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
We should not expect that, on such a clay, the full effect of drainage
would be at once apparent. The water falling on the surface would very
slowly find its way downward, at first. But after the heat of Summer,
aided by the drains underneath, had contracted and cracked the soil,
passages for the water would soon be found, and, after a few years, the
whole mass, to the depth of the drains, would become open and permeable.
As an old English farmer said of his drains, "They do better year by
year; the water gets a habit of coming to them." Although this be not
philosophical language, yet the fact is correctly stated. Water tends
towards the lowest openings. A deep well often diverts the underground
stream from a shallower well, and lays it dry. A single railroad cut
sometimes draws off the supply of water from a whole neighborhood.
Passages thus formed are enlarged by the pressure of the water, and new
ones are opened by the causes already suggested, till the drainage
becomes perfect for all practical purposes. So much is this cracking
process relied on to facilitate drainage, that skillful drainers
frequently leave their ditches partly open, after laying the tiles, that
the heat may produce the more effect during the first season.
As to the depth of drains in stiff clays, enough has already been said,
under the appropriate title. In England, the weight of authority is in
favor of four-foot drains. In this country, a less depth has thus far,
in general, been adopted in practice, but it is believed that this has
been because a greater depth has not been tried. It is understood, that
the most successful drainers in the State of New York, have been
satisfied with three-foot drains, not, as it is believed, because there
is any instance on record, in this country, of the failure of four-foot
drains, but because the effect of more shallow drains has been so
satisfactory, that it has been thought a useless expense to go deeper.
To Mr. Johnston and to Mr. Delafield, of Seneca County, the country is
greatly indebted for their enterprise and leadership in the matter of
drainage. Mr. Johnston gives it as his opinion, that "three feet is deep
enough, if the bottom is hard enough to lay tiles on; if not, go
deeper."
Without intimating that any different mode of drainage than that
adopted, would have been better on Mr. Johnston's farm, we should be
unwilling to surrender, even to the opinion of Mr. Johnston and his
friends, our conviction that, in general, three-foot drains are too
shallow. Mr. Johnston expressly disclaims any experience in draining a
proper clay soil. In the _Country Gentleman_, of June 10th, 1848, he
says:
Public-domain text, read in full here on John Shaqi.
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