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IONIC STRENGTH AND PH DEPENDENCE OF SORPTION OF PD ONTO ILLITE, BENTONITE, AND SHALE

机译:PD在伊利石,膨润土和页岩上的吸附的离子强度和PH相关性

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This paper examines sorption of palladium (Pd) onto illite, sodium-bentonite MX-80, and Queenston shale, under aerobic conditions, for Na-Ca-Cl solutions with ionic strengths(I) ranging from 0.1-6 mol/L (M) and pH_c ranging from 3-9. Sorption decreased as I increased. At pH < 5 sorption increased, while for pH > 5 sorption was essentially constant. Surface complexation modelling (SCM) for sorption of Pd onto illite and montmorillonite was developed using PHREEQC and compared to the experimental results. The results showed some agreement to the experimental data, however, the general shapes did not match. SC constants were able to be optimized for 0.1 M.
机译:本文研究了好氧条件下离子强度(I)为0.1-6 mol / L(M)的Na-Ca-Cl溶液在伊利石,钠膨润土MX-80和Queenston页岩上钯(Pd)的吸附),pH_c为3-9。吸附量随我的增加而降低。在pH <5时,吸附增加,而在pH> 5时,吸附基本恒定。使用PHREEQC建立了将Pd吸附到伊利石和蒙脱石上的表面络合模型(SCM),并与实验结果进行了比较。结果表明与实验数据有些吻合,但是,一般形状不匹配。 SC常数能够针对0.1 M进行优化。

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