首页> 外文期刊>Journal of nuclear science and technology >Migration of 137Cs Adsorbed on Fine Soil Particles through Soil Layer, (II)Re-Suspension of Fine Soil Particles Filtrated by Unsaturated Soil Layer
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Migration of 137Cs Adsorbed on Fine Soil Particles through Soil Layer, (II)Re-Suspension of Fine Soil Particles Filtrated by Unsaturated Soil Layer

机译:吸附在土壤细颗粒上的137Cs通过土壤层的迁移,(II)不饱和土壤层过滤的细颗粒的再悬浮

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In order to study the migration behavior of 137Cs adsorbed on fine soil particles, distilled water was introduced into the unsaturated sandy soil column which filtrated the fine soil particles. From the concentrations of 137Cs in the effluent and in the soil column, it was found that fine soil particles filtrated by the soil layer were re-suspensible at the surface of soil layer and the amount of re-suspension per unit time was in proportion to the amount of filtrated fine soil particles. Considering the filtration of fine soil particles by soil layer, the reaction between soil layer and fine soil particles on which 137Cs is adsorbed is described by the formula ?Q/?t= K1C-K2Q at the surface of soil layer. Good agreement was obtained between the observed 137Cs concentration in the effluent and the predicted one employing ?Q/?t=K1C-K2Q and ?Q/?t=K1C as a reaction formula at the surface of soil layer and in the subsurface part of the soil layer, respectively.
机译:为了研究吸附在土壤细颗粒上的137Cs的迁移行为,将蒸馏水引入不饱和沙土柱中,以过滤土壤细颗粒。从废水和土壤柱中的137 Cs浓度中,发现由土壤层过滤的细小土壤颗粒可重新悬浮在土壤层表面,并且每单位时间的重新悬浮量与过滤后的细土壤颗粒的数量。考虑到通过土壤层对土壤细颗粒的过滤,土壤层与吸附了137Cs的土壤细颗粒之间的反应用土壤层表面的公式ΔQ/Δt= K1C-K2Q表示。在土壤层表面和地下部分,观察到的废水中137Cs浓度与使用ΔQ/Δt= K1C-K2Q和ΔQ/Δt= K1C作为反应公式的预测浓度之间取得了良好的一致性。土层。

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