Abstract
The contents of basic salt components in the continental discharge related to weathering processes were calculated taking into account the atmospheric transfer of soluble salts from the ocean and their supply from anthropogenic sources. Real water migration coefficients characterizing the mobility of chemical elements in the hypergenesis zone were calculated on the basis of these data. It has been shown that the water migration coefficient directly depends on the solubility of basic minerals that are stable in the hypergenesis zone.
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Savenko, V.S. Water migration coefficients of chemical elements in the hypergenesis zone. Lithol Miner Resour 35, 345–350 (2000). https://doi.org/10.1007/BF02782690
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DOI: https://doi.org/10.1007/BF02782690