The Elements of Agriculture. George Edwin Waring. Читать онлайн. Newlib. NEWLIB.NET

Автор: George Edwin Waring
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that the presence of certain ingredients is necessary to fertility. This may be better explained by the assistance of the following table:

      What can you say of the soils represented in the table of analyses?

      What proportion of the fertilizing ingredients is required?

      If the soil represented in the third column contained all the ingredients required except potash and soda, would it be fertile?

      What would be necessary to make it so?

      What is the reason for this?

      What are the offices performed by the inorganic part of soils?

      The soil represented in the first column might still be fertile with less organic matter, or with a larger proportion of clay (alumina), and less sand (silica). These affect its mechanical character; but, if we look down the column, we notice that there are small quantities of lime, magnesia, and the other constituents of the ashes of plants (except ox. of manganese). It is not necessary that they should be present in the soil in the exact quantity named above, but not one must be entirely absent, or greatly reduced in proportion. By referring to the third column, we see that these ingredients are not all present, and the soil is barren. Even if it were supplied with all but one or two, potash and soda for instance, it could not support a crop without the assistance of manures containing these alkalies. The reason for this must be readily seen, as we have learned that no plant can arrive at maturity without the necessary supply of materials required in the formation of the ash, and these materials can be obtained only from the soil; consequently, when they do not exist there, it must be barren.

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      1

      By saturated, we mean that it contains all that it is capable of holding.

      2

      Bromine, iodine, etc., are sometimes detected in particular plants, but need not occupy the attention of the farmer.

1

By saturated, we mean that it contains all that it is capable of holding.

2

Bromine, iodine, etc., are sometimes detected in particular plants, but need not occupy the attention of the farmer.

3

This classification is not strictly scientific, but it is one which the learner will find it well to adopt. These bodies are called neutrals because they have no decided alkaline or acid character.

4

In some soils the fluorides undoubtedly supply plants with soluble silicates, as fluoric acid has the power of dissolving silica. Thus, in Derbyshire (England), where the soil is supplied with fluoric acid, grain is said never to lodge.

5

Sourness.

6

There is reason to suppose that alumina is an essential constituent of many plants.

7

By proximate principle, we mean that combination of vegetable elements which is known as a vegetable product, such as wood, etc.

8

Muscle is lean meat, it gives to animals their strength and ability to perform labor.

9

This, of course, supposes that the soil is fertile in other respects.

10

This pectic acid gelatinizes food in the stomach, and thus renders it more digestible.

11

See Johnston's Elements, page 41.

12

Sifted through a fine cloth called a bolting cloth.

13

The spaces between the particles.

14

In very many instances the crevices and seams of rocks are permeated by roots, which, by decaying and thus inducing the growth of other roots, cause these crevices to become filled with organic matter. This, by the absorption of moisture, may expand with sufficient power to burst the rock.

15

Some rocks contain sulphur, phosphorus, etc., and these may, perhaps, be considered as organic matter.

16

These distinctions are not essential to be learned, but are often convenient.