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Surface spectroscopic studies of Cs+, and Ba2+ sorption on chlorite-illite mixed clay

机译:亚氯酸盐-伊利石混合黏土对Cs +和Ba2 +吸附的表面光谱研究

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The sorption behavior of Cs+, and Ba2+ on natural clay was investigated using ToF-SWIS, XPS, and XRD. The natural clay was composed mainly of chlorite and illite in addition to quartz and calcite. Depth profiling up to 70 Angstrom was performed at 10 Angstrom steps utilizing ToF-SIMS to study the amount of sorbed Cs+ and Ba2+ as a function of depth in the clay matrix. The results suggest that Cs+ and Ba2+ ions were sorbed primarily by ion exchange coupled with hydrolytic sorption. According to ToF-SIMS and XPS results, the total sorbed amount of Ba2+ was larger than that of Cs+. Quantitative determination of the primary cations within the analyzed clay before and after sorption indicated that for Ba2+ sorption, Ca2+, Mg2+ and for Cs+ sorption Ca2+ K+ were the major exchanging ions. The XRD spectra of Ba-sorbed clay contained new peaks that were identified as BaCO3. [References: 10]
机译:使用ToF-SWIS,XPS和XRD研究了Cs +和Ba2 +在天然粘土上的吸附行为。除了石英和方解石外,天然粘土还主要由亚氯酸盐和伊利石组成。使用ToF-SIMS以10埃的步长进行了高达70埃的深度剖析,研究了粘土基质中Cs +和Ba2 +的吸附量随深度的变化。结果表明,Cs +和Ba2 +离子主要通过离子交换结合水解吸附而被吸附。根据ToF-SIMS和XPS结果,Ba2 +的总吸附量大于Cs +。吸附前后定量分析粘土中的主要阳离子表明,对于Ba2 +吸附,Ca2 +,Mg2 +和Cs +吸附Ca2 + K +是主要的交换离子。钡吸附的粘土的XRD谱图包含新峰,被确认为BaCO3。 [参考:10]

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