Familiar Letters on Chemistry eBook

This eBook from the Gutenberg Project consists of approximately 119 pages of information about Familiar Letters on Chemistry.

Familiar Letters on Chemistry eBook

This eBook from the Gutenberg Project consists of approximately 119 pages of information about Familiar Letters on Chemistry.

On pure sand, on calcareous soil, on naked rocks, only a few genera of plants prosper, and these are, for the most part, perennial plants.  They require, for their slow growth, only such minute quantities of mineral substances as the soil can furnish, which may be totally barren for other species.  Annual, and especially summer plants, grow and attain their perfection in a comparatively short time; they therefore do not prosper on a soil which is poor in those mineral substances necessary to their development.  To attain a maximum in height in the short period of their existence, the nourishment contained in the atmosphere is not sufficient.  If the end of cultivation is to be obtained, we must create in the soil an artificial atmosphere of carbonic acid and ammonia; and this surplus of nourishment, which the leaves cannot appropriate from the air, must be taken up by the corresponding organs, i.e. the roots, from the soil.  But the ammonia, together with the carbonic acid, are alone insufficient to become part of a plant destined to the nourishment of animals.  In the absence of the alkalies, the phosphates and other earthy salts, no vegetable fibrine, no vegetable caseine, can be formed.  The phosphoric acid of the phosphate of lime, indispensable to the cerealia and other vegetables in the formation of their seeds, is separated as an excrement, in great quantities, by the rind and barks of ligneous plants.

How different are the evergreen plants, the cacti, the mosses, the ferns, and the pines, from our annual grasses, the cerealia and leguminous vegetables!  The former, at every time of the day during winter and summer, obtain carbon through their leaves by absorbing carbonic acid which is not furnished by the barren soil on which they grow; water is also absorbed and retained by their coriaceous or fleshy leaves with great force.  They lose very little by evaporation, compared with other plants.  On the other hand, how very small is the quantity of mineral substances which they withdraw from the soil during their almost constant growth in one year, in comparison with the quantity which one crop of wheat of an equal weight receives in three months!

It is by means of moisture that plants receive the necessary alkalies and salts from the soil.  In dry summers a phenomenon is observed, which, when the importance of mineral elements to the life of a plant was unknown, could not be explained.  The leaves of plants first developed and perfected, and therefore nearer the surface of the soil, shrivel up and become yellow, lose their vitality, and fall off while the plant is in an active state of growth, without any visible cause.  This phenomenon is not seen in moist years, nor in evergreen plants, and but rarely in plants which have long and deep roots, nor is it seen in perennials in autumn and winter.

Copyrights
Project Gutenberg
Familiar Letters on Chemistry from Project Gutenberg. Public domain.