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Soil-Soil Solution Distribution Coefficients for Se, Sr, Sn, Sb, And Cs in Japanese Agricultural Soils

机译:日本农业土壤中SE,SR,Sn,Sb和Cs的土壤 - 土壤溶液分布系数

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In this study, soil-soil solution distribution coefficients (K_(d~s)) for five radionuclides (Se-75, Sr-85, Sn-113, Sb-124, and Cs-137) were determined by batch sorption tests in 142 Japanese agricultural soil samples (63 paddy soil and 79 upland soil samples). The results showed that Se- and Sb-K_d data did not have a normal or a log-normal distribution, but Sr-, Sn-, and Cs-K_d data did have a log-normal distribution. Further, Se-, Sr-, and Cs-K_d values differed between paddy and upland soil samples in t-test (p < 0.05). Spearman's rank correlation test was carried out to investigate correlations between K_d values for each radionuclide and soil properties. The combination of the K_d value and the soil property having the highest correlation coefficient (R_s) for each radionuclide was as follows: Se-K_d - concentration of water soluble P (R_s = -0.51); Sr-K_d - concentration of water soluble Ca (R_s = -0.57); Sn-K_d -concentration of water soluble Sr (R_s = 0.57); and Sb-K_d - concentration of water soluble P (R_s = -0.67). Although there were no soil properties which had a good correlation with Cs-K_d values for all soil samples, the best correlated soil property with Cs-K_d values was concentration of water soluble ammonium ion (R_s = -0.48) for upland soil samples.
机译:在这项研究中,土壤土壤溶液分配系数(K_(d〜s))为5倍的放射性核素(SE-75,SR-85系,Sn-113,SB-124,和Cs-137)通过以分批吸附试验确定142个日本农业土壤样品(63水稻土和79个旱地土壤样品)。结果表明,SE-和SB-K_D数据没有一个正常或对数正态分布,但Sr基,Sn的,和CS-K_D数据也有一个对数正态分布。此外,SE-,Sr基和Cs-K_D值在t检验(P <0.05)和稻田旱地土壤样品之间不同。 Spearman秩相关检验进行调查每个放射性核素和土壤性质K_D值之间的相关性。的K_D值并具有用于每个放射性核素最高相关系数(R_S)土壤属性的组合如下:硒K_D - 水溶性P的浓度(R_S = -0.51); SR-K_D - 水溶性的Ca浓度(R_S = -0.57);水溶性锶(R_S = 0.57)的Sn系K_D - 浓度;和Sb-K_D - 水溶性P的浓度(R_S = -0.67)。虽然有一个已用铯K_D值对于所有的土样的良好相关性没有土壤性质,与铯K_D值的最佳相关土壤性质是水溶性的铵离子(R_S = -0.48),用于旱地土壤样品的浓度。

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