WATER: PROPERTIES, STRUCTURE, AND OCCURRENCE IN NATURE 1299
H
Li Be B CNO F
He
Ne
Na Mg Al Si P S Cl Ar
K Ca
Sr
Ba
As Se Br Kr
I
H 2 O
–1.74 –1.74Li+
4.6BeOH+ (?)9.2H 3 BO 3 ,B(OH) 43.39HCO 32.64 30 1.97N 2 , NO 3 H 2 O, O 2–1.74–1.74F–, MgF+8.84.17 5.3 8.150.26 3.66 6.96SO2– 4 (NaSO 4 ) Cl–
1.55 3.92Se O 3 2–
8.6I–, IO 3 –
6.3H AsO 42 –7.3HPO 4 (MgPO 4 )
– ––
5.3H 4 SiO 44.15 3.7Al (OH) 4 –1.27 3.77 7.1Na+ Mg2+,MgSO 40.33 3.57K+
1.99 4.23Ca2+,(CaSO 4 )1.99 3.42Sr2+
4.05Ba2+6.8Br–
3.08 8.6Major Species (1)Conc. Seawater –log M (2)Conc. River water –log M (3)FIGURE 10 Some of the more important elements in natural waters, their form of occurrence and concentrations. Elements
whose distribution is significantly affected by biota are shaded. P, N, and Si (fully shaded) often become depleted in surface waters.
a) Species in parentheses are major ion pairs in sea water. b) Concentrations (M = mol/1) valid for seawater from P.G. Brewer in
Chemical Oceanography, Volume 1, J.P. Riley and G. Skirrow, eds, Academic Press, London 1975. c) From A.D. Livingstone,
Chemical Components of River and Lakes, US Geol. Survey Paper, 440 G, 1963.FIGURE 11 Cumulative distribution of inorganic species terrestrial waters. The curves represent the percentage of waters
with concentrations below that indicated on the horizontal axis. Data are mostly from the United States from various sources.
S.N. Davies and R.C.M. Dewiest, Hydrogeology, Wiley, New York, 1966.1009080706050403020100.01 0.1^110501001000UraniumMn2+Al3+Li+BrBoronFe2+F–Sr2+Fe2+
Sr2+NO^3NO^3K+K+Mg2+SO^42–SiO2ClSiO2Na+Ca2+Ca2+SO2– 4HCO- 3
Total dissolved solidsPercentage of watersParts per millionC023_004_r03.indd 1299C023_004_r03.indd 1299 11/18/2005 11:12:33 AM11/18/2005 11:12:33 AM