State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, PR China.
State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, PR China; University of Chinese Academy of Sciences, Beijing, 100049, China.
Chemosphere. 2018 Apr;196:223-230. doi: 10.1016/j.chemosphere.2017.12.158. Epub 2017 Dec 27.
Microorganisms play a key role in the redox transformation of arsenic (As) in aquifers. In this study, the impact of indigenous bacteria, especially the prevailing nitrate respirers, on arsenite (As(III)) oxidation was explored during groundwater filtration using granular TiO and subsequent spent TiO anaerobic landfill. X-ray absorption near edge structure spectroscopy analysis showed As(III) oxidation (46% in 10 days) in the presence of nitrate in the simulated anaerobic landfills. Meanwhile, iron (Fe) species on the spent TiO were dominated by amorphous ferric arsenate, ferrihydrite and goethite. The Fe phase showed no change during the anaerobic landfill incubation. Batch incubation experiments implied that the indigenous bacteria completely oxidized As(III) to arsenate (As(V)) in 10 days using nitrate as the terminal electron acceptor under anaerobic conditions. The bacterial community analysis indicated that various kinds of microbial species exist in groundwater matrix. Phylogenetic tree analysis revealed that Proteobacteria was the dominant phylum, with Hydrogenophaga (34%), Limnohabitans (16%), and Simplicispira (7%) as the major bacterial genera. The nitrate respirers especially from the Hydrogenophaga genus anaerobically oxidized As(III) using nitrate as an electron acceptor instead of oxygen. Our study implied that microbes can facilitate the groundwater As oxidation using nitrate on the adsorptive media.
微生物在含水层中砷的氧化还原转化中起着关键作用。在本研究中,使用颗粒 TiO 和随后的废 TiO 厌氧填埋场过滤地下水时,探讨了土著细菌(尤其是主要的硝酸盐呼吸菌)对亚砷酸盐(As(III))氧化的影响。X 射线吸收近边结构光谱分析表明,在模拟厌氧填埋场中存在硝酸盐的情况下,As(III)被氧化(10 天内氧化了 46%)。同时,废 TiO 上的铁(Fe)物种主要由无定形铁砷酸盐、水铁矿和针铁矿组成。在厌氧填埋场孵育过程中,Fe 相没有发生变化。批量孵育实验表明,在厌氧条件下,土著细菌在 10 天内完全利用硝酸盐作为末端电子受体将 As(III)氧化为砷酸盐(As(V))。细菌群落分析表明,在地下水基质中存在各种微生物种类。系统发育树分析表明,变形菌门是优势门,其中氢噬菌属(34%)、Limnohabitans 属(16%)和 Simplicispira 属(7%)是主要的细菌属。硝酸盐呼吸菌,特别是氢噬菌属,在厌氧条件下,以硝酸盐为电子受体,而不是氧气,将 As(III)厌氧氧化。我们的研究表明,微生物可以利用吸附介质上的硝酸盐促进地下水 As 的氧化。