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首页> 外文期刊>Mineralogical Magazine >Crystallization of the (Cd,Ca)CO3 solid solution in double diffusion systems: the partitioning behaviour of Cd~(2+) in calcite at different supersaturation rates
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Crystallization of the (Cd,Ca)CO3 solid solution in double diffusion systems: the partitioning behaviour of Cd~(2+) in calcite at different supersaturation rates

机译:双扩散系统中(Cd,Ca)CO3固溶体的结晶:方解石中Cd〜(2+)在不同过饱和率下的分配行为

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Considering an ideal solid solution, the partitioning of cadmium in calcite was studied at different levels of supersaturation (5) using counter-diffusion experiments. The effective (non-equilibrium) distribution coefficients of Cd~(2+) in calcite (D_(Cd)), varied between 20 and 100 depending on the initial concentration of reactants and the evolution of supersaturation. A function that relates the D_(Cd) with the supersaturation at nucleation was derived: logD_(Cd) = -0.401og delta + 2.42. The relationship obtained suggests that in natural waters, Cd~(2+) can be incorporated to a greater degree in calcite when the solid solution-aqueous solutions system is near to equilibrium, which can occur in scenarios where the supersaturation rate and hence the supersaturation level are relatively small.
机译:考虑到理想的固溶体,使用反扩散实验研究了在不同过饱和水平(5)下方解石中镉的分配。方解石(D_(Cd))中Cd〜(2+)的有效(非平衡)分布系数根据反应物的初始浓度和过饱和的演变在20到100之间变化。导出了将D_(Cd)与成核时的过饱和联系起来的函数:logD_(Cd)= -0.401og delta + 2.42。所获得的关系表明,在固溶体-水溶液体系接近平衡时,在自然水中,方解石中Cd〜(2+)的含量更高,这可能发生在过饱和率和过饱和率的情况下。级别都比较小。

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