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Evaluation of Sorption Distribution Coefficient of Cs onto Granite using Sorption Data Collected in Sorption Database and Sorption Model

机译:使用吸附数据库和吸附模型中CS在花岗岩中的吸附分布系数评价

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Based on the sorption distribution coefficients (K_d) of Cs onto granite collected from the JAERI Sorption Database (SDB), the parameters for a two-site model without the triple-layer structure were optimized. Comparing the experimentally measured K_d values of Cs onto Mizunami granite carried out by JAEA with the K_d values predicted by the model, the effect of the ionic strength on the K_d values of Cs onto granite was evaluated. It was found that K_d values could be determined using the content of biotite in granite at a sodium concentration ([Na]) of 1 × 10~(-2) to 5 × 10~(-1) mol/dm~3. It was suggested that in high ionic strength solutions, the sorption of Cs onto other minerals such as microcline should also be taken into account.
机译:基于Cs的吸附分布系数(K_D)在从jaeri吸附数据库(SDB)收集的花岗岩上,优化了没有三层结构的双站点模型的参数。将CS的实验测量的K_D值与JAEA对模型预测的K_D值进行了比较,评价了离子强度对Cs在花岗岩上的K_D值上的影响。发现可以使用1×10〜(-2)至5×10〜(-1)mol / dm〜3的钠浓度([Na])的花岗岩中的Bancotite的含量确定K_D值。建议在高离子强度溶液中,还应考虑CS在其他矿物质中的其他矿物质中的吸附。

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