Elements of agricultural chemistry and geologyJohnston, Jas. F. W. (James Finlay Weir)
Science
Elements of agricultural chemistry and geology
Johnston, Jas. F. W. (James Finlay Weir)
Agricultural chemistry
1. It directly affords food to the plant, which, as we have seen,
languishes where lime is not attainable. It serves also to convey other
food to the roots in a state in which it can be made available to
vegetable growth.
2. It neutralizes (removes the _sourness_) of all acid substances as
they are formed in the soil, and thus keeps the land in a condition to
nourish the tenderest plants. This is one of the important agencies
of shell-sand when laid on undrained grass lands—and this effect it
produces in common with wood-ashes, and many similar substances.
3. During the decay of organic matter in the soil, it aids and
promotes the production of nitric acid,—so influential, as I believe,
in the general vegetation of the globe (see page 35). With this acid
it combines and forms _nitrate of lime_—a substance very soluble in
water—entering readily, therefore, into the roots of plants, and
producing upon their growth effects precisely similar to those of the
now well known _nitrate of soda_. The success of frequent ploughings,
harrowings, hoeings, and other modes of stirring the land, is partly
owing to the facilities which these operations afford to the production
of this and other natural nitrates.
SECTION VII.—OF THE IRRIGATION OF THE LAND.
The irrigation of the land is, in general, only a more refined method
of manuring it. The nature of the process itself, however, is different
in different countries, as are also the kind and degree of effect it
produces, and the theory by which these effects are to be explained.
In dry and arid climates, where rain rarely falls, the soil may contain
all the elements of fertility, and require only water to call them
into operation. In such cases, as in the irrigations practised so
extensively in eastern countries, and without which, whole provinces
in Africa and Southern America would lie waste, it is unnecessary to
suppose any other virtue in irrigation than the mere supply of water it
affords to the parched and cracking soil.
But in climates such as our own, there are two other beneficial
purposes in reference to the soil, which irrigation may, and one at
least of which it always does, serve.
2. The occasional flow of _pure_ water over the surface, as in
our irrigated meadows, and its descent into the drains, where the
drainage is perfect, washes out acid and other noxious substances
naturally generated in the soil, and thus purifies and sweetens it.
The beneficial effect of such washing will be readily understood in
the case of peat lands laid down to water meadow, since, as every one
knows, peat soils abound in matters unfavourable to general vegetation,
and which are usually in part drawn off by drainage, and in part
destroyed by lime and by exposure to the air, before boggy lands can be
brought into profitable cultivation.
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