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Activation energy for diffusion of chloride ions in compacted sodium montmorillonite

机译:氯离子在致密钠蒙脱石中扩散的活化能

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Diffusion of chloride ions in compacted montmorillonite was studied for a performance assessment as buffer material in geological disposal of high-level radioactive waste. The apparent diffusion coefficients were from 6.8×10~-12 to 2.2×10~-10 m~2 s~-1 for sodium montmorillonite at dry densities from 1.0 to 1.8 Mg m~-3 at diffusion temperatures from 278 to 323 K. The activation energy increased from 14 kJ mol~-1(lower than that in free water, 17.4 kJ mol~-1)to 25 kJ mol~-1(higher than that in free water), as the dry density increased from 1.0 to 1.8 Mg m~-3.
机译:研究了氯离子在压实蒙脱土中的扩散,作为缓冲材料在高放废物地质处置中的性能评估。在278〜323 K的扩散温度下,干密度为1.0〜1.8 Mg m〜-3时,蒙脱土钠的表观扩散系数为6.8×10〜-12至2.2×10〜-10 m〜2 s -1。随着干密度从1.0增加到25 kJ mol〜-1(比自由水高),活化能从14 kJ mol〜-1(比自由水低17.4 kJ mol〜-1)增加到25 kJ mol〜-1(比自由水高)。 1.8 Mg m〜-3。

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