The solubility of Earthy Carbonates in Pure Water.
Consider that the question of thig should
be answered, at any time and not by authority; therefore, the rate of
dissolving calcic carbonate in freshwater, as allocated by Fresenius is
one-third of 10,601 parts of water, and that of Bloxham, one-half to 85,000,
and one-third of 23,000 is usually taken by 88 data when calculated than most
of these compounds are present in the ocean. water, Or about three grains per liter.
Now these statements, as you can see, have
a very contradictory character, and when combined the knowledge of this fact
with that of the most significant solvent effect for most alkaline salts in
calcic carbonate I was impressed with the view that in the case of earth
carbonates those effects on which high melting points were based on the
performance of one or more salts in the experimental liquid, a certain amount
of tested carbonate was dissolved. thus, in addition, it added to what could be
dissolved in pure water, increasing the melted value of One by a much greater proportion of what should be distributed to such carbonates.
First of all, in terms of approach.
I developed a ground solution, the
carbonate of which should be tested, with a certain amount of energy, such as
chloride, and a very weak solution of carbonate of soda or lithia. Both of
these solutions have been boiled for a long time to remove any free carbonic
acid and then allowed to cool to room temperature. Earth chloride solution I
then diluted with freshly diluted water in small quantities and measured until
the last part of the sample was removed when mixed with carbonate but appeared
to have small clouds (indicating carbonate eruption) when viewed in large
quantities and after large expiration. as long as. a thin cloud is formed under
these conditions, all the earth carbonate produced by the contact of salts used
is insoluble, most of the minutes are thrown out without a solution, so by
calculating the amount of earth carbonate present in a certain volume of liquid
we have a moderate melting point in the earth's carbonated carbonate.
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