Using 3H and 14C to constrain the degree of closed-system dissolution of calcite in groundwater
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Authors
Cartwright, Ian
Fifield, L Keith
Morgenstern, Uwe
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Pergamon Press
Abstract
This study uses 3H concentrations, 14C activities (a14C), 87Sr/86Sr ratios, and δ13C values to constrain calcite dissolution in groundwater from the Ovens catchment SE Australia. Taken in isolation, the δ13C values of dissolved organic C (DIC) and 87Sr/
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Applied Geochemistry
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2037-12-31