This question can now be satisfactorily answered: that effect is the

restoration of the elementary constituents of the soil which have

been gradually drawn from it in the shape of grain and cattle. If

the land I am speaking of had not been manured during those 16

years, not more than one-half, or perhaps than one-third part of the

carbon and nitrogen would have been produced. We owe it to the

animal excrements, that it equalled in production the meadow-land,

and this, because they restored the mineral ingredients of the soil

removed by the crops. All that the supply of manure accomplished,

was to prevent the land from becoming poorer in these, than the

meadow which produces 2,500 pounds of hay. We withdraw from the

meadow in this hay as large an amount of mineral substances as we do

in one harvest of grain, and we know that the fertility of the

meadow is just as dependent upon the restoration of these

ingredients to its soil, as the cultivated land is upon manures. Two

meadows of equal surface, containing unequal quantities of inorganic

elements of nourishment,--other conditions being equal,--are very

unequally fertile; that which possesses most, furnishes most hay. If

we do not restore to a meadow the withdrawn elements, its fertility

decreases. But its fertility remains unimpaired, with a due supply

of animal excrements, fluid and solid, and it not only remains the

same, but may be increased by a supply of mineral substances alone,

such as remain after the combustion of ligneous plants and other

vegetables; namely, ashes. Ashes represent the whole nourishment

which vegetables receive from the soil. By furnishing them in

sufficient quantities to our meadows, we give to the plants growing

on them the power of condensing and absorbing carbon and nitrogen by

their surface. May not the effect of the solid and fluid excrements,

which are the ashes of plants and grains, which have undergone

combustion in the bodies of animals and of man, be dependent upon

the same cause? Should not the fertility, resulting from their

application, be altogether independent of the ammonia they contain?

Would not their effect be precisely the same in promoting the

fertility of cultivated plants, if we had evaporated the urine, and

dried and burned the solid excrements? Surely the cerealia and

leguminous plants which we cultivate must derive their carbon and

nitrogen from the same source whence the graminea and leguminous

plants of the meadows obtain them! No doubt can be entertained of

their capability to do so.

In Virginia, upon the lowest calculation, 22 pounds weight of

nitrogen were taken on the average, yearly, from every morgen of the

wheat-fields. This would amount, in 100 years, to 2,200 pounds

weight. If this were derived from the soil, every morgen of it must

have contained the equivalent of 110,000 pounds weight of animal

excrements (assuming the latter, when dried, at the temperature of

boiling water, to contain 2 per cent.).

In Hungary, as I remarked in a former Letter, tobacco and wheat have

been grown upon the same field for centuries, without any supply of

nitrogenised manure. Is it possible that the nitrogen essential to,

and entering into, the composition of these crops, could have been

drawn from the soil?

Every year renews the foliage and fruits of our forests of beech,

oak, and chesnuts; the leaves, the acorns, the chesnuts, are rich in

nitrogen; so are cocoa-nuts, bread-fruit, and other tropical

productions. This nitrogen is not supplied by man, can it indeed be

derived from any other source than the atmosphere?

In whatever form the nitrogen supplied to plants may be contained in

the atmosphere, in whatever state it may be when absorbed, from the

atmosphere it must have been derived. Did not the fields of Virginia

receive their nitrogen from the same source as wild plants?

Is the supply of nitrogen in the excrements of animals quite a

matter of indifference, or do we receive back from our fields a

quantity of the elements of blood corresponding to this supply?

The researches of Boussingault have solved this problem in the most

satisfactory manner. If, in his grand experiments, the manure which

he gave to his fields was in the same state, i.e. dried at 110 deg

in a vacuum, as it was when analysed, these fields received, in 16

years, 1,300 pounds of nitrogen. But we know that by drying all the

nitrogen escapes which is contained in solid animal excrements, as

volatile carbonate of ammonia. In this calculation the nitrogen of

the urine, which by decomposition is converted into carbonate of

ammonia, has not been included. If we suppose it amounted to half as

much as that in the dried excrements, this would make the quantity

of nitrogen supplied to the fields 1,950 pounds.

In 16 years, however, as we have seen, only 1,517 pounds of

nitrogen, was contained in their produce of grain, straw, roots, et

cetera--that is, far less than was supplied in the manure; and in

the same period the same extent of surface of good meadow-land (one

hectare = a Hessian morgen), which received no nitrogen in manure,

2,062 pounds of nitrogen.

It is well known that in Egypt, from the deficiency of wood, the

excrement of animals is dried, and forms the principal fuel, and

that the nitrogen from the soot of this excrement was, for many

centuries, imported into Europe in the form of sal ammoniac, until a

method of manufacturing this substance was discovered at the end of

the last century by Gravenhorst of Brunswick. The fields in the

delta of the Nile are supplied with no other animal manures than the

ashes of the burnt excrements, and yet they have been proverbially

fertile from a period earlier than the first dawn of history, and

that fertility continues to the present day as admirable as it was

in the earliest times. These fields receive, every year, from the

inundation of the Nile, a new soil, in its mud deposited over their

surface, rich in those mineral elements which have been withdrawn by

the crops of the previous harvest. The mud of the Nile contains as

little nitrogen as the mud derived from the Alps of Switzerland,

which fertilises our fields after the inundations of the Rhine. If

this fertilising mud owed this property to nitrogenised matters;

what enormous beds of animal and vegetable exuviae and remains ought

to exist in the mountains of Africa, in heights extending beyond the

limits of perpetual snow, where no bird, no animal finds food, from

the absence of all vegetation!

Abundant evidence in support of the important truth we are

discussing, may be derived from other well known facts. Thus, the

trade of Holland in cheese may be adduced in proof and illustration

thereof. We know that cheese is derived from the plants which serve

as food for cows. The meadow-lands of Holland derive the nitrogen of

cheese from the same source as with us; i.e. the atmosphere. The

milch cows of Holland remain day and night on the grazing-grounds,

and therefore, in their fluid and solid excrements return directly

to the soil all the salts and earthy elements of their food: a very

insignificant quantity only is exported in the cheese. The fertility

of these meadows can, therefore, be as little impaired as our own

fields, to which we restore all the elements of the soil, as manure,

which have been withdrawn in the crops. The only difference is, in

Holland they remain on the field, whilst we collect them at home and

carry them, from time to time, to the fields.

The nitrogen of the fluid and solid excrements of cows, is derived

from the meadow-plants, which receive it from the atmosphere; the

nitrogen of the cheese also must be drawn from the same source. The

meadows of Holland have, in the lapse of centuries, produced

millions of hundredweights of cheese. Thousands of hundredweights

are annually exported, and yet the productiveness of the meadows is

in no way diminished, although they never receive more nitrogen than

they originally contained.

Nothing then can be more certain than the fact, that an exportation

of nitrogenised products does not exhaust the fertility of a

country; inasmuch as it is not the soil, but the atmosphere, which

furnishes its vegetation with nitrogen. It follows, consequently,

that we cannot increase the fertility of our fields by a supply of

nitrogenised manure, or by salts of ammonia, but rather that their

produce increases or diminishes, in a direct ratio, with the supply

of mineral elements capable of assimilation. The formation of the

constituent elements of blood, that is, of the nitrogenised

principles in our cultivated plants, depends upon the presence of

inorganic matters in the soil, without which no nitrogen can be

assimilated even when there is a most abundant supply. The ammonia

contained in animal excrements exercises a favourable effect,

inasmuch as it is accompanied by the other substances necessary to

accomplish its transition into the elements of the blood. If we

supply ammonia associated with all the conditions necessary to its

assimilation, it ministers to the nourishment of the plants; but if

this artificial supply is not given they can derive all the needed

nitrogen from the atmosphere--a source, every loss from which is

restored by the decomposition of the bodies of dead animals and the

decay of plants. Ammonia certainly favours, and accelerates, the

growth of plants in all soils, wherein all the conditions of its

assimilation are united; but it is altogether without effect, as

respects the production of the elements of blood where any of these

conditions are wanting. We can suppose that asparagin, the active

constituent of asparagus, the mucilaginous root of the marsh-mallow,

the nitrogenised and sulphurous ingredients of mustard-seed, and of

all cruciferous plants, may originate without the aid of the mineral

elements of the soil. But if the principles of those vegetables,

which serve as food, could be generated without the co-operation of

the mineral elements of blood, without potash, soda, phosphate of

soda, phosphate of lime, they would be useless to us and to

herbivorous animals as food; they would not fulfil the purpose for

which the wisdom of the Creator has destined them. In the absence of

alkalies and the phosphates, no blood, no milk, no muscular fibre

can be formed. Without phosphate of lime our horses, sheep and

cattle, would be without bones.

In the urine and in the solid excrements of animals we carry

ammonia, and, consequently, nitrogen, to our cultivated plants, and

this nitrogen is accompanied by all the mineral elements of food

exactly in the same proportions, in which both are contained in the

plants which served as food to the animals, or what is the same, in

those proportions in which both can serve as nourishment to a new

generation of plants, to which both are essential.

The effect of an artificial supply of ammonia, as a source of

nitrogen, is, therefore, precisely analogous to that of humus as a

source of carbonic acid--it is limited to a gain of time; that is,

it accelerates the development of plants. This is of great

importance, and should always be taken into account in gardening,

especially in the treatment of the kitchen-garden; and as much as

possible, in agriculture on a large scale, where the time occupied

in the growth of the plants cultivated is of importance.

When we have exactly ascertained the quantity of ashes left after

the combustion of cultivated plants which have grown upon all

varieties of soil, and have obtained correct analyses of these

ashes, we shall learn with certainty which of the constituent

elements of the plants are constant and which are changeable, and we

shall arrive at an exact knowledge of the sum of all the ingredients

we withdraw from the soil in the different crops.

With this knowledge the farmer will be able to keep an exact record,

of the produce of his fields in harvest, like the account-book of a

well regulated manufactory; and then by a simple calculation he can

determine precisely the substances he must supply to each field, and

the quantity of these, in order to restore their fertility. He will

be able to express, in pounds weight, how much of this or that

element he must give in order to augment its fertility for any given

kind of plants.

These researches and experiments are the great desideratum of the

present time. TO THE UNITED EFFORTS OF THE CHEMISTS OF ALL COUNTRIES

WE MAY CONFIDENTLY LOOK FOR A SOLUTION OF THESE GREAT QUESTIONS, and

by the aid of ENLIGHTENED AGRICULTURISTS we shall arrive at a

RATIONAL system of GARDENING, HORTICULTURE, and AGRICULTURE,

applicable to every country and all kinds of soil, and which will be

based upon the immutable foundation of OBSERVED FACTS and

PHILOSOPHICAL INDUCTION.

LETTER XVI

My dear Sir,

My recent researches into the constituent ingredients of our

cultivated fields have led me to the conclusion that, of all the

elements furnished to plants by the soil and ministering to their

nourishment, the phosphate of lime--or, rather, the phosphates

generally--must be regarded as the most important.

In order to furnish you with a clear idea of the importance of the

phosphates, it may be sufficient to remind you of the fact, that the

blood of man and animals, besides common salt, always contains

alkaline and earthy phosphates. If we burn blood and examine the

ashes which remain, we find certain parts of them soluble in water,

and others insoluble. The soluble parts are, common salt and

alkaline phosphates; the insoluble consist of phosphate of lime,

phosphate of magnesia, and oxide of iron.

These mineral ingredients of the blood--without the presence of

which in the food the formation of blood is impossible--both man and

animals derive either immediately, or mediately through other

animals, from vegetable substances used as food; they had been

constituents of vegetables, they had been parts of the soil upon

which the vegetable substances were developed.

If we compare the amount of the phosphates in different vegetable

substances with each other, we discover a great variety, whilst

there is scarcely any ashes of plants altogether devoid of them, and

those parts of plants which experience has taught us are the most

nutritious, contain the largest proportion. To these belong all

seeds and grain, especially the varieties of bread-corn, peas,

beans, and lentils.

It is a most curious fact that if we incinerate grain or its flour,

peas, beans, and lentils, we obtain ashes, which are distinguished

from the ashes of all other parts of vegetables by the absence of

alkaline carbonates. The ashes of these seeds when recently

prepared, do not effervesce with acids; their soluble ingredients

consist solely of alkaline phosphates, the insoluble parts of

phosphate of lime, phosphate of magnesia, and oxide of iron:

consequently, of the very same salts which are contained in blood,

and which are absolutely indispensable to its formation. We are thus

brought to the further indisputable conclusion that no seed suitable

to become food for man and animals can be formed in any plant

without the presence and co-operation of the phosphates. A field in

which phosphate of lime, or the alkaline phosphates, form no part of

the soil, is totally incapable of producing grain, peas, or beans.

An enormous quantity of these substances indispensable to the

nourishment of plants, is annually withdrawn from the soil and

carried into great towns, in the shape of flour, cattle, et cetera.

It is certain that this incessant removal of the phosphates must

tend to exhaust the land and diminish its capability of producing

grain. The fields of Great Britain are in a state of progressive

exhaustion from this cause, as is proved by the rapid extension of

the cultivation of turnips and mangel wurzel--plants which contain

the least amount of the phosphates, and therefore require the

smallest quantity for their development. These roots contain 80 to

92 per cent. of water. Their great bulk makes the amount of produce

fallacious, as respects their adaptation to the food of animals,

inasmuch as their contents of the ingredients of the blood, i.e. of

substances which can be transformed into flesh, stands in a direct

ratio to their amount of phosphates, without which neither blood nor

flesh can be formed.

Our fields will become more and more deficient in these essential

ingredients of food, in all localities where custom and habits do

not admit the collection of the fluid and solid excrements of man,

and their application to the purposes of agriculture. In a former

letter I showed you how great a waste of phosphates is unavoidable

in England, and referred to the well-known fact that the importation

of bones restored in a most admirable manner the fertility of the

fields exhausted from this cause. In the year 1827 the importation

of bones for manure amounted to 40,000 tons, and Huskisson estimated

their value to be from L 100,000 to L 200,000 sterling. The

importation is still greater at present, but it is far from being

sufficient to supply the waste.

Another proof of the efficacy of the phosphates in restoring

fertility to exhausted land is afforded by the use of the guano--a

manure which, although of recent introduction into England, has

found such general and extensive application.

We believe that the importation of one hundred-weight of guano is

equivalent to the importation of eight hundred-weight of wheat--the

hundred-weight of guano assumes in a time which can be accurately

estimated the form of a quantity of food corresponding to eight

hundred-weight of wheat. The same estimate is applicable in the

valuation of bones.

If it were possible to restore to the soil of England and Scotland

the phosphates which during the last fifty years have been carried

to the sea by the Thames and the Clyde, it would be equivalent to

manuring with millions of hundred-weights of bones, and the produce

of the land would increase one-third, or perhaps double itself, in

five to ten years.

We cannot doubt that the same result would follow if the price of

the guano admitted the application of a quantity to the surface of

the fields, containing as much of the phosphates as have been

withdrawn from them in the same period.

If a rich and cheap source of phosphate of lime and the alkaline

phosphates were open to England, there can be no question that the

importation of foreign corn might be altogether dispensed with after

a short time. For these materials England is at present dependent

upon foreign countries, and the high price of guano and of bones

prevents their general application, and in sufficient quantity.

Every year the trade in these substances must decrease, or their

price will rise as the demand for them increases.

According to these premises, it cannot be disputed, that the annual

expense of Great Britain for the importation of bones and guano is

equivalent to a duty on corn: with this difference only, that the

amount is paid to foreigners in money.

To restore the disturbed equilibrium of constitution of the

soil,--to fertilise her fields,--England requires an enormous supply

of animal excrements, and it must, therefore, excite considerable

interest to learn, that she possesses beneath her soil beds of

fossil guano, strata of animal excrements, in a state which will

probably allow of their being employed as a manure at a very small

expense. The coprolithes discovered by Dr. Buckland, (a discovery of

the highest interest to Geology,) are these excrements; and it seems

extremely probable that in these strata England possesses the means

of supplying the place of recent bones, and therefore the principal

conditions of improving agriculture--of restoring and exalting the

fertility of her fields.

In the autumn of 1842, Dr. Buckland pointed out to me a bed of

coprolithes in the neighbourhood of Clifton, from half to one foot

thick, inclosed in a limestone formation, extending as a brown

stripe in the rocks, for miles along the banks of the Severn. The

limestone marl of Lyme Regis consists, for the most part, of

one-fourth part of fossil excrements and bones. The same are

abundant in the lias of Bath, Eastern and Broadway Hill, near

Evesham. Dr. Buckland mentions beds, several miles in extent, the

substance of which consists, in many places, of a fourth part of

coprolithes.

Pieces of the limestone rock in Clifton, near Bristol, which is rich

in coprolithes and organic remains, fragments of bones, teeth, &c.,

were subjected to analysis, and were found to contain above 18 per

cent. of phosphate of lime. If this limestone is burned and brought

in that state to the fields, it must be a perfect substitute for

bones, the efficacy of which as a manure does not depend, as has

been generally, but erroneously supposed, upon the nitrogenised

matter which they contain, but on their phosphate of lime.

The osseous breccia found in many parts of England deserves especial

attention, as it is highly probable that in a short time it will

become an important article of commerce.

What a curious and interesting subject for contemplation! In the

remains of an extinct animal world, England is to find the means of

increasing her wealth in agricultural produce, as she has already

found the great support of her manufacturing industry in fossil

fuel,--the preserved matter of primeval forests,--the remains of a

vegetable world. May this expectation be realised! and may her

excellent population be thus redeemed from poverty and misery!

End of Project Gutenberg's Familiar Letters of Chemistry, by Justus Liebig

Familiar Letters on Chemistry, and Its Relation to Commerce, Physiology, and Agriculture · 第 8 / 8 段