,
firmly down, so as to fit closely around the tiles, and
leave no space for water to circulate about them.
Tile drains are made with
much less labor than the stone
drains, as they require less dig-
ging, while the breaking up of
the stone for the stone drain
will be usually more expen-
sive than the tiles. Drains
made with large stones are not
nearly so good as with small
<>-Sod laid on the stone, ^^^^g^ because they are more
liable to be choked up by animals working in them.
Fig. 5.
a — Tile drain trench.
b — Stone drain trench.
CULTIVATION. 187
CHAPTEK III.
ADVANTAGES OF U ND E E - DE AINI N G.
The advantages of under-draining are many and im-
portant.
1. It greatly lessens the injurious effects of drought.
2. It admits an increased supply of atmospheric
fertilizers.
3. It warms the lower portions of the soil.
4. It hastens the decomposition of roots and other
organic matter.
5. It accelerates the disintegration of the minerals
in the soil.
6. It causes a more even distribution of nutritious
matters among those parts of soil traversed by roots.
7. It improves the mechanical texture of the soil.
8. It tends to prevent grasses from " running out."
9. It enables us to deepen the surface soil.
By removing excess of water —
10. It renders soils earlier in the spring.
11. It greatly lessens the throwing out of grain in
winter.
12. It allows us to work sooner after rains.
13. It keeps off the effects of cold weather longer
in the fall.
14. It prevents the formation of acetic and other
organic acids, which induce the growth of sorrel and
similar weeds.
15. It hastens the decay of vegetable matter, and
188 CULTIVATION. '
the finer comminution of the earthy parts of the
soiL
16. It prevents, in a great measure, the evapora-
tion of water, and the consequent cooling of the soil.
17. It admits fresh quantities of water from rains,
etc., which are always more or less imbued with the
fertilizing gases of the atmosphere, to be deposited
among the absorbent parts of soil, and given up to
the demands of plants.
18. It prevents the formation of so hard a crust
on the surface of the soil as is customary on heavy
lands.
1. Under-draining lessens the effect of droughty be-
cause it gives a better cu'culation of air in the soil
(it does so by making it more open). There is al-
ways the same amount of water in and about the
surface of the earth. In winter there is more in the
soil than in summer, while in summer, that which
has been diied out of the soil exists in the atmosphere
in the form of a vai^or. It is held in the vapory-
form by heat^ which acts as hraces to keep it distend-
ed. When vapor comes in contact with substances
sufficiently colder than itself, it gives up its heat —
thus losing its braces — contracts, and becomes liquid
water.
This may be observed in hundreds of common
operations.
It is well known that a cold pitcher in summer
CULTIVATION. 189
robs the vapor in the atmosphere of its heat, and
causes it to be deposited on its own surface. It looks
as though the pitcher were sweating^ but the water
all comes from the atmosphere, not, of course, through
the sides of the pitcher.
If we breathe on a knife-blade, it condenses in the
same manner the moisture of the breath, and becomes
covered with a film of water.
Stone houses are damp in summer, because the
inner surfaces of the walls, being cooler than the
atmosphere, cause its moisture to be deposited in the
manner described. By leaving a space, however,
between the walls and the plaster, this moisture is
prevented from being troublesome, and if the space
is closed against the circulation of air containing
moisture there will be no vapor brought in contact
with the cool surface of the wall, and therefore no
deposit of moisture.
JN^early every night in the summer season, the cold
earth receives moistm-e from the atmosphere in the
form of dew.
A cabbage, which at night is very cold, condenses
water to the amount of a gill or more.
The same operation takes place in the soil. When
the air is allowed to circulate among its lower and
cooler particles, they receive moisture from the same
process of condensation. Therefore, when, by the
aid of under-drains, the lower soil becomes sufficient-
ly open to admit of a circulation of air, the deposit of
atmospheric moisture will keep the soil supplied with
water at a point easily accessible to the roots of plants.
190 CIJLTTVATION.
If we wish to satisfy ourselves that this is practi-
cally correct, we have only to prepare two boxes of
finely pulverized soil — one, five or six inches deep,
and the other fifteen or twenty inches deep — and
place them in the sun at mid-day in summer. The
thinner soil will be completely dried, while the deeper
one, though it may have been dried in an oven at
first, will soon accumulate a large amount of water
on those particles which, being lower and more
sheltered from the sun's heat than the particles of
the thin soil, are made cooler.
"With an open condition of subsoil, then, such as
may be secured by under-draining, we fortify our-
selves against drought.
2. Under-draining admits an increased supply of
atmospheric fertilizers^ because it secures a change
of air in the soil. This change is produced when
ever the soil becomes filled with water, and then
dried ; when the air above the earth is in rapid mo-
tion, and when the comparative temperature of the
upper and lower soils changes. It causes new quan-
tities of the ammonia and carbonic acid which it
contains to be presented to the absorbent parts of
the soil.
3. Under-draining warms the lower parts of the
soil, because the deposit of moisture (1) is necessarily
accompanied by an abstraction of heat from the at-
mospheric vapor, and because heat is withdrawn
from the whole amount of air circulating through
the cooler soil.
When rain falls on the parched surface soil^ it robs
CULTIVATION. 191
it of a portion of its heat, which, is carried down to
equalize the temperature for the Avhole depth. The
heat of the rain-water itself is given up to the soil,
leaving the water from one to ten degrees cooler,
when it passes out of the drains, than when received
by the earth.
This heating of the lower soil of course renders it
more favorable to vegetation.
4. Under-draining hastens the decomposition of
roots and other organic matters in the soil, by ad-
mitting increased quantities of air, thus supplying
oxygen^ which is as essential in decay as it is in com-
bustion. It also allows the resultant gases of de-
composition to pass away, leaving the air around
the decaying substances in a condition to continue
the process.
This organic decay, besides its other benefits, pro-
duces an amount of heat perfectly perceptible to the
smaller roots of plants, though not so to us.
5. Draining accelerates the disintegration of the
minerals in the soil, by admitting water and oxvgen
to keep up the process. This disintegration is aG-.
cessary to fertility, because the roots of plants can
feed only on matters dissolved from surfaces / and
the more finely we pulverize the soil, the more sur-
face we expose. For instance, the interior of a stone
can furnish no food for plants; while, if it were
finely crushed, it might make a fertile soil.
Anything tending to open thesoilto the air facili-
tates the disintegration of its particles, and thereby
increases its fertility.
192 CULTIVATION.
6. Draining causes a more even distribution of
nutritious rrtatters among those jparts of soil trav-
ersedhy roots^ because it increases the ease with which
water travels about, descending by its own weight,
moving sideways by a desire to find its level, or car-
ried upward by attraction to supply the evaporation
at the surface. By this continued motion of the
water, soluble matter from one part of the soil may
be carried to adjacent parts ; and another constitu-
ent from this latter position may be carried back to
the former. Thus the food of vegetables is evenly
distributed through the soil. As soon as one parti-
cle is fully supplied with any element of plant nu-
trition, further amounts brought by water are carried
to the next particle that can receive it — and so on,
until the supply of soluble material is exhausted.
This food is ready for absorption at any point where
it is needed, while the more open character of the
soil enables roots to occupy larger portions, making a
more even drain on the whole, and preventing the
undue impoverishment of any part.
7. Under-drains improve the mechanical texture of
the soil I because, by the decomposition of its parts,
as previously described (4 and 5), it is rendered of
a character to be more easily worked ; while smooth
round particles, which have a tendency to pack, are
roughened by the oxidation of their surfaces, and
move less easily among each other.
8. By under-draining, grasses are prevented from
running out. The grasses of meadows usually con-
sist of tillering plants, which reproduce themselves
CULTIVATION. 103
in sprouts from the upper parts of their roots, or
from the joints of the roots. These sprouts become
independent plants, and continue to tiller (thus
keeping the land supplied with a full growth ), until
the roots of the stools ( or clumps of tillers ), come
in contact with an uncongenial part of the soil,
when the tillering ceases ; the stools become extinct
on the death 'of their plants, and the grasses run
out.
The open and healthy condition of soil pro-
duced by draining prevents the tillering from being
stopped so long as the fertility of the soil lasts, and
thus keeps up a full growth of grass until the nutri-
ment of the soil is exhausted.
9. Draining enables us to deepen the surface-soil^
because the admission of air and the decay of roots,
( which descend much deeper in drained than in un-
drained land,) render the condition of the sub-soil
such, that it may be brought up and mixed with the
surface-soil, without injuring its quality.
The second class of advantages of under-drain-
ing, arising in the removal of the excess of water
in the soil, are quite as important as those just de-
scribed.
10. Soils are^ thereby^ rendered earlier in spring^
because the water, which rendered them cold, heavy,
and nntillable, is earlier removed, leaving them ear-
lier in a growing condition.
11. The throwing out of grain in winter is les-
sened, because the water falling on the earth is im-
mediately removed instead of remaining to throw up
9
194 CULTIVATION.
the soil by freezing, as it always does, from the up-
right position taken by the particles of ice.
12. We are enabled to work sooner after rains,
because the water descends, and is immediately re-
moved, instead of lying to be taken off by the slow pro-
cess of evaporation, and sinking through a heavy soil.
13. The effects of cold weather are Itejpt off longer
in the fall, by the removal of the excess of water
w^hich would produce an unfertile condition on the
first appearance of cold weather.
The drains also, from- causes already named (3),
keep the soil warmer than before being drained, thus
actually lengthening the season, by making the soil
warm enough for vegetable growth earlier in springj
and later in autumn.
14. Lands are prevented from hecoming sour hy
the formation of acetic acid, etc., because these acids
are produced in the soil only when organic matter
decomposes in contact with an excessive quantity of
water. If the water is removed, the decomposition
of the organic matter assumes a healthy form, while
the acids already produced are neutralized by atmos-
pheric influences, and the soil is restored to a condi-
tion in which it is fitted for the growth of the more
valuable plants.
15. The deca/y of roots, etc., is allowed to proceed,
because the preservative influence of too much water
is removed. Wood, leaves, or other vegetable matter
kept continually under water, will last for ages ;
while, if exposed to the action of the weather, as in
under-drained soils, they soon decay.
CULTIVATION. 195
The presence of too much water, by excluding the
oxygen of the air, prevents the comminution of m^in-
eral matters necessary to fertility.
16. The evajporation of water ^ and the consequent
cooling of the soil^ is in a great measure prevented
by draining the water out at the hottom^ of the soil,
instead of leaving it to be dried off from the sur-
face.
When water assumes the gaseous (or vapory) form,
it occupies nearly 2000 times the space it occupied
as a liquid, and as the vapor is of the same tempera-
ture as the liquid, it follows that it contains vastly
more heat. A large part of this heat is derived
from surrounding substances. When water is sprink-
led on the floor, it cools the room ; because, as it
becomes a vapor, it takes heat from the room. The
reason why vapor does not feel hotter than liquid
water is, that, its heat is diffused through the larger
mass, so that a cubic inch of vapor, into which we place
the bulb of a thermometer, contains no more heat than
a cubic inch of water. The principle is the same in
some other cases. A sponge containing a table-
spoonful of water is just as wet as one twice as large
containing two spoonfuls.
If a wet cloth be placed on the head, and the evap-
oration of its water assisted by fanning, the head
becomes cooler — a portion of its heat being taken to
sustain the vapory condition of the water.
The same principle holds true with the soil.
When the evaporation of water is rapidly going on,
by the assistance of the sun, wind, etc., a large
196 CULTIVATION.
quantity of heat is abstracted, and the soil becomes
cold.
This cooling of the soil by the evaporation of
water, is of very great injury to its power of pro-
ducing crops, and the fact that under-drains lessen
it, is one of the best arguments in favor of their
use. Some idea may, perhaps, be formed of the
amount of heat taken from the soil in this way, from
the fact that, in midsummer, twenty-iive hogsheads
of water may be evaporated from a single acre in
twelve hours.
17. When not saturated with water the soil ad-
mits the water of rains, etc., which bring with them
fertilizing gases from the atmosphere^ to be deposit-
ed among the absorbent parts of the soil, and given
up for the necessities of the plant. When this rain
falls on lands already saturated, it cannot enter the
soil, but must run off from the surface, or be re-
moved by evaporation, either of which is injurious.
The first, because fertilizing matter is washed away.
The second, because the soil is deprived of necessary
heat.
18. The formation of crust on the surface of the
soil is due to the evaporation of the water of the soil.
It arises partly from the fact that the water in the
soil is saturated with mineral substances, which it
leaves at its point of evaporation at the surface.
This soluble matter often forms a very hard crust,
which is a complete shield to prevent the admission of
air with its ameliorating effects, and should, as far
as possible, be avoided. Under-draining is the best
CULTIVATION. 197
means of doing this, as it is the best means of lessen-
ing the evaporation, and of preventing the puddling
of the clay in the soil.
The foregoing are some of the more important
reasons why nnder-draining is always beneficial.
Thorough experiments have amply proved the truth
of the theory.
" Land which requires draining is that which, at
some time during the year, (either from an accumu-
lation of the rains which fall upon it, from the later-
al flow or soakage from adjoining land, from springs
which open within it, or from a combination of two
or all of these sources,) becomes filled with water
that does not readily find a natural outlet, but
remains until removed by evaporation. Every con-
siderable addition to its water wells up, and soaks
its very surface ; and that which is added after it is
already brim-full, must flow ofi" over the surface, or lie
in puddles upon it. Evaporation is a slow process,
and it becomes more and more slow as the level of
the water recedes from the surface, and is sheltered
by the overlying earth from the action of sun and
wind. Therefore, at least during the periods of
spring and fall preparation of the land, during the
early growth of plants, and often even in mid-
summer, the water-taUe^ — the top of the water of
saturation, — is within a few inches of the surface,
preventing the natural descent of roots, and, by
reason of the small space to receive fresh rains, caus-
ing an interruption of work for some days after each
storm.
198 CULTIVATION.
" If such land is properly furnished with tile drains,
(having a clear and sufficient outfall, offering suffi-
cient means of entrance to the water which reaches
them, and carrying it, by a uniform or increasing
descent, to the outlet,) its water will be removed to
nearly, or quite, the level of the floor of the drains, '
and its water-table will be at the distance of some
feet from the surface, leaving the spaces between the
particles of all the soil above it filled with air instead
of water. The water below the drains stands at a
level, like any other water that is dammed up.
Rain-water falling upon the soil, will descend by its
own weight to this level, and the water will rise into
the drains, as it would flow over a dam, until the
proper level is again obtained. Spring-water enter-
ing from below, and water oozing from the adjoin-
ing land, will be removed in like manner, and the
usual condition of the soil, above the water-table,
will be that which is best adapted to the growth of
useful plants.
"In the heaviest storms, some water will flow over
the surface of even the dry est beach sand ; but in a
well-drained soil the water of ordinary rains will be
at once absorbed, will slowly descend toward the
water- able, and will be removed by the drains so
rapidly, even in heavy clays, as to leave the ground
fit for cultivation, and in a condition for steady
growth, within a short time after the rain ceases. It
has been estimated that a drained soil has room
between its particles for about one quarter of its
bulk of water, that is, four inches of drained soil con-
CULTIVATION. 199
tains free space enough to receive a rain-fall one inch
in depth, and, by the same token, four feet of
drained soil can receive twelve inches of rain, —
more than is known to have ever fallen in twenty-
four hours since the deluge, and more than one quar-
ter of the annual rain-fall in the United States y *
Of the ^VQQi^e profits of under-draining this is not
the place to speak : many of the agricultural papers
contain numerous accounts of its success. It may be
well to remark here, that many English farmers
give it, as their experience, that under-drains on
heavy clay lands in ordinary cultivation, pay for
themselves every three years, or that they produce a
perpetual profit of 33^- per cent., on their original
cost. This is not the opinion of theorists and hooh
farmers. It is the conviction of practical men, who
know,yr(?m experience^ that under-drains are bene-
ficial.
The best evidence of the utility of under-drain-
ing is the position, with regard to it, which has been
taken by the English national government, which
aifords much protection to the agricultural interests
of the people, — a protection which in this country is
unwisely and unjustly withheld.
In England, a very large sum from the public
treasury has been appropriated as a fund for loans,
on under-di*ains, which was lent to farmers for the
purpose of under-draining their estates, the only
security given being the increased value of the soil.
The time allowed for payments was twenty years,
* Drainmg for Profit and Health, p. 22.
200 CULTIVATION.
and only i^ve per cent, interest is charged. By the
influence of this patronage, the actual wealth of the
kingdom has been rapidly increased, while the
farmers themselves can raise their farms to the
highest fertility, without immediate investment for
draining.
The best proof that the government has not acted
injudiciously in this matter is, that private capitalists
employ their money in the same manner, and loans
on under-drains are considered a very safe invest-
ment.
One very important, though not strictly agricul-
tural, effect of thorough drainage is its removal of
certain local diseases, peculiar to the vicinity of
marshy or low moist soils. The health-reports in
several places in England, show that where fever and
ague was once common, it lias almost entirely dis-
appeared since the general use of under-drains in
those localities.
CHAPTEK lY.
SUB-SOIL PLOWING.
The sub-soil plow is an implement differing in figure
from the surface plow. It does not turn a furrow,
but merely runs through the sub-soil like a mole —
loosening and making it finer by lifting, but allow-
ing it to fall back and occupy its former place. It
CULTIVATION.
20i
usually follows the surface plow, entering the soil to
the depth of from eight to fifteen inches below the
bottom of the surface furrow.
The best pattern now made (the steel sub-soil
plow) is represented in the following figure.
Fig. 6.— Wrought Iron and Steel Sub-soil Plow.
The sub-soil plows first made raised the whole soil
about eight inches, and required very great power in
their use, often six or eight oxen. The implement
shown in the figure, raising the soil but slightly, may
be worked with much less power, and produces
equally good results. It may be run to a good
depth in most soils by a single yoke of oxen.
The motion of any part of the soil w^hich is efifected
by this sub-soil plow is very slight, but it is exerted
throughout the whole mass of the soil above the
9*
202 CULTIVATION.
plow and for a considerable distance sideways tow-
ard the surface. If the land is too wet, this motion
will be injurious rather than beneficial, but if it is
dry enough to crumble, it will be very much loosened.
If we hold in the hand a ball of dry clay, and press
it hard enough to produce the least motion among
its particles, the whole mass becomes pulverized.
On the same principle, the sub-soil plow renders the
compact lower soil sufficiently fine for the entrance
of roots.
Notwithstanding its great benefits on land, which
is sufficiently dry, sub-soiling cannot be recommended
for wet lands ; for, in such case, the rains of a single
season would often be sufficient to entirely overcome
its efiects by packing the sub-soil down to its former
hardness.
On lands not overcharged with water, it is produc-
tive of the best results, it being often sufficient to
turn the balance between a gaining and a losing
business in farming.
It increases nearly every efiect of under-draining ;
especially does it overcome drought, by loosening
the soil, and admitting air to circulate among the
particles of the sub-soil, and deposit its moisture, on
the principle described in the chapter on under-
draining.
It deepens the surface-soil, because it admits roots
into the sub-soil where they decay and leave carbon,
while the circulation of air so afiects the mineral
parts, that they become of a fertile character. As
a majority of roots decay in the surface-soil, they
CULTIVATION. 203
there deposit much mineral matter obtained from
the sub-soil, and thus render it richer.
The retention of atmospheric manures is more
folly insured by the better exposure of the clayey
portions of the soil.
The sub-soil often contains matters which are defi-
cient in the surface-soil. By the use of the sub-soil
plow, they are rendered available.
Sub-soiling is similar to under-draining in continu-
ing the tillering of grasses.
"When the sub-soil is a thin layer of clay on a sandy
bed (as in many parts of the country), the sub-soil
plow, by passing through it, opens a passage for water,
and often affords a sufiicient drainage.
If plants will grow better on a soil six inches deep
than on one of three inches, there is no reason why
they should not be benefited in proportion, by disturb-
ing the soil to the whole depth to which roots will
travel — even to a depth of two feet. The minute
rootlets of corn and most other plants will, if allow-
ed by cultivation, occupy the soil to a greater depth
than this, having a fibre in nearly every cubic inch of
the soil for the whole distance. There are very few
cultivated plants whose roots would not travel to a
depth of thirty inches or more. Even the onion sends
its roots to the depth of eighteen inches when the soil
is well cultivated.
The object of loosening the soil is to admit roots-
to a sufiicient depth to hold the plant in its position,
— to obtain the nutriment necessary to its growth, —
to receive moisture from the lower portions of the
20dl: CULTIVATION.
soil, — and, if it be a bulb, tuber, or tap, to assume
the form requisite for its largest development.
It must be evident that roots, penetrating the soil
to a depth of two feet, anchor the plant with greater
stability than those which are spread more thinly
near the surface.
The roots of plants traversing the soil to such
great distances, and being located in nearly every
part, absorb mineral and other food, in solution in
water, only through the spongioles at their ends.
Consequently, by having these ends in every part of
the soil, it is all brought under contribution, and the
amount supplied is greater, while the demand on any
particular part may be less than when the whole re-
quirements of plants have to be supplied from a depth
of a few inches.
The ability of roots to assume a natural shape in
the soil, and grow to their largest size, must depend
on the condition of the soil. If it is finely pulverized
to the whole depth to which they ought to go, they
will be fully developed ; while, if the soil be too hard
for penetration, they will be deformed or small. Thus
a parsnip may grow to the length of two and a half
feet, and be of perfect shape, while, if it meet in its
course, at a depth of eight or ten inches, a cold^ hard
sub-soil, its growth must be arrested, or its form in-
jured.
Roots are turned aside by a hard or wet sub-soil,
as they would be if received by the surface of a plate
of glass.
Add to this the fact tb^t cold, impenetrable sub-
CULTIVATION. 205
soils are chemically uncongenial to vegetation, and
we have sufficient evidence of the importance, and
in many cases the absolute necessity of sub-soiling
and under-draining.
It is unnecessary to urge the fact that a garden
soil of two feet is more productive than a field soil
of six inches ; and it is certain that proper attention
to these two modes of cultivation will in a majority
of cases make a garden of the field — more than doub-
ling its value in ease of working, increased produce,
certain security against drought, and more even distri-
bution of the demands on the soil — while the outlay
will be largely repaid by an immediate increase of
crops.
The sub-soil will be much improved in its charac-
ter the first year, and a continual advancement ren-
ders it in time equal to the original surface-soil, and
extending to a depth of two feet or more.
The sub-soil plow has come into very general use.
The implement has ceased to be a curiosity ; and the
man who now objects to its use, may be classed with
him who shells his corn on a shovel over a half-bush-
el, instead of employing an improved machine, which
will enable him to do more in a day than he can do
in the " good old way " in a week.
In no case will the use of the sub-soil plow be found
anything but satisfactory, except in occasional in-
stances where there is some chemical difficulty in the
sub-soil, which will be overcome by a year or two
of exposure — and even such cases are extremely rare.
As was before stated, its use on wet lands is not
203 CULTIVATION.
advisable until thej have been under-drained, as
excess of water prevents its effects from being per-
manent.
CHAPTEK Y.
PLOWING AND OTHEK PROCESSES FOR
PULVERIZING THE SOIL.
The advantages of pulverizing the soil, and the
reasons why it is necessary, have been sufficiently
explained to need no further remark. Few farmers,
when they plow, dig, or harrow, are enabled to give
substantial reasons for the operation. If they will re-
j9.ect on what has been said in the preceding chapters,
concerning the supply of mineral food to the plant
by the soil, and the effect of air and moisture about
the roots, they will find more satisfaction in their
labor.
PLOWING.
The kind of plow used in cultivating the surface-
soil, must be decided by the kind of soil. This
question the practical, observing farmer will be able
to solve.
As a general rule, it may be stated that the plow
which runs the deejpest^ with the same amount of
CULTIVATION'. 207
force, is the best, but this rule is not without its
exceptions.
The advantages of deejp plowing cannot be too
strongly urged.
The statement that the deeper and the jmer the
soil is rendered, the more productive it will become,
is in every respect true, and no single instance will
contradict it.
It must not be inferred from this, that we would
advise a farmer, who has always plowed his soil to
the depth of only six inches, to double the depth at
once. Such a practice in some soils would be highly
injurious, as it would completely bury the more fer-
tile and better cultivated soil, and bring to the top
one which contains no organic matter, and has never
been subject to atmospheric influences. This would,
perhaps, be so little fitted for vegetation that it
would scarcely sustain plants until their roots could
reach the more fertile parts below. Such treatment
of the soil ( turning it upside down ) is excellent in
garden culture, where the great amount of manures
applied is sufiicient to overcome the temporary bar-
renness of the soil, but it is not to be recommended
for all field cultivation, where much less manure is
employed.
The course to be pursued in such cases is to plow
a little deeper each year. By this means the soil
may be gradually deepened to any desired extent.
The amount of uncongenial soil which will thus be
brought up, is slight, and will not interfere at all
with the fertility of the soil, while the elevated por-
208 CULTIVATION.
tion will become, in a single year, so altered bv ex-
posure, that it will equal the rest of the soil in
fertility.
Often where lime has been used in excess, it has
sunk to the sub-soil, where it remains inactive. A
slight deepening of the surface plowing would mix
this lime with the surface-soil, and render it again
useful.
When the soil is light and sandy, resting on a
heavy clay sub-soil, or clay on sand, the bringing up
of the mass from below will improve the texture of
the upper parts.
As an instance of the success of deep plowing, we
call to mind the case of a farmer in New Jersey,
who had a field which had yielded about twenty-five
bushels of corn per acre. It had been cultivated at
ordinary depths. After laying it out in eight-step
lands (24 feet,) he plowed it at all depths from five
to ten inches on the difierent lands, and sowed oats
evenly over the whole field. The crop on the five
inch soil was very poor, on the six inch rather better,
on the seven inch better still, and on the ten inch
soil it was as fine as ever grew in 'New Jersey ; it
had stifi" straw and broad leaves, while the grain
was also much better than on the remainder of the
field.
There is an old anecdote of a man who died, leav-
ing his sons with the information that he had buried
a pot of gold for them, somewhere on the farm.
They commenced digging for the gold, and dug over
the whole farm to a great depth without finding the
CULTIVATION. 209
gold. The digging, however, so enriched* the soil
that they were fully compensated for their disap-
pointment, and became wealthy from the increased
produce of their farm.
Farmers will find, on experiment, that they have
gold buried in their soil, if they will but dig deep
enough to obtain it. The law gives a man the own-
ership of the soil for an indefinite distance from the
surface, but few seem to realize that there is another
farrrh below the one they are cultivating, which is
quite as valuable as the one on the surface, if it were
but properly worked.
Fall jplowing^ especially for heavy lands, is the
best means of securing the action of the frosts of
winter to pulverize the soil. If it be a stiff clay, it
will be well to throw the up-soil in high ridges ( by
ridging and back-furrowing,) so as to expose the
largest possible amount of surface to the freezing and
thawing of winter. This, with the rotting of the
sod, (which is thus made ready for the feeding
of plants,) makes the effects of fall plowing almost
universally beneficial. The earlier the plowing is
done, the more thoroughly the sod is rotted and pre-
pared for the nutrition of the crop of the next year.
The great improvement of the age in the mechan-
ical branch of agriculture, has been made in England,
during the past ten or tw^elve years, in the application
of the steam-engine to the work of cultivating the
soil. It would be beyond the scope of a simple
elementary book like this to enter fully into a de-
scription of the machinery by which this work is
210 CULTIVATION.
done, and the method of its operation ; but it is worthy
of remark, that there are now in use in England
about 500 sets of the apparatus, and that the system
has been in successful operation there for about a
dozen years. A single engine (of 14 horse power)
moves to the field on its own wheels, carrying the
tackle with it, and plows an acre an hour with ease,
or draws a deep cultivator through from three to five
acres in an hour. The engine stands on one head-
land, and a pulley- wheel on the other, an endless steel
wire rope passes around a windlass under the engine,
and around the pulley opposite. The gang of plows,
or the wide cultivator, is drawn back and forth be-
tween the two.
THE HAEKOW AND CULTIVATOR.
The harrow^ an implement largely used in all
parts of the world, to pulverize the soil, and break
clods, has become so firmly rooted in the afiections
of farmers, that it must be a very long time before
they can be convinced that it is not the best imple-
ment for the use to which it is devoted. It is true
that it pulverizes the soil for a depth of two or three
inches, and thus much improves its appearance, bene-
fiting it, without doubt, for the earliest stages of the
growth of plants. Its action, however, is very defec-
tive, because, from the wedge shape of its teeth, it
continually acts to jpack the soil ; thus — although
favorable for the germination of the seed — it is not
calculated to benefit the plant during the later stages
CULTIVATION. 211
of its growth, when the roots require the soil to be
pulverized to a considerable depth.
The cultivator may be considered an i7nproved
harrow, the principal difference between them being,
that while the teeth of the harrow are pointed at
the lower end, those of the cultivator are shaped
like a small double plow, being large at the bottom
and growing smaller toward the top. They lift
the earth up, instead of pressing it downward, thus
loosening instead of compacting the soil.
Many styles of cultivators are now sold at agri-
cultural warehouses. A very good one, for field use,
may be made by substituting the cultivator teeth for
the spikes in an old harrow frame.
CHAPTEK YI.
ROLLING, MULCHING, WEEDING, ETC.
ROLLING.
Rolling the soil with a large roller, drawn by
a team, is in many instances a good accessory to cul-
tivation. By its means, the following results are ob-
tained : —
1. The soil at the surface is pulverized without the
compacting of the lower parts, the area of contact
being large.
212 CTJLTIVATION.
2. The stones on the land are pressed down so as
to be out of the way of the mowing machine.
3. The soil is compacted around seeds after sow-
ing in such a manner as to exclude light and to touch
them in every part, both of which are of essential
advantage in their germination, and assist in giving
them a good start.
4. When the soil is smoothed in this manner, there
is less surface exposed for the evaporation of water
with its cooling effect.
5. Light sandy lands, by being rolled in the fall,
are rendered more compact, and the loosening effects
of frequent freezing and thawing are lessened.
6. The most important use of the roller is in com-
pacting the earth about the roots of grass and grain
crops early in the spring. The freezing and thaw-
ing of winter leave them usually partly uncovered,
or surrounded by air spaces. Their best growth re-
quires that these roots be closely pressed by the earth,
— ^and this pressure is given by the roller better than
in any other way.
If well under-drained, a large majority of soils
would doubtless be benefited by a judicious use of the
roller.*
MULCHING.
Mulching consists in covering the soil with salt
hay, litter, seaweed, leaves, spent tanbark, chips, or
other refuse matter.
Every farmer must have noticed that, if a board or
* Field rollers should be made in sections, for ease of turning.
CULTIVATION. 213
rail, or an old brush-heap, be removed in spring from
soil where grass, is growing, the grass afterward
grows in those places much larger and better than
in other parts of the field.
This improvement arises from various causes.
1. The evaporation of water fi-om the soil is pre-
vented during drought by the shade afforded by the
malch ; and it is therefore kept in better condition,
as to moisture and temperature, than when evapora-
tion goes on more freely. This condition is well cal-
culated to advance the chemical changes necessary to
prepare the matters — both organic and mineral — in
the soil for the use of plants.
2. A heavy mulch breaks the force of rains, and
prevents them from compacting the soil, as would be
the result were no such precaution taken.
3. Mulching protects the surface-soil from freez-
ing as readily as w^hen exposed, and thus keeps it
longer open for the admission of air and moisture.
"When unprotected, the soil early becomes frozen ;
and all water falling, instead of entering, as it should
do, passes oiF over the surface.
5. The throwing out of winter grain is often pre-
vented, because this is due to the frequent freezing
and thawing of the surface-soil.
6. When the wet surface-soil freezes, it is raised up,
and the young plants growing in it are raised with
it ; when the frost is thawed out, the soil falls back
to its original position, while parts of the crowns or
roots of the crop remain raised. The next freeze
takes hold of them lower down, and lifts them again ;
214 CULTIVATION.
the next thaw leaves them higher than ever, — until in
spring, sonietimes, the crown of a shoot of wheat
will be standing several inches above the level of
the soil. The use of a mulch prevents both the
freezing and the thawing from being so frequent and
active as thej would be if no protection were used.
7. It also prevents the " baking " of the soil, or the
formation of a crust.
Nursery-men often keep the soil about the roots of
young trees mulched continually. One of the chief
arguments for this treatment is, that it prevents the
removal of the moisture from the soil and the conse-
quent loss of heat. Also that it keeps up a full sup-
ply of water for the uses of the roots, because it keeps
the surface of the soil cool, and causes a deposit of dew.
It has been suggested, and is undoubtedly true, that
a mulch on the ground, by affording a good shelter for
minute (microscopic) insects, causes them to accumu-
late in such quantities as to add (by their eggs, their
excrement, and their dead bodies) to the fertilizing
matter in the soil. How important this addition
may be, we cannot of course know, but it is certain
that mulching exercises greater good effect than can
reasonably be attributed, in the present state of our
knowledge, to any or all of the above described actions.
It is the opinion of many, that at least one-half of
the beneficial effect of seaweed, or coarse stable ma-
nure, when used as a top dressing, is due to its action
as a mulch.
It is a good plan to sow oats very thinly over land
intended for winter fallow, after the removal of crops,
CULTIVATION. 215
as they will grow a little before being killed by the
frost, when they will fall down, thus affording a very
beneficial mulch to the soil.
When farmers spread coarse manure on their fields
in the fall to be plowed under in the spring, they ben-
efit the land by the mulching, perhaps as much as by
the addition of fertilizing matter, because they give
it the protecting influence of the straw, etc.
It is an old and true saying that " snow is the
poor man's manure." One reason why it is so bene-
ficial is, that it acts as a most excellent mulch. It
contains no more ammonia than rain-water does ;
and, were it not for the fact that it protects the soil
against loss of heat, and produces other benefits of
mulching, it would have no more advantageous effect.
The severity of the winters at the North is largely
compensated for by the long duration of snow.
It is well known that when there is but little snow
in cold countries, wheat is very liable to be winter
hilled. An evenly spread mulch, and thorough
draining, will greatly prevent this.
This treatment is peculiarly applicable to the cul-
tivation of flowers, both in pots and in beds out of
doors. It is almost indispensable to the profitable
production of strawberries, and many other garden
crops, such as asparagus, rhubarb, etc. An excel-
lent treatment for newly transplanted trees, is to put
stones about their roots. A good mulching, by the
use of leaves, copying the action of nature in forests,
has nearly as good an effect ; for it is chiefly as a
mulch that the stones are beneficial.
216 CULTIVATION.
WEEDma.
If a farmer were asked — what is the use of weeds ?
he might make out quite a list of their benefits,
among which might be some of the following : — ■
1. Thej shade tender plants, and in a measure
serve as a mulch to the ground.
2. Some weeds, by their offensive odor, drive
away many insects.
^ 3. They may serve as a green crop to be plowed
into the soil, and increase its organic matter.
4. They make us stir the soil, and thus increase
its fertility.
Still, while thinking out these excuses for weeds
(all but the last of which are very feeble ones), he
would see other and more urgent reasons why they
should not be allowed to grow.
1. They occupy the soil to the disadvantage of
crops.
2. They exclude light and heat from cultivated
plants, and thus interfere with their growth.
3. They take up mineral and other matters from
the soil, and hold them during the growing season,
thus depriving crops of their use.
It is not necessary to argue the injury done by
weeds. Every farmer is well convinced that they
should be destroyed, and the best means of accom-
plishing this is of the greatest importance.
In the first place, we should protect ourselves against
their increase. This may be done (in a measure) : —
Bjr decomposing all manures in compost, whereby
' CULTIVATION. 217
many of the seeds contained will be killed by the
heat of fermentation.
By hoeing, or otherwise destroying growing weeds
before they mature their seeds ; and
By keeping the soil in the best chemical condition.
This last point is one of much importance. It
is well known that soils deficient in potash will
naturally produce one kind of plants, while soils
deficient in phosphoric acid will produce plants
of another species, etc. Many soils produce certain
weeds which would not grow on them spontaneously
if they were fitted for the growth of better plants.
It is also believed that those weeds, which naturally
grow on the most fertile soils, are the ones most
easily destroyed. There are exceptions (of which
the Thistle is one), but this is given as a general rule.
By careful attention to the foregoing points,
weeds may be kept from increasing, while those
already in the soil may be eradicated in various
ways, chiefly by mechanical means, such as hoeing,
plowing, etc.
Prof. Mapes used to say, and experience often
shows, that six bushels of salt annually sown broad-
cast over each acre of land, will destroy very many
weeds, as well as grubs and worms.
The common hoe is a very imperfect tool for the
purpose of removing weeds, as it prepares a better
soil for, and replants in a position to grow, nearly as
many weeds as it destroys.
The scuffle-hoe (or push-hoe) is much more efiec-
tive, as, when worked by a man walking backward^
10
218 CULTIVATION.
and retiring as he works, it leaves nearly all of the
weeds on the surface of the soil to be killed by the
sun. When used in this way, the earth is not
trodden on after being hoed — as is the case when
the common hoe is employed. This treading, besides
compacting the soil, covers the roots of many weeds,
and causes them to grow again.
The scuffle-hoe, however, except in very light soil,
will not run so deeply as it is often desirable to
loosen it, and must, in such cases, be superseded by
ihQ prong-hoe (or potato-hook), which is a capital sub-
stitute for the common hoe in nearly all cases.
Much of the labor of weeding usually performed
by men, might be more cheaply done by horses.
There are various implements for this purpose, some
of which have come into very general use.
One of the best of these is the Langdon Harse
Hoe^ which is a shovel-shaped plow, to be run one
or two inches deep. It has a wing on each side to
prevent the earth from falling on to the plants in the
rows. At the rear, or upper edge, is a kind of rake
or comb, which allows the earth to pass through,
while the weeds pass over the comb and fall on the
surface of the soil, to be killed by the heat of the
sun. It is a simple and cheap tool, and will perform
the work of twenty men with hoes. The hand hoe
will be necessary only in the rows.
CULTIVATOES.
The cultivator^ which was described in the pre-
ceding chapter, and of which there are various pat-
CULTIVATION.
219
terns in nse, is excellent for weeding and for loosen-
ing the soil between the rows of corn, etc. The
one called the uTviversal cultivator, having its side
bars made of iron, curved so that at whatever dis-
tance it is placed the teeth will point straight for-
ward^ is a much better tool than those of the older
patterns, which had the teeth so arranged that when
set for wide rows, they pointed toward the clevis.
It is difficult to keep such a cultivator in its place,
while the " universal " is as difficult to move out of
a straight line.
IMPEOVED HOKSE-HOE.
The irnjproved (or Knox's) horse-hoe^ is a combina-
FiG. 7.
tion of the " Langdon " horse-hoe and the cultivator,
and is the best implement, for many purposes, that
has yet been made.
An excellent tool, called a Muller, is used in Rhode
220 CULTIVATION.
Island. It consists of a stick of heavy wood, five or
six feet long and about three inches by six inches in
size, drawn by fastening one trace to each end, having
stilts or handles rising from the upper side, and two
rows of sharpened iron teeth six inches long on the
under side — the front row of teeth point forward, and
the rear row backward. It is a " horse-rake" for the
ground, and leaves it as fine as a hand-rake would,
while it works it much more deeply.
One of the best cultivators that it is possible to use
between rows of corn — or other plants — is a small
sub-soil plow of the kind shown on p. 201, drawn by
one horse, and running five or six inches deep. It
mellows the land deeply and thoroughly.
There is much truth in the following proverbs :
" A garden that is well kept, is kept easily."
" You must conquer weeds, or weeds will conquer
you."
"The best time to kill weeds is before they come
up."
It is almost impossible to give a recapitulation of
the matters treated in this section, as it is, itself, but
an outline of subjects which might occupy our whole
book. The scholar and the farmer should understand
every principle which it contains as well as they un-
derstand the multiplication table ; and their applica-
tion will be found, in every instance, to produce the
best results.
CTJLTIYATION. 221
The two great rules of meclianical cultivation
are —
Thorough uNDER-DKAmiNG.
Deep and frequent disturbance of the soil.
SECTION FIFTH.
ANALYSIS
SECTM FIFTH.
ANALYSIS.
CHAPTER I.
. At the time when this book was first written, iii
1853, it was the very general opinion of scientific,
and of many practical, men, that it was within the
power of the chemist, by separating the different
parts of the soil, weighing each, to determine wheth-
er the soil were fertile or barren ; how long it might
continue fertile without the use of manure; what
manures were best suited to restoring or preserving
its fertility ; and what class of plants it was best fit-
ted to produce.
In this belief, these pages were devoted, very large-
ly, to showing the farmer how he could best regulate
his operations in the light of such teachings as soil
analysis gives.
As is often the case in the adoption of new discov-
eries, a further acquaintance with the subject showed
226 ANALYSIS.
that, so far as the processes of practical agriculture are
concerned, soil analysis is of but little, if any, value.
True, the amount of potash, for instance, which is
contained in the soil, may be determined with great
precision, and it seemed, at first, that this sort of
knowledge was enough for practical use ; but further
research and reasoning have shown that the question
of quantity is of no more consequence than the
question of condition. Of the potash in the soil
only the y^ or the -j-oV'o P^^'* ^^ available to the
plants of a single year's growth ; — why the other 99,
or 999 parts are not available, and how they may be
made so, the soil analysis, from which so much was
hoped for, does not tell us.
The causes of fertility and barrenness lie beyond
the reach of weight aiid measure, and it is an unfor-
tunate truth that, aside from a very simple indica-
tion of the internal character of our soils, the science
of chemistry can only help us in studying their char-
acter wlien we follow it through the by-ways of its
more subtle reasoning. Much of what is known of
the manner in which the soil gives nutriment to the
plant has been learned from the bringing together of
the results of many experiments, — studying them by
the light of what chemistry has positively taught.
This knowledge is of great value, and is sufficient
to §)rm the foundation of a really scientific agricul-
ture ; but there is no doubt that much more is yet to
be learned, and that we are still very far from know-
ing all that we must know of the use of manures,
the functions of the soil, and the growth of plants.
ANALYSIS. 227
While waiting for its further instruction, let us make
the best possible use of what chemistry now teaches
with certainty, in the analysis of the ashes of plants,
and of manures.
Practice and science have combined to show us
how all soils may be raised to a high, possibly to the
highest, state of fertility, and a knowledge of the
composition of crops and manures shows how we
may best maintain its good condition.
The one safe rule for all farmers to adopt is the
following : —
Always ketuen in the earthy constitubnts of
MANURE the FULL EQUIVALENT OF THE EARTHY CON-
STITUENTS OF THE CROP.
This will prevent the soil from deteriorating, and
we may safely trust to the process of cultivation, and
to the action of atmospheric influences, to make it
yearly better, by developing fresh supplies of its ash-
forming parts.
228
ANALYSIS.
CHAPTEH II.
TABLES OF ANALYSIS.
AJSTALYSES OF THE ASHES OE CKOPS.
No. I.
Wheat.
Wheat I -p^^
Straw. I ^y®-
Rye
Straw.
Ashes in 1000 dry parts
Silica (sand)
Lime
Magnesia
Peroxide of Iron
Potash
Soda
Chlorine
Sulphuric Acid
Phosphoric Acid
20
16
28
120
7
23t
91
3
498
60
654
67
83
13
124
~^ 2
11
58
31
24
5
50
104
14
221
116
10
496
40
645
91
24
14
174
3
5
8
38
No. II.
Corn.
Corn
Stalks.
Barley.
Barley
Straw.
Ashes in 1000 dry parts
Silica (sand)
Lime
Magnesia
Peroxide of Iron
Oxide of Manganese
Potash
Soda
Chlorine
Sulphuric Acid
Phosphoric Acid
15
15
15
162
8
261
63
2
23
449
44
270
86
66
8
96
277
20
5
171
28
271
26
75
15
136
81
1
1
389
61
706
95
32
7
1
62
6
10
16
31
ANALYSIS.
229
No. III.
Oats.
Oat
Straw.
Buck
Wheat.
Po-
tatoes,
Ashes in 1000 dry parts
20
51
21
90
Silica {sand)
7
60
99
4
i262f
3
104
438
484
81
38
18
191
97
32
33
27
7
67
104
11
87
201
22
500
42
Lime
21
Magnesia
53
Peroxide of Iron
5
Potash
557
Soda
19
Chlorine
43
Sulphuric Acid
137
Phosphoric Acid
126
Organic Matter
T50
Water.
No. lY.
Peas.
Beans.
Turnips.
Turnip
Tops.
Ashes in 1 000 dry parts
25
27
76
170
Silica (sand)
5
53
85
10
361
91
23
44
333
12
58
80
6
336
106
1^
378
71
128
48
9
398
108
37
131
67
870 Water.
8
233
Mao'nesia
81
Peroxide of Iron
8
Potash
286
Soda
54
160
Sulphuric Acid
125
PhnQnbnrio A fid . .......
93
Organic Matter
230
ANALYSIS.
No. y.
Ashes in 1000 dry parts
Silica (sand)
Aluraiaa (day)
Lime
Magnesia
Peroxide of Iron
Potash
Soda .
Chlorine
Sulphuric Acid
Phosphoric Acid
Flax.
50
257
37?
148
44
36?
117
118
29
32
130
Linseed.
46
75
83
146
9
240
45
2
23
865
Meadow
Hay.
60
344
196
78
7
236
19
28
29
68
Eed
Clover.
75
48
371
46
2
267
71
48
60
88
No. YI.
Amount of Inorganic Matter removed from the soil by ten bushels of
grains, etc., and by the straw, etc., required in their production
— estimated in pounds :
1620 Iba.
Rye
Straw.
11.34
.20
5.91
1.58
.88
.05
2.49
.30
42.25
66
Potash
Soda
Lime
Magnesia
Oxide of Iron . . . .
Sulphuric Acid. . .
Phosphoric Acid. .
Chlorine
Silica
Pounds carried oflf.
1200 lbs.
Wheat.
Wheat
Eye.
Straw.
2.86
8.97
2.51
1.04
.12
1.33
.34
4.84
.56
1.46
2.76
1.18
.08
.94
.15
.03
4.20
.11
6.01
2.22
.79
6.64
.14
47.16
.05
12
72
Hi
ANALYSIS.
231
No. VIL
Corn.
1620 lbs.
Corn
Stalks.
Oats.
700 lbs.
Oat
Straw.
Potash
2.78
.12
1.52
4.52
.06
6.84
19.83
6.02
4.74
.57
.36
12.15
1.33
19.16
1.69
.39
.64
.02
.66
2.80
.02
.18
12.08
Soda
Lime
Magnesia
3.39
1.59
Oxide of Iron
.78
Sulphuric Acid
1.41
Phosphoric Acid
1 07
Chlorine
136
Silica
20.32
Pounds carried off
9
71
H
42
No. VIII.
Potash
Soda
Lime
Magnesia
Oxide of Iron . . . .
Sulphuric Acid . .
Phosphoric Acid. .
Chlorine
Silica
Pounds carried off
Buck
Wheat.
1.01
2.13
,78
1.20
.14
.25
5.40
.09
11
Barley.
1.90
1.18
.96
LOO
.20
.01
6.35
.01
3.90
14
660 bbls.
Barley
Straw.
2.57
.23
3.88
1.81
.90
.66
1.25
.40
28.80
40
2000 lbs.
Flax.
11 78
11.82
11. «5
9.38
7.32
3.19
13.05
2.90
25.71
100
232
ANALYSIS.
No. IX
Beans.
1120 lbs.
Bean
Straw.
Field
Peas.
1366 lbs.
Pea
Straw.
Potash
5.54
1.83
98.98
.28
.10
.16
7.80
.13
.18
86.28
1.09
13.60
4.55
.20
.64
5.00
1.74
4.90
5.90
1.40
.81
1.30
.15
.64
5.50
.23
.7
3.78
Soda
Lime
43.93
Magnesia
6.50
Oxide of Iron
1.40
Sulphuric Acid
5.43
Phosphoric Acid ......
3.86
Chlorine
.08
Sihca
16.02
Pounds carried off
17
68
16
80
No. X.
Potash
Soda
Lime
Magnesia
Oxide of Iron. . . .
Sulphuric Acid. . .
Phosphoric Acid . .
Chlorine
Silica
Pounds carried off.
ITon
Turnips.
7.14
.86
2.31
.91
.23
2.30
L29
.61
1.36
Turnip
Tops.
4.34
.84
3.61
.48
.13
1.81
1.31
2.35
.13
ITon
Potatoes.
27.82
.93
1.03
2 63
.26
6.81
6 25
2.13
2.14
2000 lbs.
Red
Clover.
31.41
8.34
43.77
5.25
.23
7.05
10.28
5.86
5.81
17
15
50
118
ANALYSIS.
233
No. XI.
Potash
Soda
Lime
Magnesia
Oxide of Iron. . .
Sulphuric Acid. .
Phosphoric Acid
Chlorine
Silica
Pounds carried off.
2000 lbs.
2000 lbs.
Meadow
Cabbage.
Hay.
Water 9-10
18.11
5.25
1.35
9.20
22.95
9.45
6.75
2.70
1.69
.25
2.70
9.60
5.97
5.60
2.59
2.60
37.89
.35
:oo
45
No. XII.
Composition of Ashes, leached and unleached, showing their manurial
value :
Oak
unleached.
Oak
leached.
Beech
unleached.
Beech
leached.
Potash
84
56
750
45
6
12
35
548
6
8
158
29
634
113
8
14
31
2
Soda
Lime
426
Magnesia . .
70
Oxide of Iron
15
Sulphuric Acid
Phosphoric Acid
57
Chlorine
234
Al^ALYSIS.
No. XIII.
Potash
Soda
Lime
Magnesia
Oxide of Iron . .
Sulphuric Acid.
Phosphoric Acid
Chlorine
Birch
Seaweed
leached.
unleached.
180
210
522
94
30
99
5
3
248
43
52
^98
Bitumin-
ous Coal
unleached.
2
2
21
2
40
9
2
1
No. xiy.
TOBACCO.
Analysis of the ash of the Plant [Will & Fresenius] —
Potash 19.55
Soda 0.2'7
Magnesia 1 1.07
Lime 48.68
Phosphoric Acid ; , 3.66
Sulphuric Acid 3. 29
Oxide of Iron 2.99
Chloride of Sodium 3.54
Loss.... 6.95
100.00
Analysis of the ash of the Root [Berthier] —
Soluble Matter 12.8
Insoluble Matter ST.*?
The Soluble parts consist of nearly —
Carbonic Acid 10.0
Sulphuric Acid. 10.3
Muriatic Acid (Chlorine, &c.) 18.26
Potash and Soda 61.44
100.00
ANALYSIS.
235
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236
ANALYSIS.
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ANALYSIS.
237
No. XYII.
Amount of Ash left after burning 1000 lbs. of various plants, ordina-
rily dry:
its straw
Wheat
Barley
Oats
Rye
Indian Corn
Pea
Bean
Meadow Hay-
Clover
Rye Grass "
Potato
Turnip
Carrot
20
30
40
20
15
30
30
60
90
95
8
5
15
to 100
15
8
20
No. XVIII.
MANURES.
HOESE MANURE.
Solid Dung —
Combustible Matter 19.68
Ash 3.07
Water 77.25
Composition of the Ash— 10.000
Silica 62.40
Potash 11. .30
Soda 1.98
Oxide of Iron 1.17
Lime 4 63
Magnesia 3.84
Oxide of Manganese 2. 1 3
Phosphoric Acid 10.49
Sulphuric Acid 1.89
Chlorine 0.03
Loss , 0.14
100.00
238 ANALYSIS.
No. XIX.
NIGHT SOIL.
Solid (Ash) -
Earthy Phosphates, and a trace of Sulphate of Lime 100
Sulphate of Soda and Potash, and Phosphate of Soda. ... 8
Carbonate of Soda 8
Silica 16
Charcoal and Loss 18
150
Urine —
Urea* 30.10
Uric Acid 1.00
Sal Ammoniac* 1.50
Lactic Acid, etc 17.14
Mucus .32
Sulphate of Potash 3.71
Sulphate of Soda 3.16
Phosphate of Ammonia* 1.65
Earthy Phosphates 3.94
Salt (Chloride of Sodium) : 4.45
Silica 0.03
67.00
Water 983.00
1000.00
♦ Supply Ammonia.
No. XX.
cow MANURE.
Solid (Ash)—
Phosphates 20.9
Peroxide of Iron 8.8
Lime 1.5
Sulphate of Lime (Plaster) 3.1
Chloride of Potassium trace
Silica 63.7
Loss 2.0
100.0
ANALYSIS. 239
ItsTo. XXI.
COMPARATIVE YALTJE OP THT3 URINE OF DIFFERENT ANIMALS.
Solid Matter.
Organic. Inorgania Total.
Man 23.4 7.6 31
Horse 27. 83. 60
Cow 50. 20. 70
Pig 56. 18. 74
Sheep 28. 12. 40
No. XXII.
GUANO.
Water 6.40
Ammonia 2,71
Uric Acid 34.70
Oxalic Acid, etc 26.79
Fixed Alkaline Salts.
Sulphate of Soda 2.94
Phosphate of Soda 48
Chloride of Sodium (salt) 86
Earthy Salts.
Carbonate of Lime 1.36
Phosphates 19.24
Foreign Matter.
Silicious grit and sand 4.52
100.00
Composition of Fresh Farm-yard Manure, (composed of Horse, Pig,
and Cow Dung, about 14 days old). Analysis made Nov. 3d. 1854^
by Dr. Augustus Yoelcker, Professor of Chemistry in the Eoyal Ag-
ricultural College, Cirencester, England :
Water 66.17
Soluble Organic Matter 2.48
* Soluble Inorganic Matter (Ash) —
Soluble Silica (silicic acid) 237
Phosphate of Lime 299
Lime 066
Magnesia Oil
Potash 573
* Containing Nitrogen 149
Equal to Ammonia .181
2i0 ANALYSIS.
Chloride of Sodium 030
Carbonic Acid and loss 218
1.54
♦insoluble Organic Matter 25.76
Insoluble Inorganic Matter (Ash) —
Soluble Silica ( .,. . ..) 96*7
Insoluble Silica \ ''^^^^" ^^'^^ \ 561
Oxide of Iron, Alumina, with Phosphates 596
(Containing Phosphoric Acid, .118)
(Equal to bone earth, .386)
Lime 1.120
Magnesia , ., — ....... .143
Potash 099
Soda 019
Sulphuric Acid 061
Carbonic Acid and loss 484
4.05
100.00
According to this analysis one ton (2,000 lbs.) Farm-yard Manure con-
tains—
Soluble Silica (silicic acid) 24 lbs.
Ammonia (actual or potential) 15f
Phosphate of Lime 13^o
Lime 23jo
Magnesia. , — 3|o
Potash 13i
Soda If
Common Salt .".'; ^o
Sulphuric Acid 2^
Water 132:i|
Woody Fibre, etc 5*79
Of course no two samples of Farm-yard Manure are exactly of the
same composition. Tiiat analyzed by Dr. Voelcker was selected
-with much care, as representing a fair average.
GREEN SAND MARL ( OF NEW JERSEY).
Protoxide of Iron 15.5
Alumina 6.9
Lime 5.3
Magnesia 1.6
Potash 4.8
* Containing Nitrogen 494
Equal to Ammonia .599
The whole Manure contains Ammonia in a free state 034
» ' " " " in the form of salts 088
ANALYSIS. 241
Soluble Silica 32.4
Insoluble Silica and Sand 19.8
Sulphuric Acid 6
Phosphoric Acid 1.3
"Water 8.0
Carbonic Acid, etc 3.8
lOO.O
This is an average of three analyses copied from Prof. Geo. H. Cook's
report of the Geology of New Jersey. According to this estimate
one ton (2000 lbs.) of Green Sand Marl contains —
Lime 106 lbs.
Magnesia 32 "
Potash 96 "
Soluble Silicic Acid 648 "
Sulphuric Acid 12 "
Phosphoric Acid 26 "
(Equal to Phosphate of Lime 56^ lbs.)
For the analysis of fertile and barren soils, see page 63.
11
THE PRACTICAL FARMER,
THE PRACTICAL FARMER.
Who is \hQ practical farmer f Let us look at two
pictures and decide.
Here is a farm of 100 acres iu ordinary condition.
It is owned and tilled by a hard-working man, who,
in the busy season, employs one or two assistants.
The farm is free from debt, but it does not produce
an abundant income; therefore, its owner cannot
afford to purchase the best implements or make
other needed improvements ; besides, he don't
helieve in such things. His father was a good solid
farmer; so was his grandfather; and so is he, or
he thinks he is. He is satisfied that " the good old
way " is best, and he sticks to it. He works from
morning till night ; from spring till fall. In the
winter he rests, as much as his lessened duties will
allow. During this time, he reads little, or nothing.
Least of all does he read about farming. He don't
w^ant to learn how to dig potatoes out of a book.
Book farming is nonsense. Many other similar ideas
keep him from agricultural reading. His house is
comfortable, and his barns are quite as good as his
246 THE PRACTICAL FARMER.
neighbors', while his farm gives him a living. It
is true that his soil does not produce as much as it
did ten years ago ; but prices are better, and he is
satisfied.
Let us look at his premises, and see how his affairs
are managed. . First, examine the land. Well, it is
good fair land. Some of it is a little springy, but it
is not to be called loeb. When first laid down, it will
produce a ton and a half of hay to the acre — it used
to produce two tons. There are some stones on the
land, but not enough, in his estimation, to do harm.
The plowed fields are pretty good ; they will produce
35 bushels of corn, 13 bushels of wheat, or 30 bushels
of oats per acre, when the season is not dry. His
father used to get more ; but, somehow, the weather
is not so favorable as it was in old times. He ha^
thought of raising root crops, but they take more
labor than he can afford to hire. Over in the back
part of tlie land there is a muck-hole, which is the
only piece of worthless land on the whole farm.
ISTow, let us look at the barns and barn-yards.
The stables are pretty good. There are some wide
cracks in the siding, but they help to ventilate, and
make it healthier for the cattle. The manure is
thrown out of the back windows, and is left in piles
under the eaves of the barn. The rain and sun make
it nicer to handle. The cattle have to go some dis-
tance for water ; and this gives them exercise. All
of the cattle are not kept in the stable ; the fatten-
ing stock are kept in the various fields, where hay is
fed out to them from the stack. The barn-yard is
THE PKACTICAL FARMER. 247
often occupied by cattle, and is covered with their
manure, which lies there until it is carted on to the
land. In the shed are the tools of the farm, consist-
ing of carts, plows — not deep plows: this farmer
thinks it best to have roots near the surface of the
soil where they can have the benefit of the sun's heat,
— a harrow, hoes, rakes, etc. These tools are all in
good order; and, anlike those of his less prudent
neighbor, they are protected from the weather.
The crops are cultivated with the plow and hoe, as
they have been since the land was cleared, and as
they always will be until this man dies.
Here is the ' practical farmer ' of the present day-
Hard working, out of debt, and economical, — of dol-
lars and cents, if not of soil and manures. He is a
better farmer than two-thirds of the three million
farmers in the country. He is one of the best farm-
ers in his town — there are but few better in the
county, not many in the State. He represents the
better average class of his profession.
"With all this, he is, in matters relating to his busi-
ness, an unreading, unthinking man. He knows
nothing of the first principles of farming, and is suc-
cessful by the indulgence of nature, not because he
imderstands her, and is able to make the most of her
assistance.
This is an unpleasant fact, but it is one which
cannot be denied. We do not say this to disparage
the farmer, but to arouse him to a realization of his
position, and of his power to improve it.
But let us see where he is wrong.
248 THE PRACTICAL FAEMER.
He is wrong in thinking that his land does not
need draining. He is wrong in being satisfied with
one and a half tons of hay to the acre when he might
easily get two and a half. He is wrong in not
removing as far as possible every stone that can
interfere with the deep and thorough cultivation of
his soil. He is wrong in reaping less than his father
did, when he should get more. He is wrong in as-
cribing to the weather, and similar causes, what is
due to the actual impoverishment of his soil. He is
wrong in not raising turnips, carrots, and other
roots, which his winter stock so much need, when
they might be raised at a cost of less than one-third
of their value as food. He is wrong in considering
worthless a deposit of muck, which is a mine of
wealth if properly employed. He is wrong in
ventilating his stables at the cost of heat He is
wrong in his treatment of his manures, for he loses
more than one half of their value from evaporation,
fermentation, and leaching. He is wrong in not
having water at hand for his cattle — their exercise
detracts from their accumulation of fat and the
economy of their heat, and it exposes them to cold.
He is wrong in not protecting his fattening stock from
the cold of winter ; for, under exposure to cold, the
food, which would otherwise be used in the forma-
tion oifat, goes to the production of the animal heat
necessary to counteract the chilling influence of the
weather, p. 44. He is wrong in allowing his manure
to lie unprotected in the barn-yard. He is wrong
in not adding to his tools the deep surface plow, the
THE PRACTICAL FAKMEK. 249
sub-soil plow, the cultivator, and many other imple-
ments of improved construction. He is wrong in
cultivating with the plow and hoe, those crops which
could be better or more cheaply managed with the
cultivator or horse-hoe. He is wrong in many things
more, as we shall see if we examine all of his yearly
routine of work. He is right in a few things ; and
but a few, as he himself would admit, had he that
knowledge of his business which he could obtain in
the leisure hours of a single winter. Still he thinks
himself a practical farmer. In twenty years, we
shall have fewer such, for our young men have the
mental capacity and mental energy necessary to raise
them to the highest point of practical education, and
to that point they are gradually but surely rising.
We have far fewer now than twenty years ago.
Let us now place this same farm in the hands of
an educated and understanding cultivator; and at
the end of ^nq years, look at it again :
He has sold one half of it, and cultivates but fifty
acres. The money for which the other fifty were
sold has been used in the improvement of the farm.
The land has all been under-drained, and shows the
many improvements consequent on such treatment.
The stones and small rocks have been removed, leav-
ing the surface of the soil smooth, and allowing the
use of the sub-soil plow, which, with the under-drains,
has more than doubled the productive power of the
farm. Sufiicient labor is employed to cultivate with
improved tools, extensive root crops, and they invari-
ably give a large yield. The grass land produces a
11*
250 THE PEACTICAL FAKMEB.
yearly average of 2^ tons of hay per acre. From 80
to 100 bushels of corn, 30 bushels of wheat, and 45
bushels of oats are the average of the crops reaped.
The soil has been put in the best possible condition,
while it is regularly supplied with manures containing
everything taken away in the abundant crops. Tlie
principle that all earthy matters sold away must be
bought back again, is never lost sight of in the regu-
lation of crops and the application of manm'es. The
worthless muck-bed was retained, and is made worth
a dollar a load to the compost-heap, especially as the
land requires an increase of organic matter. A new
barn has been built large enough to store all of the
hay produced on the farm. It has stables, which
are tight and warm, and are well ventilated above the
cattle. The stock being thus protected from the
loss of their heat, give more milk, and make more
fat on a less amount of food than they did under the
old system. Water is near at hand, and the animals
are not obliged to over-exercise. The manure is
carefully composted, either under a shed constructed
for the pui-pose with a tank and pump, or is thrown
into the cellar below, where the hogs mix it with a
large amount of muck, which has been carted in
after being thoroughly decomposed by the lime and
salt mixture.
They are thus protected against all loss, and are
prepared for the immediate use of crops. 'No ma-
nures are allowed to lie in the barn-yard, but they
are all early removed to the compost heap, where
they are preserved by being mixed with carbona-
THE PK ACTIO AL FAEMEK. 251
ceous matter. In the tool shed, we find deep sur-
face-plows, sub-soil plows, cultivators, horse-hoes,
seed-drills, and many other valuable implements.
This farmer takes one or more agricultural papers,
from which he learns new methods of cultiva-
tion, while his knowledge of the reasons of various
agricultural effects enables him to discard the injudi-
cious suggestions of mere hook farmers and unedu-
cated dreamers.
Here are two specimen farmers. ITeither descrip-
tion is over-drawn. The first is much more care-
ful in his operations than the majority of our rural
population. The second is no better than many who
may be found in America.
"We appeal to the common sense of the reader of
this work to know which of the two is the jpraotical
farmer — let him imitate either, as his judgment
shall dictate.
FINIS.
EXPLANATION OF TERMS.
Absokb— to soak up a liquid or gas, or to take substances from
air or from watery solutions,
Abstbact— to take from.
Acid — sour ; a sour substance,
Agricultube — the art of cultivating- the soil.
Alkali — the direct opposite of an add^ with which it has a ten-
dency to unite.
Alumesta — the base of clay.
Analysis — separating into its primary parts any compound sub-
stance,
Cabbonate— ^a compoiind, consisting of carbonic acid and an
alkali.
Caustic — burning.
Chlobide — a compound containing chlorine.
CLEVis^that part of a plow by which the drawing power is at-
tached.
Decoimpose — to separate the constituents of a body from their
combinations, forming simple substances into new com-
pounds.
Digestion — the decomposition of food in the stomach and in-
testines of animals (agricultural).
Dew — deposit of the insensible vapor of the atmosphere on cold
surfaces,
ExcBEMENT — the matter given out by the organs of plants and
animals, being those parts of their food which they are una-
ble to assimilate.
Fermentation — a kind of decomposition.
Gas — air — aeriform matter.
Ingredient — component part.
254 EXPLANATION OF TERMS.
Inorganic — mineral, or earthy, not organized by animal or veg-
etable life.
MouLDBOARD — that part of the surface-plow which turns the
sod.
Mulching — covering the soil with litter, leaves, or other refuse
matter. See p. 212.
Neutralize — to overcome the characteristic properties or effects
of.
Organic Matter — that kind of matter which possesses or has
possessed an organized (or living) form.
Oxide — a compound of oxygen with a metal.
Phosphate — a compound of phosphoric acid with an alkali.
Pungent — pricking.
Putrefaction — rotting.
Saturate — to fU the pores of any substance, as a sponge with
water, or charcoal with ammonia.
Silicate — a compound of silicic acid with an alkali.
Soluble — capable of being dissolved.
Solution — a liquid containing another substance dissolved in it.
Saturated Solution — one which contains as much of the
foreign substance as it is capable of holding.
Spongioles — the absorbent ends of roots.
Sulphate — a compound of sulphuric acid with an alkali
Vapor — (see "gas").
!(r^