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Calcite and aragonite growth rate experiments have been performed in the presence of aqueous Ba at 25 °C using the constant addition technique as a function of CaCO3 mineral growth rate (mol/m2/s). The partitioning of Ba in calcite at −8.4 ≤ Logrcalcite ≤ −7.3 exhibits a weak dependence on growth rate that can be expressed as:LogDBa,calcite=0.2477±0.0543×Logrcalcite-0.2949±0.4222;R2=0.81In the case...
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