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Proceedings and Documents of the House, 1858
Volume 665, Page 1448   View pdf image
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XX

that organic matter as they exist in solutions of soils had any effect
on this reaction.

We also know by the analysis of Sprenger, that a lucerne crop
of 8 5 tons contains of.

Soiling 6.5 tons, containing of Chlorine, 13 lbs.
Hay 2 "           " " "            14 lbs.

Total amount of Chlorine 27 lbs.

If we take this as an averaging crop per acre, then according to
the preceding 27 lbs., or we will say 30 lbs. of Chlorine (equal to
about I bushel of common salt) must be contained in 6,000,000 lbs.
of soil (one acre) to produce the average crop of lucerne, and con-
sequently every part of the soil has to contain 1-200.000 of its
weight of Chlorine; or if we dissolve the Chlorine in a certain
quantity of this soil by a solvent of equal weight, the solution will
also contain 1-200.000 of Chlorine, and by evaporating from it one-
half, a solution will be obtained which contains 1-100.000 of Chlor-
ine, an amount which can be detected by nitrate of silver, as above
stated.

For the purpose of testing a soil for its sufficiency or deficiency
in Chlorine, it is therefore only necessary to take a certain portion
of the prepared solution of the soil; to evaporate from it one-half
and to test with nitrate of silver. If no precipitate occurs after
heating and stirring the mass, it is a proof for the deficiency of the
soil in Chlorine.

Determination of Lime and Magnesia.

Both Lime and Magnesia exercise a double action as constituents
of soils; on one side they present themselves as fundamental ingre-
dients of soils, participating in the formation of the Cement, and as
such, their sufficiency or deficiency in soils is expressed by the
condition of the Cement; on the other side they serve as directly
nourishing substances to plants, and only to this extent can they be
subject to our discussion in this place. Experience teaches us in
this respect, that it would be difficult to find out a cultivated soil,
which would show itself so deficient in Lime and Magnesia, that it
could not supply that portion of them which the plants require as
nutriment. For this reason it cannot be of any practical use to
determine the quantities of Lime and Magnesia which may be ex-
tracted from soils; it is however a matter of importance to have an
idea of the mutual proportion of their quantities; and for this purpose
the following treatment may perfectly answer:

Take two equal parts of the original solution of the soil (about
a quarter of an ounce for each) and add to the one an equal volume
of alcohol and a few drops of sulphuric acid; the whole quantity of

 

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Proceedings and Documents of the House, 1858
Volume 665, Page 1448   View pdf image
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