Farm drainage: The Principles, Processes, and Effects of Draining Land with Stones, Wood, Plows, and Open Ditches, and Especially with TilesFrench, Henry F. (Henry Flagg)
Science
Farm drainage: The Principles, Processes, and Effects of Draining Land with Stones, Wood, Plows, and Open Ditches, and Especially with Tiles
French, Henry F. (Henry Flagg)
Drainage
to us particles of every variety of shape and structure, of which a
certain part is evidently of vegetable origin. In these figures I
have given a very rude representation of these particles; and I
must beg you particularly to remember that they are not meant to
represent by any means accurately what the microscope exhibits, but
are only designed to serve as a plan by which to illustrate the
mechanical properties of the soil. On referring to Fig. 91, we
perceive that there are two distinct classes of pores; first, the
large ones, which exist _between_ the particles of soil, and
second, the very minute ones, which occur in the particles
themselves; and you will at the same time notice, that whereas all
the larger pores--those between the particles of soil--communicate
most freely with each other, so that they form canals, the small
pores, however freely they may communicate with one another in the
interior of the particle in which they occur, have no direct
connection with the pores of the surrounding particles. Let us now,
therefore, trace the effect of this arrangement. In Fig. 91, we
perceive that these canals and pores are all empty, the soil being
_perfectly dry_; and the canals communicating freely at the surface
with the surrounding atmosphere, the whole will of course be filled
with air. If in this condition, a seed be placed in the soil, as at
_a_, you at once perceive that it is freely supplied with air, _but
there is no moisture_; therefore, when soil is _perfectly dry_, a
seed cannot grow.
[Illustration: Fig. 91.]
[Illustration: Fig. 92.]
"Let us turn our attention now to Fig. 92. Here we perceive that
both the pores and canals are no longer represented white, but
black, this color being used to indicate water; in this instance,
therefore, water has taken the place of air, or, in other words,
the soil is _very wet_. If we observe our seed _a_ now, we find it
abundantly supplied with water, but _no air_. Here again,
therefore, germination cannot take place. It may be well to state
here, that this can never occur _exactly_ in nature, because water
having the power of dissolving air to a certain extent, the seed
_a_ in Fig. 92 is, in fact, supplied with a _certain_ amount of
this necessary substance; and, owing to this, germination does take
place, although by no means under such advantageous circumstances
as it would were the soil in a better condition.
[Illustration: Fig. 93.]
[Illustration: Fig. 94.]
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