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通过模拟降雨研究外源硒在 3 种农业土壤中的淋溶行为及化学形态分布。

Leaching behaviors and chemical fraction distribution of exogenous selenium in three agricultural soils through simulated rainfall.

机构信息

College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China.

College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China; Key Laboratory of Plant Nutrition and the Agri-environment in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China.

出版信息

Ecotoxicol Environ Saf. 2019 May 30;173:393-400. doi: 10.1016/j.ecoenv.2019.02.042. Epub 2019 Feb 21.

Abstract

To clarify the leaching risk of selenium (Se) in agricultural soils, a laboratory column experiment was conducted to study the characteristics of leaching and chemical fractions of Se in three different soils treated with different levels of exogenous selenate under simulated local rainfall. Results demonstrated that the Se concentration in leachates of all tested soils decreased rapidly at the beginning of leaching and slowly decreased thereafter. After leaching, Se concentrations in leachates of all tested soils at 1, 3, and 6 mg/kg exogenous Se concentrations were 0.06-0.24, 0.25-0.84, and 0.60-1.65 mg/L, respectively, which exceeded the standard limit of the Chinese Environmental Quality Standards for Groundwater (<0.01 mg/L) (GB/T 14848-2017). The cumulative leached Se amount accounted for 51.27-86.22% of the total Se. Those results indicated the high risk of Se leaching in the tested soils. The Elovich model could better describe Se leaching processes in krasnozem, while the leaching processes of Se in black soil and loess soil accorded with the power function model. Se mainly existed in soluble fraction (61.33-81.05%) before leaching and residual fraction (48.91-68.04%) after leaching. The soluble and exchangeable Se fractions were the main contributors of Se in leachates. In addition, the parameters of the U and I values could well describe the distribution of Se fractions in soil during leaching. In general, more attention should be placed on the assessment of Se leaching in soil.

摘要

为了阐明农业土壤中硒(Se)的浸出风险,进行了一项实验室柱实验,以研究在模拟当地降雨条件下,用不同水平的外源硒酸盐处理三种不同土壤时硒的浸出特征和化学形态。结果表明,所有测试土壤中浸出液中的硒浓度在浸出初期迅速下降,随后缓慢下降。淋洗后,所有测试土壤中 1、3 和 6mg/kg外源硒浓度下的浸出液中硒浓度分别为 0.06-0.24、0.25-0.84 和 0.60-1.65mg/L,均超过中国地下水环境质量标准(GB/T 14848-2017)(<0.01mg/L)的标准限值。累积淋失硒量占总硒的 51.27-86.22%。这些结果表明,测试土壤中硒的淋失风险较高。Elovich 模型可以更好地描述克拉斯诺耶姆土壤中硒的淋失过程,而黑土和黄土土壤中硒的淋失过程符合幂函数模型。淋洗前硒主要以可溶态(61.33-81.05%)和残渣态(48.91-68.04%)存在。可溶态和交换态硒是淋出液中硒的主要贡献者。此外,U 和 I 值的参数可以很好地描述硒在土壤淋失过程中各形态的分布。总体而言,应更加关注土壤中硒淋失的评估。

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