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硫物种如何加速有毒硒氧阴离子的生物固定并促进稳定的六方硒形成。

How sulfur species can accelerate the biological immobilization of the toxic selenium oxyanions and promote stable hexagonal Se formation.

机构信息

Department of Environmental Technology, Wageningen University and Research, the Netherlands.

Department of Environmental Technology, Wageningen University and Research, the Netherlands.

出版信息

J Hazard Mater. 2022 Sep 5;437:129367. doi: 10.1016/j.jhazmat.2022.129367. Epub 2022 Jun 14.

DOI:10.1016/j.jhazmat.2022.129367
PMID:35897181
Abstract

Toxic selenium oxyanions and sulfur species are often jointly present in contaminated waters and soils. This study investigated the effect on kinetics and resulting products for bio-reduction of selenium oxyanions in the presence of biologically produced sulfur resulting from bio-oxidation of sulfide in (bio)gas-desulfurization (bio-S) and of sulfate. Selenite and selenate (~2 mmol L) bio-reduction was studied in batch up to 28 days at 30 C and pH 7 using lactic acid and a sulfate-reducing sludge, 'Emmtec'. Bio-S addition increased the selenite removal rate, but initially slightly decreased selenate reduction rates. Selenite reacted with biologically generated sulfide resulting in selenium-sulfur, which upon further bio-reduction creates a sulfur bio-reduction cycle. Sulfate addition increased the bio-reduction rate for both selenite and sulfate. Bio-S or sulfate promoted hexagonal selenium formation, whereas without these, mostly amorphous Se resulted. With another inoculum, 'Eerbeek', bio-S accelerated the selenite reduction rate less than for 'Emmtec' because of lower sulfur and higher selenite bio-reduction rates. Bio-S addition increased the selenate reduction rate slightly and accelerated hexagonal selenium formation. Hexagonal selenium formation is advantageous because it facilitates separation and recovery and is less mobile and toxic than amorphous Se. Insights into the interaction between selenium and sulfur bio-reduction are valuable for understanding environmental pathways and considerations regarding remediation and recovery.

摘要

有毒硒氧阴离子和硫物种通常共同存在于受污染的水和土壤中。本研究调查了在生物氧化硫化物产生的生物硫(生物-S)和硫酸盐存在下,硒氧阴离子生物还原的动力学和产物的影响。在 30°C 和 pH 7 下,使用乳酸和硫酸盐还原污泥 'Emmtec',在批处理中研究了硒酸盐和硒酸盐(~2 mmol L)的生物还原,直到 28 天。生物-S 的添加增加了亚硒酸盐的去除率,但最初略微降低了硒酸盐的还原率。亚硒酸盐与生物生成的硫化物反应生成硒-硫,随后进一步生物还原产生硫生物还原循环。硫酸盐的添加增加了亚硒酸盐和硫酸盐的生物还原速率。生物-S 或硫酸盐促进了六方硒的形成,而没有这些则主要形成无定形硒。对于另一种接种物 'Eerbeek',由于硫和亚硒酸盐生物还原率较低,生物-S 对亚硒酸盐还原速率的加速作用小于 'Emmtec'。生物-S 的添加略微增加了硒酸盐的还原速率,并加速了六方硒的形成。六方硒的形成是有利的,因为它便于分离和回收,并且比无定形硒的移动性和毒性更小。了解硒和硫生物还原之间的相互作用对于理解环境途径以及修复和回收方面的考虑因素非常有价值。

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