CHAPTER VIII.

THE COMPOSITION AND PROPERTIES OF FARM-YARD AND LIQUID MANURES.

In the preceding chapter, a general manure has been defined as one

containing all the constituents of the crop to which it is to be

applied, in a state fitted for assimilation. This condition is fulfilled

only by substances derived from the vegetable and animal kingdoms, and

most effectually by a mixture of both. On this account, and also because

its properties are such as enable it to act powerfully on the soil,

farm-yard manure must always be of the highest importance. It is, in

fact, the typical manure, and in proportion as other substances approach

it in properties and composition, is their value for general purposes on

the farm.

Farm-yard manure is a mixture of the dung and urine of domestic animals,

with the straw used as litter; and its value and composition must

necessarily depend upon that of these substances, as well as on the

proportion in which they are mixed. The dung of animals consists of that

part of their food which passes through the intestinal canal without

undergoing assimilation; the urine containing the portion which has been

assimilated and is again excreted, in consequence of the changes which

are proceeding in the tissues of the animal. Their composition is

naturally very different, and must be separately considered.

_Urine._--Urine consists of a variety of earthy and alkaline salts, and

of certain organic substances, generally rich in nitrogen, dissolved in

a large quantity of water. That of the different domestic animals has

been frequently examined, but the analyses of Fromberg give the most

complete view of their manurial value:--

Horse. Swine. Ox. Goat. Sheep.

Extractive matter } 2.132 0.142 2.248 0.100 0.340

soluble in water }

Extractive matter } 2.550 0.387 1.421 0.454 3.330

soluble in spirit}

Salts soluble in } 2.340 0.909 2.442 0.850 1.957

water }

Salts insoluble in} 1.880 0.088 0.155 0.080 0.052

water }

Urea 1.244 0.273 1.976 0.378 1.262

Hippuric acid 1.260 ... 0.550 0.125 ...

Mucus 0.005 0.005 0.007 0.006 0.025

Water 88.589 98.196 91.201 98.007 92.897

------ ------- ------- ------- -------

100.000 100.000 100.000 100.000 99.863

_Composition of the Ash of these Urines._

Horse. Swine. Ox. Goat. Sheep.

Carbonate of lime 12.50 ... 1.07 trace 0.82

Carbonate of magnesia 9.46 ... 6.93 7.3 0.46

Carbonate of potash 46.09 12.10 77.28 trace ...

Carbonate of soda 10.33 ... ... 53.0 42.25

Sulphate of potash ... ... 13.30 ... 2.98

Sulphate of soda 13.04 7.00 ... 25.0 7.72

Phosphate of soda ... 19.00 ... ... ...

Phosphate of lime }

Phosphate of magnesia } ... 8.80 ... ... 0.70

Chloride of sodium 6.94 53.10 0.30 14.7 32.01

Chloride of potassium ... trace ... ... 12.00

Silica 0.55 ... 0.35 ... 1.06

Oxide of iron and loss 1.09 ... 0.77 ... ...

------ ------ ------ ------ ------

100.00 100.00 100.00 100.00 100.00

Human urine has been accurately examined by Berzelius, although his

estimate of the proportion of urea is generally admitted to be above the

average. His analysis gives the following numbers:--

Natural. Dry Residue.

Urea 3.010 44.70

Lactic acid, lactate of ammonia,} 1.714 25.58

and extractive matter }

Uric acid 0.100 1.49

Mucus 0.032 0.48

Sulphate of potash 0.371 5.54

Sulphate of soda 0.316 4.72

Phosphate of soda 0.294 4.39

Biphosphate of ammonia 0.165 2.46

Chloride of sodium 0.445 6.64

Muriate of ammonia 0.150 2.46

Phosphates of magnesia and lime 0.100 1.49

Silica 0.003 0.05

Water 93.300

------- ------

100.000 100.00

Among the special organic constituents of the urine are three

substances, urea, uric acid, and hippuric acid, which are of much

importance in a manurial point of view. The first of these is found in

considerable quantity in the urine of all animals, but is especially

abundant in the carnivora. Uric acid is found only in these animals, and

is the most remarkable constituent of the excrement of birds, serpents,

and many of the lower animals. Hippuric acid is most abundant in the

herbivora. These substances are all highly nitrogenous. They contain--

Urea. Uric Acid. Hippuric Acid.

Carbon 20.00 36.0 60.7

Hydrogen 6.60 2.4 5.0

Nitrogen 46.70 33.4 8.0

Oxygen 26.70 28.2 26.3

------ ----- -----

100.00 100.0 100.0

They are extremely prone to change, and in presence of animal matters

readily ferment, and are converted into salts of ammonia. Thus human

urine, which, at the time of emission is free from smell of ammonia, and

has a slightly acid reaction, becomes highly ammoniacal if it be kept

for a few days. This is due to the conversion of urea into carbonate of

ammonia; and the same change takes place, though more slowly, with uric

and hippuric acids.

It is obvious, from the foregoing analyses, that great differences must

exist in the manurial value of the urine of different animals. Not only

do they vary greatly in the proportion of solid matters which they

contain, but also in the kind and quantity of their nitrogenous

constituents. They differ also in regard to their saline ingredients;

and while salts of potash and soda form the principal part of the ash of

the urine of the ox, sheep, goat, and horse, and phosphoric acid and

phosphates are entirely absent, that of the pig contains a considerable

quantity of the latter substances, and in this respect more nearly

resembles the urine of man. Human urine is also much richer in urea and

nitrogenous constituents generally, and has a higher value than any of

the others.

It is especially worthy of notice that the urine of the purely

herbivorous animals (with the exception of the sheep, which contains a

small quantity), are devoid of phosphates and urea; and consequently,

when employed alone, they are not general manures--a matter of some

importance in relation to the subject of liquid manuring, which will be

afterwards discussed.

_Dung._--The solid excrement of animals is equally variable in

composition. That of the domestic animals which had the ordinary winter

food was found to have the following composition:--

Horse. Cow. Sheep. Swine.

Per-centage of water in the } 77.25 82.45 56.47 77.13

fresh excrement }

Ash in the dry excrement 13.36 15.23 13.49 37.17

100 parts of ash contained--

Horse. Cow. Sheep. Swine.

Silica 62.40 62.54 50.11 13.19

Potash 11.30 2.91 8.32 3.60

Soda 1.98 0.98 3.28 3.44

Chloride of sodium 0.03 0.23 0.14 0.89

Phosphate of iron 2.73 8.93 3.98 10.55

Lime 4.63 5.71 18.15 2.63

Magnesia 3.84 11.47 5.45 2.24

Phosphoric Acid 8.93 4.75 7.52 0.41

Sulphuric acid 1.83 1.77 2.69 0.90

Carbonic acid ... trace trace 0.60

Oxide of manganese 2.13 ... ... ...

Sand ... ... ... 61.37

---- ---- ---- ----

99.80 99.29 99.64 99.82

Human faeces contain about 75 per cent of water; and their dry residue

was found by Way to have the following composition:--

Organic matter 88.52

Insoluble siliceous matters 1.48

Oxide of iron 0.54

Lime 1.72

Magnesia 1.55

Phosphoric acid 4.27

Sulphuric acid 0.24

Potash 1.19

Soda 0.31

Chloride of sodium 0.18

------

100.00

In a sample analyzed by myself there were found--

Organic matter 86.75

Phosphates 8.19

Alkaline salts, containing 1.18 of phosphoric } 2.53

acid }

Insoluble matters 2.53

------

100.00

Nitrogen 4.59

Equal to ammonia 5.57

It is to be observed that the urine and dung of animals differ

conspicuously in the composition of their ash, the former being

characterized by the abundance of alkaline salts, while the latter

contains these substances in small proportion, but is rich in earthy

matters, and especially in phosphoric acid. Salts of potash, for

example, form nine-tenths of the inorganic part of the urine of the ox,

while less than three per cent of that alkali is found in its dung.

Phosphoric acid, on the other hand, is not met with in the urine, but

forms about ten per cent of the dung. Silica is the most abundant

constituent of the dung, but a large proportion of that found on

analysis has been swallowed in the shape of grains of sand and particles

of soil mechanically mixed with the food, although part is also derived

from the straw and grains, which contain that substance in great

abundance. The difference in the quantity of nitrogen they contain is

also very marked, and is distinctly shown by the following analyses by

Boussingault, which give the quantity of carbon, hydrogen, nitrogen,

oxygen, and ash in the dung and urine of the horse and the cow in their

natural state, and after drying at 212 deg..

+---------+--------------------------+--------------------------+

| | HORSE. | COW. |

| +-------------+------------+-------------+------------+

| | Natural. | Dry. | Natural. | Dry. |

| +-------------+------------+-------------+------------+

| |Urine.| Dung.|Urine.|Dung.|Urine.| Dung.|Urine.|Dung.|

| +------+------+------+-----+------+------+------+-----+

|Carbon | 4.46| 9.56| 36.0| 38.7| 3.18| 4.02| 27.2| 42.8|

|Hydrogen | 0.47| 1.26| 3.8| 5.1| 0.30| 0.49| 2.6| 5.2|

|Nitrogen | 1.55| 0.54| 12.5| 2.2| 0.44| 0.22| 3.8| 2.3|

|Oxygen | 1.40| 9.31| 11.3| 37.7| 3.09| 3.54| 26.4| 37.7|

|Ash | 4.51| 4.02| 36.4| 16.3| 4.68| 1.13| 40.0| 12.0|

|Water | 87.61| 75.31| 0.0| 0.0| 88.31| 90.60| 0.0| 0.0|

| +------+------+------+-----+------+------+------+-----+

| |100.00|100.00| 100.0|100.0|100.00|100.00| 100.0|100.0|

+---------+------+------+------+-----+------+------+------+-----+

Hence, weight for weight, the urine of the horse, in its natural state,

contains three times as much nitrogen as its dung; that of the cow twice

as much; and the difference, especially in the horse, is still more

conspicuous when they are dry.

It is obvious that the quality of farm-yard manure must depend--1. On

the kind of animal from which it is produced; 2. On the quantity of

straw which has been used as litter; 3. On the nature of the food with

which the animals have been supplied; 4. On the extent to which its

valuable constituents have been rendered available by the treatment to

which it has been subjected; and 5. On the care which has been taken to

prevent the escape of the urine, or of the ammonia produced by its

decomposition.

The composition of farm-yard manure has engaged the attention of several

chemists; but there are still many points on which our information

regarding it is less complete than might be desired. Its investigation

is surrounded with peculiar difficulties, not merely on account of its

complexity, but because its properties render it exceedingly difficult

to obtain a sample which fairly represents its average composition. In

the case of long dung, these difficulties are so great that it is

scarcely possible to overcome them; and hence, discrepancies are

occasionally to be met with in the analyses of the most careful

experimenters. The most minute and careful analyses yet made are those

of Voelcker, who has compared the composition of fresh and rotten dung,

and studied the changes which the former undergoes when preserved in

different ways. He employed in his experiments both fresh and rotten

dung, and subjected them to different methods of treatment. His analyses

are given in the accompanying table, in which column 1 gives the

composition of fresh long dung, composed of cow and pig dung. 2. Is dung

of the same kind, after having lain in a heap against a wall, but

otherwise unprotected from the weather for three months and eleven days

in winter, during which time little rain fell. 3. The same manure, kept

for the same time under a shed. 4. Well rotten dung, which had been kept

in the manure heap upwards of six months. 5. The same, after having lain

against a wall for two months and nine days longer.

+-------------------------------+-------------+-------------+--------------+

| | 1 | 2 | 3 |

+-------------------------------+-------------+-------------+--------------+

| Water | 66.17 | 69.86 | 67.32 |

| Soluble organic matters | 2.48 | 3.86 | 2.63 |

| Soluble inorganic matters. | | | |

| Silica | 0.237 | 0.279 | 0.239 |

| Phosphate of lime | 0.299 | 0.300 | 0.331 |

| Lime | 0.066 | 0.048 | 0.056 |

| Magnesia | 0.011 | 0.019 | 0.004 |

| Potash | 0.573 | 1.096 | 0.676 |

| Soda | 0.051 | 0.187 | 0.192 |

| Chloride of sodium | 0.030 | 0.106 | 0.058 |

| Sulphuric acid | 0.055 | 0.160 | 0.119 |

| Carbonic acid and loss | 0.218 | 0.775 | 0.445 |

| | ----- 1.54 | ... 2.97 | ----- 2.12 |

| | | | |

| Insoluble organic matters | 25.76 | 18.44 | 20.46 |

| Insoluble inorganic matters-- | | | |

| Soluble silica | 0.967 | 0.712 | 1.893 |

| Insoluble silica | 0.561 | 0.857 | 1.075 |

| Oxide of iron, alumina, and | | | |

| phosphates | 0.596 | 0.810 | 1.135 |

+-------------------------------+-------------+-------------+--------------+

+-------------------------------+-------------+-------------+

| | 4 | 5 |

+-------------------------------+-------------+-------------+

| Water | 75.42 | 73.90 |

| Soluble organic matters | 3.71 | 2.70 |

| Soluble inorganic matters | | |

| Silica | 0.254 | 0.147 |

| Phosphate of lime | 0.382 | 0.129 |

| Lime | 0.117 | 0.018 |

| Magnesia | 0.047 | 0.018 |

| Potash | 0.446 | 0.960 |

| Soda | 0.023 | 0.082 |

| Chloride of sodium | 0.037 | 0.052 |

| Sulphuric acid | 0.058 | 0.072 |

| Carbonic acid and loss | 0.106 | 0.584 |

| | ----- 1.47 | ----- 2.06 |

| | | |

| Insoluble organic matters | 12.82 | 14.39 |

| Insoluble inorganic matters-- | | |

| Soluble silica | 1.424 | 1.10 |

| Insoluble silica | 1.010 | 1.54 |

| Oxide of iron, alumina, and | | |

| phosphates | 0.947 | 0.37 |

+-------------------------------+-------------+-------------+

+-------------------------------+-------------+-------------+--------------+

| | 1 | 2 | 3 |

+-------------------------------+-------------+-------------+--------------+

| Containing phosphoric acid |(0.178) |(0.177) |(0.298) |

| Equal to bone earth |(0.386) |(0.277) |(0.646) |

| Lime | 1.120 | 1.291 | 1.868 |

| Magnesia | 0.143 | 1.029 | 0.078 |

| Potash | 0.099 | 0.127 | 0.208 |

| Soda | 0.019 | 0.046 | 0.038 |

| Sulphuric acid | 0.061 | 0.099 | 0.098 |

| Carbonic acid and loss | 0.484 | 0.929 | 1.077 |

| | ----- 4.05 | ----- 4.90 | ----- 7.47 |

| | ----- | ----- | ------ |

| | 100.00 | 100.00 | 100.00 |

| | | | |

| Containing nitrogen | 0.149 | 0.270 | 0.170 |

| Equal to ammonia | 0.181 | 0.320 | 0.206 |

| Containing nitrogen | 0.494 | 0.470 | 0.580 |

| Equal to ammonia | 0.599 | 0.570 | 0.700 |

| Total nitrogen | 0.643 | 0.740 | 0.750 |

| Equal to ammonia | 0.780 | 0.890 | 0.906 |

+-------------------------------+-------------+-------------+--------------+

+-------------------------------+-------------+-------------+

| | 4 | 5 |

+-------------------------------+-------------+-------------+

| Containing phosphoric acid |(0.274) |(0.06) |

| Equal to bone earth |(0.573) |(0.10) |

| Lime | 1.667 | 2.25 |

| Magnesia | 0.091 | 0.02 |

| Potash | 0.045 | 0.12 |

| Soda | 0.038 | 0.01 |

| Sulphuric acid | 0.063 | 0.10 |

| Carbonic acid and loss | 1.295 | 1.44 |

| |----- 6.58 | ---- 6.95 |

| | ----- | ------ |

| | 100.00 | 100.00 |

| | | |

| Containing nitrogen | 0.297 | 0.149 |

| Equal to ammonia | 0.360 | 0.180 |

| Containing nitrogen | 0.309 | 0.613 |

| Equal to ammonia | 0.375 | 0.744 |

| Total nitrogen | 0.606 | 0.762 |

| Equal to ammonia | 0.735 | 0.924 |

+-------------------------------+-------------+-------------+

On examining and comparing these analyses, it appears that the

differences are by no means great, although, on the whole, they tend to

show that, weight for weight, well-rotten dung is superior to fresh,

provided it has been properly treated. Not only is the quantity of

valuable matters existing in the soluble state materially increased,

whereby the dung is enabled to act with greater rapidity, but, owing to

evaporation and the escape of carbonic acid, produced by the

decomposition of the organic substances, the proportion of those

constituents which are most important to the plant is increased. This is

particularly to be noticed, in regard to the nitrogen, which has

distinctly increased in all cases in which the dung has been kept for

some time; and the practical importance of this observation is very

great, because it has been commonly supposed that, during the process of

fermentation, ammonia is liable to escape into the air. It would appear,

however, that there is but little risk of loss in this way, so long as

the dung-heap is left undisturbed; and it is only when it is turned that

any appreciable quantity of ammonia volatilizes. It is different,

however, with the action of rain, which soon removes, by solution, a

considerable quantity of the nitrogen contained in farm-yard manure; and

the deterioration must necessarily be most conspicuous in rotten dung,

which sometimes contains nearly half of its nitrogen in a soluble

condition. The effect produced in this way is conspicuously seen, by the

results of weighings and analyses of small experimental dung-heaps, made

by Dr. Voelcker at different periods. The subjoined table shows the

composition of the heap, lying against a wall, and exposed to the

weather at different periods:--

+--------------------------+-------------------------------------------+

| | WHEN PUT UP. |

| +---------+------------+---------+----------+

| | Nov 3d | April 30th | Aug 23d | Nov 15th |

| | 1854. | 1855. | 1855. | 1855. |

| +---------+------------+---------+----------+

| Weight of manure in lbs. | 2838 | 2026 | 1994 | 1974 |

| +---------+------------+---------+----------+

| Water | 1877.9 | 1336.1 | 1505.3 | 1466.5 |

| Dry Matter | 960.1 | 689.9 | 488.7 | 507.5 |

| +---------+------------+---------+----------|

| Consisting of-- | | | | |

| Soluble organic matter | 70.38 | 86.51 | 58.83 | 54.04 |

| " mineral matter | 43.71 | 57.88 | 39.16 | 36.89 |

| Insoluble organic matter | 731.07 | 389.74 | 243.22 | 214.92 |

| " mineral matter | 114.94 | 155.77 | 147.49 | 201.07 |

| +---------+------------+---------+----------+

| Total nitrogen | 18.23 | 18.14 | 13.14 | 13.03 |

| Equal to ammonia | 22.14 | 22.02 | 15.96 | 15.75 |

+--------------------------+---------+------------+---------+----------+

In this case, during the winter six months, which were very dry, the

manure lost 541.8 lbs. of water and 270.2 lbs. of dry matter, but the

nitrogen remained completely unchanged. But during the succeeding

semi-annual period, when rain fell abundantly, the quantity of nitrogen

is diminished by nearly a third, while the water has increased, and the

loss of dry matter by fermentation, notwithstanding the high temperature

of the summer months, was only 182.4 lbs. The soluble mineral matters

also, which increased during the first period, are again reduced during

the second, until they also fall to about two-thirds of their maximum

quantity. That this effect is to be attributed to the solvent action of

rain is sufficiently obvious, from a comparison of the results afforded

by the other heaps, which had been kept under cover during the same

period, as shown below.

+--------------------------+----------------------------------------------|

| | WHEN PUT UP. |

| +----------+------------+----------+-----------+

| | Nov. 3d, | April 30th | Aug. 23d | Nov. 15th |

| | 1854. | 1855. | 1855. | 1855. |

| +----------+------------+----------+-----------+

| Weight of manure in lbs. | 3258 | 1613 | 1297 | 1235 |

| +----------+------------+----------+-----------|

| Water | 2156.0 | 917.6 | 563.2 | 514.5 |

| Dry Matter | 1102.0 | 695.4 | 733.8 | 720.5 |

| +----------+------------+----------+-----------|

| Consisting of-- | | | | |

| Soluble organic matter | 80.77 | 74.68 | 53.56 | 66.28 |

| " mineral matter | 50.14 | 54.51 | 39.55 | 54.68 |

| Insoluble organic matter | 839.17 | 410.24 | 337.32 | 341.97 |

| " mineral matter | 131.92 | 155.97 | 303.37 | 257.57 |

| +----------+------------+----------+-----------+

| Total nitrogen | 20.93 | 19.26 | 16.54 | 1.79 |

| Equal to ammonia | 25.40 | 23.33 | 20.08 | 2.81 |

+--------------------------+----------+------------+----------+-----------+

The loss of nitrogen is here comparatively trifling, and during the

whole year, but little exceeds two pounds, of which the greater part

escapes during the first six months, and the soluble inorganic matters

are almost unchanged. The total weight of the manure, however, undergoes

a very great reduction, due chiefly to evaporation of water, but in part

also to the loss of organic matters evolved in the form of carbonic acid

during fermentation.

When the manure is spread out, as it is usually found under cattle in

open yards, the deterioration is very great, a quantity thus treated

having lost, in the course of a year, nearly two-thirds of its nitrogen,

and four-fifths of its soluble inorganic matters.

The general conclusion deducible from these analyses is that, provided

it be carefully prepared, farm-yard manure does not differ very largely

in value, although the balance is in favour of the well-rotten dung.

This result is in accordance with that obtained by other experimenters,

who have generally found from 0.5 to 0.6 per cent of nitrogen, and 1 or

2 per cent of phosphates. But when carelessly managed, it may fall

greatly short of this standard, as is particularly seen in a sample

examined by Cameron, which had been so effectually washed out by the

rain, as to retain only 0.15 per cent of ammonia. These cases, however,

are exceptional, and well made and well preserved farm-yard manure will

generally be found to differ comparatively little in value; and when

bought at the ordinary price, the purchaser, as we shall afterwards more

particularly see, is pretty sure to get full value for his money, and

the specialities of its management are of comparatively little moment to

him. But the case is very different when the person who uses the manure

has also to manufacture it. The experiments already quoted have shown

that, though the manure made in the ordinary manner may, weight for

weight, be as valuable as at first, the loss during the period of its

preservation is usually very large, and it becomes extremely important

to determine the mode in which it may be reduced to the minimum.

In the production of farm-yard manure of the highest quality, the object

to be held in view is to retain, as effectually as possible, all the

valuable constituents of the dung and urine. But in considering the

question here, it will be sufficient to refer exclusively to its

nitrogen, both because it is the most important, and also because the

circumstances which favour its preservation are most advantageous to the

other constituents. In the management of the dung-heap, there are three

things to be kept in view:--First, To obtain a manure containing the

largest possible amount of nitrogen; secondly, To convert that nitrogen

more or less completely into ammonia; and thirdly, To retain it

effectually.

As far as the first of these points is concerned, it must be obvious

that much will depend on the nature and quantity of the food with which

the animals yielding the dung are supplied, and the period of the

fattening process at which it is collected. When lean beasts are put up

to feed, they at first exhaust the food much more completely than they

do when they are nearly fattened, and the manure produced is very

inferior at first, and goes on gradually improving in quality as the

animal becomes fat.

When the food is rich in nitrogenous compounds, the value of the manure

is considerably increased. It has been ascertained, for instance, that

when oil-cake has been used, not less than seven-eighths of the valuable

matters contained in it reappear in the excrements; and as that

substance is highly nitrogenous, the dung ought, weight for weight, to

contain a larger amount of that element. That it actually does so, I

satisfied myself by experiments, made some years since, when the dung

and urine of animals fed on turnips, with and without oil-cake, were

examined; but unfortunately, no determination of the total quantity of

the excretions could be made, so that it was impossible to estimate the

increased value. It has been commonly supposed that when cattle are fed

with oil-cake, the increased value of the manure is equal to from

one-half to two-thirds the price of the oil-cake; but this is a rather

exaggerated estimate as regards linseed-cake, although it falls short of

the truth in the case of rape, as we shall afterwards more particularly

see.

Although it may be possible, in this way, to increase the quantity of

nitrogen as a manure, there is a limit to its accumulation, due to the

fact, that it is contained most abundantly in the urine, which can only

be retained by the use of a sufficient supply of litter. Where that is

deficient, the dung-heap becomes too moist, and the fluid and most

valuable part drains off, either to be lost, or to be collected in the

liquid manure-tank. In the well managed manure-heap, the quantity of

litter should be sufficient to retain the greater part of the liquid

manure, and to admit of only a small quantity draining from it, which

should be pumped up at intervals, so as to keep the whole in a proper

state of moisture. Attention to this point is of great moment, and

materially affects the fermentation. When it is too moist or too dry,

that process is equally checked; in the former case by the exclusion of

air, which is essential to it; and in the latter, by the want of water,

without which the air cannot act. The exact mode in which the manure is

to be managed must greatly depend on whether the supply of litter is

large or small. In the latter case the urine escapes, and is collected

in the liquid manure-tank, and must be used by irrigation, and in some

cases this mode of application has advantages, but in general, it is

preferable to avoid it, and have recourse to substances which increase

the bulk of the heap sufficiently to make it retain the whole of the

liquid. For this purpose, clay, or still better, the vegetable refuse of

the farm, such as weeds, ditch cleanings, leaves, and, in short, any

porous matters, may be used. But by far the best substance, when it can

be obtained, is dry peat, which not only absorbs the fluid, but fixes

the ammonia, by converting it more or less completely into humate.

Reference has been already made to the absorbent power of peat in the

section on soils, but it may be mentioned here that accurate experiment

has shown that a good peat will absorb about 2 per cent[L] of ammonia,

and when dry will still retain from 1 to 1.5 per cent, or nearly twice

as much as would be yielded by the whole nitrogen of an equal weight of

farm-yard manure. Peat charcoal has been recommended for the same

purpose, but careful experiment has shown that it _does not absorb

ammonia_, although it removes putrid odour; and though it may be

usefully employed when it is wished to deodorize the manure heap, it

must not be trusted to for fixing the ammonia.

Much stress has frequently been laid on the advantage to be derived from

the use of substances capable of combining chemically with the ammonia

produced during the fermentation of dung and gypsum, sulphate of iron,

chloride of manganese, sulphate of magnesia, and sulphuric acid, have

been proposed for this purpose, and have been used occasionally, though

not extensively. They all answer the purpose of _fixing_ the ammonia,

that is, of preventing its escaping into the air; but the risk of loss

in this way appears to have been much exaggerated, for a delicate

test-paper, held over a manure-heap, is not affected; and during

fermentation, humic acid is produced in such abundance, as to combine

with the greater part of the ammonia. The real source of deterioration

is the escape of the soluble matters in the drainings from the

manure-heap, which is not prevented by any of these substances; and

where no means are taken to preserve or retain this portion, the loss is

extremely large, and amounts, under ordinary circumstances, to from a

third to a half of the whole value of the manure. Manure, therefore,

cannot be exposed to the weather without losing a proportion of its

valuable matters, depending upon the quantity of rain which falls upon

it. Hence it is obvious that great advantage must be derived, especially

in rainy districts, from covered manure-pits. This plan has been

introduced on some farms with good effect; but the expense and doubts

as to the benefits derived from it, have hitherto prevented the practice

becoming general. The principal difficulty experienced in the use of the

covered dung-pit is, that, where the litter is abundant, the urine does

not supply a sufficiency of moisture to promote the active fermentation

of the dung, and it becomes necessary to pump water over it at

intervals; but when this is properly done, the quality of the manure is

excellent, and its valuable matters are most thoroughly economized.

Although covered dung-pits have been but little used, their benefits

have been indirectly obtained by the method of box-feeding, one of the

great advantages of which is held to be the production of a manure of

superior quality to that obtained in the old way. In box-feeding none of

the dung or urine is removed from under the animals, but is trampled

down by their feet, and new quantities of litter being constantly added,

the whole is consolidated into a compact mass, by which the urine is

entirely retained. Whatever objection may be taken to this system, so

far as the health of the animals is concerned, there is no doubt as to

the complete economy of the manure, provided the quantity of litter used

be sufficient to retain the whole of the liquid. But its advantage is

entirely dependent on the possibility of fulfilling this condition.

Whether box manure is really superior to that which can be prepared by

the ordinary method is very questionable, but it undoubtedly surpasses a

large proportion of that actually produced. It is more than probable,

however, that the careful management of the manure-heap would yield an

equally good product. It is manifest that the same number of cattle, fed

in the same way, on the same food, and supplied with the same quantity

of litter, must always excrete the same quantities of valuable matters;

and the only question to be solved is, whether they are more effectually

preserved in the one way than the other? It will be readily seen that

this cannot be done by analysis alone, but that it is necessary to

conjoin with it a determination of the total weight of manure produced;

for though, weight for weight, box manure may be better than ordinary

farm-yard manure, the total quantity obtained by the latter method, from

a given number of cattle, may be so much greater, that the deficiency in

quality may be compensated for. At the present time our knowledge is too

limited to admit of a definite opinion on this subject, but it is highly

deserving of the combined investigation of the farmer and the chemist.

Supposing the conditions which produce the manure containing the largest

quantity of nitrogen to have been fulfilled, we have now to consider

those which affect its evolution in the form of ammonia. This change is

effected by _fermentation_. When a quantity of manure is left to itself

it becomes hot, and gradually diminishes in bulk, and if it be turned

over after some time, the smell of ammonia may be more or less

distinctly observed. This ammonia is produced, in the first instance,

from the urine, the nitrogenous constituents of which are rapidly

decomposed, and the fermentation thus set up in the mass of manure

extends first to the solid dung, and then to the straw of the litter,

and gradually proceeds until a large quantity of ammonia is produced.

When fresh manure is deposited in the soil, the same changes occur, but

they then proceed more slowly, and experience has shown that a much

smaller effect is produced on the crop to which it has been applied than

when it has been well fermented in the heap. This effect is consistent

with theory, which would further indicate that well-fermented dung must

be especially advantageous when applied to quick-growing crops, and less

necessary to those which come slowly to maturity. As a rule, well

fermented manure is to be preferred, provided it has been well managed

and carefully prepared; but when this has not been done, and the manure

has been exposed to the weather, or made in open courts or hammels, the

economic advantages are all on the side of the fresh dung. It may be

questioned also whether, now that there are so many other available

sources of ammonia, it may not in many instances be advantageous to use

the dung fresh, conjoined with a sufficient quantity of some salt of

ammonia, or other substance fitted to supply the quantity of that

element necessary for the requirements of the crop.

After the farm-yard manure has been prepared at the homestead, it is

often necessary to cart it out to the field some time before it is to be

applied, and it is a question of some importance to determine how it may

be best preserved there. The general practice is to store it in heaps in

the corners of the fields, but some difference of opinion exists as to

whether it should be lightly thrown up so as to leave it in a porous

state, and so promote its further fermentation, or whether it should be

consolidated as much as possible by driving the carts on to the top of

the heap during its construction. Considering the risks to which the

manure is exposed on the field, the latter plan would appear to be the

best. It is advisable also to interstratify the dung with dry soil, so

as to absorb any liquid which may tend to escape from it, and it should

also be covered with a well-beaten layer of earth, in order to exclude

the rain. Although these precautions must not be omitted if the manure

is to be stored in heaps, it will probably be often found quite as

advantageous to spread it at once, and leave it lying on the surface

until it is convenient to plough it. The loss of ammonia by

volatilization will, under such circumstances, especially in the cold

season of the year, be very trifling, and the rain which falls will only

serve to incorporate the soluble matters with the soil, where they will

be retained by its absorptive power.

In the actual application of the manure to the crop, several points

require consideration. It is especially important to determine whether

it ought to be uniformly distributed through the soil, or be kept near

the roots of the plants. Both systems have their advocates, and each has

advantages in particular cases. The choice between the two must greatly

depend upon the nature of the crop and the soil. When the former is of a

kind which spreads its roots wide and deep through the soil, the more

uniformly the manure can be distributed the better; but when it is used

with plants whose roots do not travel far, it is more advantageous to

accumulate it near the seeds. Obvious advantages also attend this

practice in soils which are either too heavy or too light. When, for

example, it is necessary to cultivate turnips in a heavy clay, the

manure put into the drills produces a kind of artificial soil in the

neighbourhood of the plants, in which the bulbs expand more readily than

in the clay itself. On the other hand, when a large quantity of dung, in

a state of active fermentation, comes into immediate contact with the

roots, its effect is not unfrequently injurious. These and many other

points, which will readily suggest themselves to any one who studies the

composition and properties of farm-yard manure, belong more strictly to

the subject of practical agriculture, and need not be enlarged on here.

In the present state of agriculture, a proper estimate of the money

value of farm-yard manure is of much importance in an economic point of

view, and many matters connected with the profitable management of a

farm must hinge upon it. If an estimate be made upon the principle which

will be explained when we come to treat of artificial manures, it

appears that fresh farm-yard manure of good quality is worth from 12s.

to 15s. per ton, and well-rotted dung rather more. It is questionable,

however, whether the system of valuation which is accurate in the case

of a guano or other rapidly acting substance, is applicable to farm-yard

manure, the effects of which extend over some years. A deduction must be

made for the years during which the manure remains unproductive, and

also for the additional expense incurred in carting and distributing a

substance so much more bulky than the so-called portable manures, and it

would not be safe to estimate its value at more than 7s. or 8s. per ton.

_Liquid Manure._--This term is applied to the urine of the animals fed

on the farm, and to the drainings from the manure-heap, which, in place

of being returned to it, are allowed to flow away, and collected in

tanks, from which they are distributed by a watering-cart, or according

to the method recently introduced in Ayrshire, and since adopted in

other places, by pipes laid under-ground in the fields, and through

which the manure is either pumped by steam-power, or, where the

necessary inclination can be obtained, is distributed by gravitation.

That liquid manure must necessarily be valuable, is an inference which

maybe at once drawn from the analyses of the urine of different animals

already given, and of which it chiefly consists. In addition to the

urine, however, it contains also the soluble organic and mineral matters

of the dung, as well as a quantity of solid matters in suspension, among

which phosphates are found, and thus it possesses a supply of an

element which would be almost entirely deficient if it were composed of

urine alone. In the following analyses by Professor Johnston, No. 1 is

the drainings of the manure-heap when exposed to rain; and No. 2 the

same, when moistened with cows' urine pumped over it, the results being

expressed in grains per gallon:--

No. 1. No. 2.

Ammonia 9.6 21.5

Organic matter 200.8 77.6

Ash 268.8 518.4

----- -----

Total solids in a gallon 479.2 617.5

The ash contained--

Alkaline salts 207.8 420.4

Phosphates 25.1 44.5

Carbonate of lime 18.2 31.1

Carbonate of magnesia, and loss 4.3 3.4

Silica and alumina 13.4 19.0

----- -----

268.8 518.4

More elaborate analyses of the same fluid have since been made by Dr.

Voelcker, with the subjoined results per gallon:--

1. 2. 3.

Organic matters and ammoniacal } 263.80 250.63 70.121

salts }

Silica 2.49 9.98 1.154

Oxide of iron 0.70 0.68 ...

Lime 5.34 25.18 13.011

Magnesia 2.96 15.33 1.660

Potash 103.23 112.26 13.411

Chloride of potassium 72.00 77.38 7.712

Chloride of sodium 17.18 46.03 17.258

Phosphoric acid 2.70 9.51 2.304

Sulphuric acid 22.31 37.60 3.408

Carbonic acid, and loss 33.90 27.95 14.025

------ ------ -------

Total solids 526.61 612.53 144.064

Ammonia 114.16 22.31 26.647

The differences are here very remarkable, especially in the quantity of

ammonia, which is exceedingly large in the first sample. All of them are

particularly rich in potash, and contain but a small proportion of

phosphoric acid. The general inference to be deduced from them is, that

liquid manure is a most important source of the alkalis and ammonia, and

must be peculiarly valuable on soils in which these substances are

deficient.

The system of liquid manuring, originally introduced by Mr. Kennedy of

Myremill, Ayrshire, and which has since been adopted in some other

places, differs from liquid manuring in its _strict_ sense, for not only

are the drainings of the manure-heap employed, but the whole solid

excrements are mixed with water in a tank, and rape-dust and other

substances occasionally added, and distributed through the pipes.

It has been abandoned on Mr. Kennedy's farm, but is in use at Tiptree

Hall, and on the farm of Mr. Ralston, Lagg, where the fluid is

distributed by gravitation.

The arrangements employed by Mr. Mechi are identical with those formerly

in use at Myremill. The greater part of the stock is kept on boards, and

the liquid and solid excrements are collected together in the tank, and

largely diluted before distribution. The liquid from the tanks has been

recently examined by Dr. Voelcker, who found it to contain per gallon--

Organic matter and ammoniacal salts 53.03

Soluble silica 6.47

Insoluble siliceous matter (clay) 15.17

Oxide of iron and alumina 2.36

Lime 6.60

Magnesia 1.73

-----

Potash 0.35

Chloride of potassium 1.95

Chloride of sodium 4.81

Phosphoric acid 3.72

Sulphuric acid 1.94

Carbonic acid, and loss 0.47

-----

Total solids 96.60

Ammonia 8.10

The quantity of this liquid distributed per acre is about 50,000

gallons, at a cost of 2d. per gallon. As this quantity contains about 39

lbs. of ammonia, it must be nearly equivalent to 2 cwt. of Peruvian

guano, which costs, with the expense of spreading, from 28s. to 30s. per

acre, while the cost of distributing the liquid exceeds L1: 17s. per

acre. On the other hand, the rapidity with which liquid manure produces

its effect must be taken into account. It is on this that its chief

value depends, and especially when applied to grass land in early

spring, it produces an abundant crop just when turnips and other winter

food are exhausted. Mr. Telfer, Cunning Park, who has used this system

for a good many years, has come to the conclusion that it is only in

this way that it can be made profitable; and though pipes are laid all

over his farm, he has latterly restricted the use of the liquid manure

entirely to Italian ryegrass. Its effect on the cereals is much less

marked, and it can scarcely be considered as capable of advantageous

application to the general operations of the farm. Neither can liquid

manure be applied to all soils. It fails entirely on heavy clays, but is

peculiarly adapted to light sandy soils; and even barren sand may by its

repeated application, be made to yield luxuriant crops. It is not likely

that the system of liquid manuring will extend, except in localities

where it is possible to distribute it by gravitation; and even then, it

will probably be found most economical to restrict its use to one

portion of the farm; and for that purpose, the poorest and most sandy

soil ought to be selected.

_Sewage Manure._--The use of the sewage of towns as a manure is closely

connected with that of the liquid manure produced on the farm. Its

application must take place in a similar manner, and be governed by the

same principles. Although numerous attempts have been made to convert it

into a solid form, or to precipitate its valuable matter, none of them

have succeeded; nor can it be expected that any plan can be devised for

the purpose, because the most important manurial constituents are

chiefly soluble, and cannot be converted into an insoluble state, or

precipitated from their solution. In its liquid form, however, sewage

manure has been employed with the best possible effect in the

cultivation of meadows. The most important instance of its application

is in the neighbourhood of Edinburgh, where 325 acres receive the sewage

of nearly half the town, and have been converted from barren sand into

land which yields from L20 to L30 per acre. The contents of the sewer,

taken just before it flows into the first irrigated meadow, near

Lochend, were found to contain per gallon--

Soluble organic matter 21.90

Insoluble organic matter 21.70

Peroxide of iron and alumina 2.01

Lime 10.50

Magnesia 2.00

Sulphuric acid 6.09

Phosphoric acid 6.14

-----

Chlorine 12.20

Potash 2.89

Soda 13.27

Silica 6.50

------

105.20

Ammonia 14.90

It is interesting to notice that this sewage is superior in every

respect to the liquid manure used at Tiptree Hall; and the good effects

obtained from its application, in the large quantities in which it is

used in the Craigentinny meadows, may be well imagined. It operates, not

merely by the substances which it holds in solution, but also by

depositing a large quantity of matters carried along in suspension, and

is in reality warping with a substance greatly superior to river-mud. A

deposit collected in a tank, where the sewage passes through a farm, is

used as a manure, and contains--

Peroxide of iron and alumina 4.45

Lime 1.74

Magnesia 0.39

Potash 0.10

Soda 0.06

Phosphoric acid 1.08

Sulphuric acid 0.16

Organic matter 17.95

Sand 20.51

Water 53.56

------

100.00

Ammonia 0.93

And even, though containing more than half its weight of water and 20

per cent of sand, this substance has considerable value as a manure.

The growing evils of the existing system of sewage, and the enormous

waste of a manurial matter, which the experience of the Craigentinny

meadows has shewn to be productive of the most important effects, has

recently directed much attention to the conversion of the contents of

our sewers into a useful manure. Numerous plans for its precipitation

and conversion into a solid manure have been proposed, but most of these

have shewn an entire ignorance of the fundamental principles of

chemistry, and the best only succeed in precipitating a very small

proportion of its valuable matters, and leave almost the whole of the

ammonia, as well as the greater part of the fixed alkalies, in solution.

Nor is it to be expected that any process will be discovered by which

these substances can be precipitated, because solubility is the special

characteristic of their compounds, and no means is known by which it is

possible to convert them into an insoluble form. If sewage is to be used

at all, there seems little doubt that it must be by applying it entire,

and in the liquid state. But here again, the expense of conveying it on

to the land becomes an obstacle which it must frequently be impossible

to overcome. When it can be conveyed by gravitation, as is the case in

the neighbourhood of Edinburgh, it may undoubtedly be used with the

utmost advantage, and with the very best economic results. But when it

requires to be carried to a great distance through pipes, and raised to

a high level by pumping, all these advantages disappear. If the cost of

application amounts to 2d. a gallon, as in Mr. Mechi's case, or even to

half that sum, it may be fairly concluded that it cannot be used with

any great prospect of large economic results, and that, unless under

very exceptional cases, it must be unprofitable.

The chances of success must also greatly depend upon the kind of soil on

which it is used. Experience has shewn that its effects are most

beneficial on light and deep sandy soils, but that on heavy retentive

clays it is without effect, or even absolutely injurious. In clay soils

it is important to use every means of getting rid of moisture, and any

plan which adds 200 or 300 tons of water to them, only aggravates their

natural defects to an extent which more than counterbalances the

benefits derived from the manurial matter it contains. Whatever the

ultimate result of the use of town sewage in the liquid form may be, it

is unlikely that it will be employed in general agricultural practice.

It is more probable that it will be found necessary to set apart a

certain breadth of land to be treated by it exclusively. Many plans have

been proposed for conveying it through considerable districts, and

selling to the surrounding farmers the quantities which they require,

but wherever large sewage-works are established, it will be impossible

to depend on a precarious demand, and the promoters of such schemes will

be compelled, as part of their speculation, to supply not only the

manure, but the land on which it is to be used. Indeed, the difficulties

attending the whole question are so formidable, that even those who are

most anxious to see a stop put to the waste of manurial matter must

admit that the prospect of a successful economic result is not

encouraging. Nor is it likely that anything will be done until the whole

system of managing town refuse is changed, and in place of deluging it

with water, some plan can be contrived which, while fulfilling sanatory

requirements, shall preserve it in a concentrated form, or convert it

into a dry and inodorous substance.

FOOTNOTES:

[Footnote L: Report on the economic uses of peat. Highland Society's

Transactions, N.S., vol. iv. p. 549.]

Elements of Agricultural Chemistry · 第 8 / 14 章