期刊
GEOCHIMICA ET COSMOCHIMICA ACTA
卷 72, 期 6, 页码 1498-1512出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.gca.2008.01.014
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Time-dependent sorption and desorption of Cd on calcite was studied over 2 10 days utilizing Cd-109 as a tracer to distinguish between 'labile' and 'non-labile' forms of sorbed Cd. Stabilizing the calcite suspensions for 12 months under atmospheric P-CO2 and controlled temperature was necessary to reliably follow Cd dynamics following initial sorption. Results revealed time-dependant Cd sorption and marked desorption hysteresis by calcite under environmentally relevant conditions. Data obtained were fitted to a first-order kinetic model and a concentric shell diffusion model. Both models described the progressive transfer of Cd2+ to a less reactive form within calcite and subsequent desorption of Cd subject to different initial tact times. The kinetic model provided a better fit to the combined sorption and desorption data (R-2 = 0.992). It differentiates between two 'pools' of sorbed Cd2+ on calcite, 'labile' and 'non-labile', in which labile sorbed Cd is in immediate equilibrium with the free Cd2+ ion activity in solution whereas non-labile Cd is kinetically restricted. For the diffusion model (R-2 = 0.959), the rate constants describing Cd dynamics in calcite produced a half-life for Cd desorption of similar to 175 d, for release to a 'zero-sink' solution. Results from this study allow comment on the likely mechanisms occurring at the calcite surface following long-term Cd sorption. (C) 2008 Published by Elsevier Ltd.
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