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不同微生物状态下含氧砂质土壤中硒的水相、固相和气态分配

Aqueous, solid and gaseous partitioning of selenium in an oxic sandy soil under different microbiological states.

作者信息

Darcheville O, Février L, Haichar F Z, Berge O, Martin-Garin A, Renault P

机构信息

Laboratory of Radioecology and Ecotoxicology, IRSN/DEI/SECRE, Building 186, Cadarache, B.P. 3, 13115 Saint Paul-lez-Durance Cedex, France.

出版信息

J Environ Radioact. 2008 Jun;99(6):981-92. doi: 10.1016/j.jenvrad.2007.11.006. Epub 2008 Mar 4.

Abstract

The aim of this study was to investigate the role of microorganisms on the behaviour of selenium in natural soil maintained under strictly aerobic conditions. Six-day batch experiments were performed with soils constrained to different microbiological states, either by sterilisation or by adding organic substrates. Selenium was added to the soil as selenite. The distribution of selenium in the gaseous, liquid and solid phases of the batch was measured. Selenium partitioning between the various solid phases was investigated by chemical sequential extractions. Active microorganisms played major effects on the distribution of selenium within the soil. On the one hand, microorganisms could promote selenium volatilisation (in relatively small amounts), leading to the spreading of selenium compounds outside the soil. On the other hand, microbial activities increased both amount of selenium retained by the soil and the strength of its retention (less exchangeable selenium), making selenium less susceptible to remobilisation.

摘要

本研究的目的是调查微生物在严格需氧条件下的天然土壤中对硒行为的作用。通过灭菌或添加有机底物,对处于不同微生物状态的土壤进行了为期六天的批次实验。以亚硒酸盐的形式向土壤中添加硒。测量了批次中硒在气相、液相和固相中 的分布。通过化学连续萃取研究了硒在各种固相之间的分配。活性微生物对土壤中硒的分布起主要作用。一方面,微生物可促进硒的挥发(量相对较小),导致硒化合物在土壤外扩散。另一方面,微生物活动增加了土壤保留的硒量及其保留强度(可交换硒减少),使硒不易被重新活化。

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