Se(Ⅳ)在伊利石-蒙脱石混合物中的扩散行为

Se(Ⅳ) Diffusion Behavior in Illite-Montmorillonite Mixture

  • 摘要: 采用贯穿扩散法研究了Se(Ⅳ)(代替79Se(Ⅳ))在伊利石-蒙脱石混合物中的扩散行为。结果表明,蒙脱石的伊利石化对Se(Ⅳ)的迁移行为有明显影响,Se(Ⅳ)的有效扩散系数De从3.89×10-11 m2/s增加至18.1×10-11m2/s。伊利石-蒙脱石混合物比例为1∶9~5∶5时,De的变化不明显,伊利石-蒙脱石混合物比例为6∶4时,De明显增大,表明矿物的优势组分对Se(Ⅳ)的扩散行为起主导作用。随着伊利石-蒙脱石混合物比例从1∶9增大至6∶4,Se(Ⅳ)的岩石容量因子由4.07降低至0.75,分配系数由22.7×10-4 m3/kg降低至1.95×10-4 m3/kg,它们均随伊利石含量的增加而降低,这表明由于伊利石对Se(Ⅳ)的吸附能力较蒙脱石弱,导致伊利石-蒙脱石混合物对Se(Ⅳ)的阻滞能力变弱,从而增大了Se(Ⅳ)的迁移能力。

     

    Abstract: The diffusion behavior of Se(Ⅳ) (surrogate to 79Se (Ⅳ)) in illite-montmorillonite mixture was investigated by through-diffusion method. The results show that the migration of Se(Ⅳ) is altered significantly by the illitization of montmorillonite. The effective diffusion coefficient of Se(Ⅳ) increases from 3.89×10-11 m2/s to 18.1×10-11 m2/s. When the illite-montmorillonite ratio is in the range of 1∶9 and 5∶5, De values have no obvious change. Whereas, De values increase significantly at illite montmorillonite ratio of 6∶4, indicating that the predominant composition of the mineral clay plays a leading role in Se(Ⅳ) diffusion. When the illite-montmorillonite ratio increases from 1∶9 to 6∶4, the rock capacity and distribution coefficient of Se(Ⅳ) decrease from 4.07 to 0.75 and from 22.7×10-4 m3/kg to 1.95×10-4 m3/kg, respectively. Both of them decrease with the increase of illite content. It demonstrates that the hindrance of illite-montmorillonite mixture turns worse due to the weaker sorption of Se(Ⅳ) on illite, leading the increase of Se(Ⅳ) migration in illite-montmorillonite mixture.

     

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