Geology, Vol. 1 [of 3] : $b Geologic processes and their resultsSalisbury, Rollin D.
Science
Geology, Vol. 1 [of 3] : $b Geologic processes and their results
Salisbury, Rollin D.
Geology
=Volume and composition.=—Every 1000 parts of sea-water contain about
34.40 parts by weight of mineral matter in solution. The principal
solids, acids, and bases, combined according to the principles laid
down by Dittmar, are shown in the following table:[2]
Chloride of sodium 77.758
Chloride of magnesium 10.878
Sulphate of magnesium 4.737
Sulphate of calcium 3.600
Sulphate of potassium 2.465
Bromide of magnesium 0.217
Carbonate of calcium 0.345
-------
Total salts 100.000
Expressed in terms of tons per cubic mile of sea-water, the composition
is as follows:[139]
Tons per Cubic Mile.
Chloride of sodium (NaCl) 117,434,000
Chloride of magnesium (MgCl₂) 16,428,000
Sulphate of magnesium (MgSO₄) 7,154,000
Sulphate of calcium (CaSO₄) 5,437,000
Sulphate of potassium (K₂SO₄) 3,723,000
Bromide of magnesium (MgBr₂) 328,000
Carbonate of calcium (CaCO₃) 521,000
-----------
For sea-water, total dissolved matter 151,025,000
Aside from the ingredients shown in the above tables, the presence of
the following has been proved: iodine, fluorine, phosphorus, silicon,
boron, silver, lead, copper, zinc, cobalt, nickel, iron, manganese,
aluminum, barium, strontium, arsenic, lithium, cæsium, rubidium, and
gold. Oxygen, nitrogen, and carbonic acid gas are also present in
quantity. The amount of carbonic acid is estimated to be 18 times as
great as in the atmosphere.[140]
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