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
If we expect, therefore, to furnish passage for but two feet of water in
the year, our drains need not be so numerous as would be necessary to
accommodate twice that quantity, unless, indeed, the time for its
passage may be different; and this leads us to another point which
should ever be kept in mind in New England--the necessity of quick
drainage. The more violent storms and showers of our country, as
compared with England, have been spoken of when considering _The Size of
Tiles_. The sudden transition from Winter to Summer, from the breaking
up of deep snows with the heavy falls of rain, to our brief and hasty
planting time, requires that our system of drainage should be efficient,
not only to take off large quantities of water, but to take them off in
a very short time. How rapidly water may be expected to pass off by
drainage, is not made clear by writers on the subject.
"One inch in depth," says an English writer, "is a very heavy fall of
rain in a day, and it generally takes two days for the water to drain
fully from deep drained land." One inch of water over an acre is
calculated to be something more than one hundred tons. This seems, in
gross, to be a large amount, but we should expect that an inch, or even
two inches of water, spread evenly over a field, would soon disappear
from the surface; and if not prevented by some impervious obstruction,
it must continue downward.
It is said, on good authority, that, in England, the smallest sized
pipes, if the fall be good, will be sufficiently large, at ordinary
distances, to carry off all the surplus water. In the author's own
fields, where two-inch tiles are laid at four feet depth and fifty feet
apart, in an open soil, they seem amply sufficient to relieve the ground
of all surplus water from rain, in a very few days. Most of them have
never ceased to run every day in the year, but as they are carried up
into an undrained plain, they probably convey much more water than falls
upon the land in which they lie.
So far as our own observation goes, their flow increases almost as soon
as rain begins to fall, and subsides, after it ceases, about as soon as
the water in the little river into which they lead, sinks back into its
ordinary channel, the freshet in the drains and in the stream being
nearly simultaneous. Probably, two-inch pipes, at fifty feet distances,
will carry off, with all desirable rapidity, any quantity of water that
will ever fall, if the soil be such that the water can pass through it
to the distance necessary to find the drains; but it is equally probable
that, in a compact clay soil, fifty feet distance is quite too great for
sufficiently rapid drainage, because the water cannot get to the drains
with sufficient rapidity.
DISTANCES DEPEND UPON THE COMPARATIVE PRICES OF LABOR AND TILES.
Public-domain text, read in full here on John Shaqi.
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