SOILS.

The nature and management of soils must be measurably understood by any

one who would be a thorough cultivator. The productive power of a soil

depends much upon the character of the subsoil. A gravelly subsoil is,

on the whole, the best. A thin soil lying on a cold clay subsoil--the

hardpan of the East, and the crowfish clay of the West--however rich it

may be, will be unproductive; while the same soil, on a gravelly

subsoil, would produce abundantly. The best soils, for all purposes, are

the brown or hazel-colored. Plowed in wet weather, they do not make

mortar, and in dry weather they will not break in clods. Dark-mixed and

russet moulds are considered the next best. The worst are the dark-gray

or ash-colored. The deep-black alluvial soils of the Western prairies

are an exception to all other soils, possessing, under proper treatment,

great powers of production. Soils do not, to any considerable extent,

afford food for plants. A willow-tree has been known to gain one hundred

and fifty pounds' weight, without exhausting more than two or three

ounces of the soil, and even that might have been wasted in drying and

weighing.

In our article on manures, we have shown that it is the texture of

soils, and their power to control moisture and heat, that renders them

productive: hence, no soil can be poor that is stirred deep and kept in

a friable condition, without being too open and porous; and no soil can

be good that is hard and not retentive of moisture, without having water

stand upon it. Hence, the great secret of successful farming, is, such a

mixture of the soils, and of fertilizers with the soil, as shall keep it

friable and moist, and such thorough drainage as will prevent water from

standing so as to become stagnant, and to unduly chill the roots of

growing plants. Nature has provided, near at hand, all that is essential

to productiveness; all that is necessary is to properly mix them. We do

not believe that there is an acre of land now under cultivation in the

United States, in a latitude where corn will grow, on which we can not

raise a hundred bushels of shelled Indian corn, without applying

anything but what may be raised out of that soil, and procured in the

shape of manure by animals in consuming that product. The poorest farm

in America may be brought up to a state of great fertility, without

applying one dollar's worth of any foreign substance. Plow _deep_, turn

under all the green substances possible, and feed out the products on

the farm and apply the manure, and mix opposite soils, that may be found

in different localities. Three years will secure great productiveness,

and the same course will increase its value, from year to year, without

cost. Three things only are essential to convert poor land into the

best; deep and thorough stirring and pulverization, suitable draining,

and thorough mixture of soils of different qualities, and the

incorporation of such animal and vegetable substances as can be produced

on the land itself. We would not declare against foreign manures, but

insist that the necessary ingredients are found, or may be manufactured

near at hand. The philosophy of deep plowing and thorough pulverization

is obvious. A fine soil will retain and appropriate moisture in an

eminent degree, on the principle of capillary attraction, or as a sponge

or a piece of loaf sugar will take up water. There is also room for

excess of water to sink away from the surface, and return again when

needed. It also affords room for the roots of plants. Such a soil also

receives moisture from the atmosphere. The atmosphere also contains much

water, and more in the heat of summer than at any other time. The air

also, with a constant pressure of fifteen pounds to the square inch,

enters to a considerable depth into the soil, and the deeper it is

stirred, and the more thoroughly it is pulverized, the more it will

enter. In coming in contact with the cool moisture below, it is

condensed and waters the soil, on the principle that a pitcher of cold

water in a warm room has large drops of water on the outside; that water

is a mere condensation of moisture in the atmosphere. The cool subsoil

acts in the same way upon the atmosphere at night. A deeply

disintegrated soil, also, seldom washes by rain. Shallow-plowed and

coarse land sends off the water after a slight rain, while deep-plowed

and thoroughly pulverized land retains it. The philosophy of manures

involves the same principles. All the fertilizers act upon soils in such

a manner as to render them fine, and open an immense surface to the

action of the atmosphere, and form large reservoirs for moisture through

their innumerable fine pores. Draining is to carry off an excess of

water that would stand on an unfavorable subsoil. That water, on

undrained land, causes two evils; it stagnates and renders plants

unhealthy, and it is too cool, rendering land what we call cold. Thus,

the deeper you plow land, and the finer you make it, the warmer it will

be, and the more perfectly it will control moisture. Mixing soils by

subsoiling, trenching, and deep plowing, and by carting on foreign

substances, is wholly on this principle. Sand that drifts about with the

wind is too light to retain moisture, and needs clay carted on. By this

means the poorest white sand has often been converted into the most

productive soil. Definite rules for this mixture of soils can not be

safely given. The rules must differ in different localities and

circumstances; it must, therefore, be determined by experiment.

Analyzing soils is sometimes of use, but usually has too much importance

attached. We do not advise farmers to study it. Let them try

applications and mixtures, at first on a small scale: they will soon

learn what is best on their farms, and may then proceed without loss.

Some lands are of such a character that the carting on, and suitably

mixing, the substances in which they are deficient, may cost as much as

it did to clear the land of its original forest; but it will pay well

for a long series of years. So well are we persuaded of the utility and

correctness of these brief hints, that, in selecting a farm, we should

regard the location more than the quality of the soil. The latter we

could mend easily; while we should find it difficult to move our farm to

a more favorable location. Poor land near a city or large town, or on

some great thoroughfare, we should much prefer to good land far removed

from market, or in an unpleasant location.

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