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
A comparison of the composition of rain-water with that of springs
and rivers gives some idea of the solvent work of water. From a
study of the water of nineteen of the principal rivers of the world
Murray has compiled the following table[38] showing the amount of
mineral matter in average river water:
_MATERIAL IN SOLUTION IN ONE CUBIC MILE OF AVERAGE RIVER WATER._[39]
Constituents. Tons in a Cubic Mile.
Calcium carbonate (CaCO₃) 326,710
Magnesium carbonate (MgCO₃) 112,870
Calcium phosphate (Ca₃P₂O₈) 2,913
Calcium sulphate (CaSO₄) 34,361
Sodium sulphate (Na₂SO₄) 31,805
Potassium sulphate (K₂SO₄) 20,358
Sodium nitrate (NaNO₃) 26,800
Sodium chloride (NaCl) 16,657
Lithium chloride (LiCl) 2,462
Ammonium chloride (NH₄Cl) 1,030
Silica (SiO₂) 74,577
Ferric oxide (Fe₂O₃) 13,006
Alumina (Al₂O₃) 14,315
Manganese oxide (Mn₂O₃) 5,703
Organic matter 79,020
-------
Total dissolved matter 762,587
Murray also estimates that the aggregate amount of water flowing
into the sea annually is about 6528 cubic miles, which, on the
above basis, would carry about 4,975,000,000 tons of mineral matter
in solution.
A large number of analyses of waters of rivers from the United
States and Canada give an average of about .15,044 part in a
thousand of mineral matter in solution, more than one-third being
CaCO₃. The average amount of mineral matter in solution in 48
European streams cited by Bischoff[40] is .2127 part in a thousand,
of which CaCO₃ is rather more than half. The average mineral matter
in solution in 36 rivers cited by Roth[41] (including some of those
tabulated by Bischoff) is .2033 part in a thousand, of which CaCO₃
is slightly less than one-half.
An average for American and European rivers, so far as determinable
from data at hand, is about .1888 part in a thousand in solution,
of which CaCO₃ is slightly less than one-half. These last figures
are probably not very far from an average for river water in
general.
The following table shows the total amount of solids carried in
solution by the rivers indicated:[42]
Rhine 5,816,805 tons per year.
Rhone 8,290,464 „ „ „
Danube 22,521,434 „ „ „
Thames 613,930 „ „ „
Nile 16,950,000 „ „ „
Croton 66,795 „ „ „
Hudson 438,000 „ „ „
Mississippi 112,832,171 „ „ „
ECONOMIC CONSIDERATIONS.
Public-domain text, read in full here on John Shaqi.
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