Draining for Profit, and Draining for HealthWaring, George E. (George Edwin)
Science
Draining for Profit, and Draining for Health
Waring, George E. (George Edwin)
Drain-tiles; Drainage
Salt marshes are formed of the silty deposits of rivers and of the sea.
The former bring down vegetable mould and fine earth from the uplands, and
the latter contribute sea weeds and grasses, sand and shells, and millions
of animalculæ which, born for life in salt water only, die, and are
deposited with the other matters, at those points where, from admixture
with the fresh flow of the rivers, the water ceases to be suitable for
their support. It is estimated that these animalculæ alone are the chief
cause of the obstructions at the mouths of the rivers of Holland, which
retard their flow, and cause them to spread over the flat country
adjoining their banks. It is less important, however, for the purposes of
this chapter, to consider the manner in which salt marshes are formed,
than to discuss the means by which they may be reclaimed and made
available for the uses of agriculture. The improvement may be conveniently
considered under three heads:—
First—The exclusion of the sea water.
Second—The removal of the causes of inundation from the upland.
Third—The removal of the rain-fall and water of filtration.
*The Exclusion of the Sea* is of the first importance, because not only
does it saturate the land with water,—but this water, being salt, renders
it unfertile for the plants of ordinary cultivation, and causes it to
produce others which are of little, or no value.
The only means by which the sea may be kept out is, by building such dykes
or embankments as shut out the highest tides, and, on shores which are
exposed to the action of the waves, will resist their force. Ordinarily,
the best, because the cheapest, material of which these embankments can be
made, is the soil of the marsh itself. This is rarely,—almost never,—a
pure peat, such as is found in upland swamps; it contains a large
proportion of sand, blue clay, muscle mud, or other earthy deposits, which
give it great weight and tenacity, and render it excellent for forming the
body of the dyke. On lands which are overflowed to a considerable extent
at each high tide, (twice a day,) it will be necessary to adopt more
expensive, and more effective measures, but on ordinary salt meadows,
which are deeply covered only at the spring tides, (occurring every
month,) the following plan will be found practical and economical.
Public-domain text, read in full here on John Shaqi.
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