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Understanding Variation in Partition Coefficient, Kd, Values Volume II

Understanding Variation in Partition Coefficient, Kd, Values Volume II

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Table 5.1. Estimated mean composition of river<br />

water of the world from Hem (1985). 1<br />

Dissolved Constituent<br />

5.3<br />

Total Concentration<br />

mg/l mol/l<br />

Silica, as H 4SiO 4 20.8 2.16 x 10 -4<br />

Ca 15 3.7 x 10 -4<br />

Mg 4.1 1.7 x 10 -4<br />

Na 6.3 2.7 x 10 -4<br />

K 2.3 5.9 x 10 -5<br />

Inorganic Carbon, as CO 3 57 9.5 x 10 -4<br />

SO 4 11 1.1 x 10 -4<br />

Cl 7.8 2.2 x 10 -4<br />

F 1 5 x 10 -5<br />

NO 3 1 2 x 10 -5<br />

PO 4 0.0767 8.08 x 10 -7<br />

1 Most values from this table were taken from Hem (1985: Table 3,<br />

Column 3). Mean concentrations of total dissolved fluoride and<br />

phosphate are not listed <strong>in</strong> Hem (1985, Table 3). The concentration of<br />

dissolved fluoride was taken from Hem (1985, p. 120) who states that the<br />

concentration of total dissolved fluoride is generally less than 1.0 mg/l for<br />

most natural waters. Hem (1985, p. 128) lists 25 micro g/l for average<br />

concentration of total dissolved phosphorous <strong>in</strong> river water estimated by<br />

Meybeck (1982). This concentration of total phosphorus was converted<br />

to total phosphate (PO 4) listed above.

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