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用于估算西班牙非饱和土壤中放射性铯和放射性锶吸附的扩散实验:与批量吸附数据的比较。

Diffusion experiments for estimating radiocesium and radiostrontium sorption in unsaturated soils from Spain: comparison with batch sorption data.

机构信息

Departament de Química Analítica, Universitat de Barcelona, Barcelona, Spain.

出版信息

J Hazard Mater. 2010 Sep 15;181(1-3):1072-9. doi: 10.1016/j.jhazmat.2010.05.124. Epub 2010 Jun 2.

Abstract

As sorption data obtained from batch tests are often used to estimate pollutant transport in unsaturated soils, comparison between sorption data obtained in the two conditions is required to ensure a correct risk assessment. With this aim, radiostrontium and radiocesium apparent diffusion coefficients (D(a)) were quantified in nine unsaturated soils, and the derived distribution coefficients (K(d)) were compared with K(d) data from batch experiments. The D(a)(Sr) and the D(a)(Cs) ranged from 1.8x10(-11) to 1.5x10(-10) m(2) s(-1), and from 1.0x10(-13) to 5.9x10(-11) m(2) s(-1), respectively. The D(a)(Sr) varied according to both soil packing parameters and properties governing Sr interaction. For Cs, the soil sorption properties explained the variation on D(a)(Cs). The K(d) values derived from D(a) (from 0.014 to 1.8 L kg(-1) for Sr; from 0.55 to 942 L kg(-1) for Cs) were lower than from batch tests (from 1 to 97 L kg(-1) for Sr; from 10 to 14,600 L kg(-1) for Cs), thus indicating that batch data may not accurately describe radionuclide transport in unsaturated soils. However, the two sets of data correlated well, thus suggesting that radionuclide transport can be estimated from batch tests, which are faster than diffusion experiments.

摘要

由于从批量测试中获得的吸附数据通常用于估计非饱和土壤中的污染物迁移,因此需要比较两种条件下获得的吸附数据,以确保正确的风险评估。为此,在 9 种非饱和土壤中量化了放射性锶和放射性铯的表观扩散系数(D(a)),并将得出的分配系数(K(d))与批量实验中的 K(d)数据进行了比较。D(a)(Sr)和 D(a)(Cs)的范围分别为 1.8x10(-11)至 1.5x10(-10) m(2) s(-1)和 1.0x10(-13)至 5.9x10(-11) m(2) s(-1)。D(a)(Sr)的变化取决于土壤填充参数和控制 Sr 相互作用的特性。对于 Cs,土壤吸附特性解释了 D(a)(Cs)的变化。从 D(a)得出的 K(d)值(Sr 的范围为 0.014 至 1.8 L kg(-1);Cs 的范围为 0.55 至 942 L kg(-1))低于批量测试(Sr 的范围为 1 至 97 L kg(-1);Cs 的范围为 10 至 14,600 L kg(-1)),这表明批量数据可能无法准确描述非饱和土壤中的放射性核素迁移。然而,这两组数据相关性很好,因此表明可以从批量测试中估计放射性核素迁移,批量测试比扩散实验更快。

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