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Between Carbonate Minerals and Solutions

Rimstidt JD, Balog A, Webb J (1998) Distribution of trace elements between carbonate minerals and aqueous solutions. Geochim Cosmochim Acta 62 1851-1863... [Pg.428]

The latter two assumptions are simplistic, considering the number of factors that affect pH and oxidation state in the oceans (e.g., Sillen, 1967 Holland, 1978 McDuff and Morel, 1980). Consumption and production of CO2 and O2 by plant and animal life, reactions among silicate minerals, dissolution and precipitation of carbonate minerals, solute fluxes from rivers, and reaction between convecting seawater and oceanic crust all affect these variables. Nonetheless, it will be interesting to compare the results of this simple calculation to observation. [Pg.82]

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