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硫酸盐呼吸细菌将硒酸盐还原为硒化物:细胞悬浮液和河口沉积物的实验。

Reduction of selenate to selenide by sulfate-respiring bacteria: experiments with cell suspensions and estuarine sediments.

机构信息

U.S. Geological Survey, Menlo Park, California 94025.

出版信息

Appl Environ Microbiol. 1987 Jun;53(6):1365-9. doi: 10.1128/aem.53.6.1365-1369.1987.

Abstract

Washed cell suspensions of Desulfovibrio desulfuricans subsp. aestuarii were capable of reducing nanomolar levels of selenate to selenide as well as sulfate to sulfide. Reduction of these species was inhibited by 1 mM selenate or tungstate. The addition of 1 mM sulfate decreased the reduction of selenate and enhanced the reduction of sulfate. Increasing concentrations of sulfate inhibited rates of selenate reduction but enhanced sulfate reduction rates. Cell suspensions kept in 1 mM selenate were incapable of reducing either selenate or sulfate when the selenate/sulfate ratio was >/=0.02, indicating that irreversible inhibition occurs at high selenate concentrations. Anoxic estuarine sediments having an active flora of sulfate-respiring bacteria were capable of a small amount of selenate reduction when ambient sulfate concentrations were low (<4 mM). These results indicate that sulfate is an inhibitor of the reduction of trace quantities of selenate. Therefore, direct reduction of traces of selenate to selenide by sulfate-respiring bacteria in natural environments is constrained by the ambient concentration of sulfate ions. The significance of this observation with regard to the role sediments play in sequestering selenium is discussed.

摘要

脱硫脱硫弧菌亚种的洗涤细胞悬浮液能够将亚硒酸盐还原为硒化物,以及将硫酸盐还原为硫化物。这些物质的还原受到 1mM 硒酸盐或钨酸盐的抑制。添加 1mM 硫酸盐会降低亚硒酸盐的还原,并增强硫酸盐的还原。硫酸盐浓度的增加会抑制亚硒酸盐还原的速率,但会增强硫酸盐还原的速率。当亚硒酸盐/硫酸盐比值≥0.02 时,保持在 1mM 硒酸盐中的细胞悬浮液不能还原亚硒酸盐或硫酸盐,这表明在高硒酸盐浓度下会发生不可逆抑制。当环境中硫酸盐浓度较低(<4mM)时,具有活跃硫酸盐呼吸细菌群落的缺氧河口沉积物能够进行少量的亚硒酸盐还原。这些结果表明硫酸盐是痕量亚硒酸盐还原的抑制剂。因此,在自然环境中,硫酸盐呼吸细菌直接将痕量的亚硒酸盐还原为硒化物受到环境中硫酸盐离子浓度的限制。讨论了这一观察结果对于沉积物在固定硒方面的作用的意义。

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