Evaporation also causes CaCO 3 to precipitate from water before NaCl, the latter
being a more soluble salt. The formation of CaCO 3 removes calcium ions from
the water, increasing the Na+: (Na++Ca^2 +) value. Data for rivers influenced by
evaporation plot along a diagonal B to B¢on Fig. 5.3, evolving toward a sea-
148 Chapter Five
Total dissolved salts (mg l
–1)
Ionic strength (mol l
–1
)
0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1.0
Weight ratio of Na/(Na+Ca)
10
100
1000
10 000
0.7
2 ¥ 10 –3
4 ¥ 10 –5
+= Seawater data
= Lake data
= River data
++
++
+
+
+
+
Mississippi B
Ganges
Lena
Niger
Orinoco
Weathering
dominance
Rainfall
dominance
Mobile
Congo
Lake Superior
Negro
A
A¢
Onyx
Ob Columbia
Yukon
Volga
Rio Grande
Colorado
Pecos
Pecos
Jordan
Caspian
Black
Major oceans
Salton Sea
Baltic
Evaporation
B¢
Fig. 5.3Variation of the weight ratio of Na/(Na+Ca) as a function of the total dissolved salts
and ionic strength for surface waters. Arrows represent chemical evolution of rivers from
source downstream. Modified from Science 170 , 1088–1090, Gibbs, R.J. Copyright (1970) by
the AAAS.