Elements of Chemical And Physical Geology volume 1
Elements of Chemical And Physical Geology volume 1
Gustav Bischof
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Et de Thys. 1844, T. 8, p. 425. I Ibid. T. 12, p. 5. With regard to the presence of sulphuretted hydrogen in sea- water, see Chapter XVI. I 2 116 CARBONIC ACID IN SEA- WATER. of green plants, and the variation in the proportion of gases con- tained in sea-water. It has been already pointed out by A. And Ch. Morren, * that green animalcules produce, under the influence of the sun's rays, similar effects upon the gases contained in fresh water. F The presence of carbonic acid in sea-water is suff...iciently proved by the preceding observations, and indeed it might well be asked, how it could possibly be wanting in a fluid in which a far greater number of animals breathe than upon land. In reference to geology it is of particular importance. The carbonic acid contained in sea-water will constantly dissolve carbonate of lime when present upon the sea-bottom. If, as appears to follow from my researches, the carbonate of lime and carbonate of magnesia are present in sea- water as sesqui carbonates, the quantities of these carbonates which I have found in it require 0*165 carbonic acid in order to be dissolved, consequently about one-fifth of the quantity of this acid is present in sea-water.
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