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The document discusses calculations related to redox reactions, isotope fractionation, and the properties of groundwater. It includes detailed steps for determining the measured Eh of a solution, δ18O values for rain, enrichment factors for isotope reactions, and the saturation of calcite in groundwater. Key findings include the calculated Eh of -0.22 V, δ18O of rain at -7.8‰, and a saturation index of 1.00 for calcite.

Author

Cheikh Sohibou

Language

EN