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Non-linear coupling of geochemical reservoirs

A different weathering reaction proposed by Berner et al. (1983) involves HC03 instead, but is entirely equivalent to the present equation when HC03 dissociation is taken into account. [Pg.394]

Carbonic acid is diprotic and its dissociation may be written with the two equations [Pg.394]

Combining the last three equations gives the C02 pressure as a function of the speciation of carbonates [Pg.394]

Writing for short p=pCo2 =Ca2+, y=Z(C02), and label with the subscript r the riverine values. The alkalinity A of a solution (Stumm and Morgan, 1981) is defined as its neutralizing capacity [Pg.395]

Subtracting (7.4.14 ) from (7.4.15) and turning to the short notation results in [Pg.395]


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