Water Resources and Environmental Engineering Research Unit, University of Oulu, Oulu, Finland.
Environmental Geochemistry, Bayreuth Center for Ecology and Environmental Research (BayCEER), University of Bayreuth, Bayreuth, Germany.
Environ Microbiol. 2020 Apr;22(4):1572-1587. doi: 10.1111/1462-2920.14922. Epub 2020 Feb 6.
Mining operations produce large quantities of wastewater. At a mine site in Northern Finland, two natural peatlands are used for the treatment of mining-influenced waters with high concentrations of sulphate and potentially toxic arsenic (As). In the present study, As removal and the involved microbial processes in those treatment peatlands (TPs) were assessed. Arsenic-metabolizing microorganisms were abundant in peat soil from both TPs (up to 10 cells g ), with arsenate respirers being about 100 times more abundant than arsenite oxidizers. In uninhibited microcosm incubations, supplemented arsenite was oxidized under oxic conditions and supplemented arsenate was reduced under anoxic conditions, while little to no oxidation/reduction was observed in NaN -inhibited microcosms, indicating high As-turnover potential of peat microbes. Formation of thioarsenates was observed in anoxic microcosms. Sequencing of the functional genemarkers aioA (arsenite oxidizers), arrA (arsenate respirers) and arsC (detoxifying arsenate reducers) demonstrated high diversity of the As-metabolizing microbial community. The microbial community composition differed between the two TPs, which may have affected As removal efficiencies. In the present situation, arsenate reduction is likely the dominant net process and contributes substantially to As removal. Changes in TP usage (e.g. mine closure) with lowered water tables and heightened oxygen availability in peat might lead to re-oxidation and re-mobilization of bound arsenite.
采矿作业会产生大量废水。在芬兰北部的一个矿区,两个天然泥炭地被用于处理高浓度硫酸盐和潜在有毒砷(As)的受采矿影响的水。在本研究中,评估了这些处理泥炭地(TP)中砷的去除及其涉及的微生物过程。砷代谢微生物在两个 TP 的泥炭土中都很丰富(高达 10 细胞 g ),其中砷酸盐呼吸者的丰度比亚砷酸盐氧化者高约 100 倍。在未抑制的微宇宙培养中,有氧条件下补充的亚砷酸盐被氧化,而缺氧条件下补充的砷酸盐被还原,而在 NaN 抑制的微宇宙中几乎没有观察到氧化/还原,这表明泥炭微生物具有很高的砷转化潜力。在缺氧微宇宙中观察到硫代砷酸盐的形成。功能基因标志物 aioA(亚砷酸盐氧化者)、arrA(砷酸盐呼吸者)和 arsC(解毒砷酸盐还原者)的测序表明,砷代谢微生物群落具有很高的多样性。两个 TP 之间的微生物群落组成不同,这可能影响了 As 的去除效率。在当前情况下,砷酸盐还原可能是主要的净过程,并对 As 的去除有很大贡献。TP 使用的变化(例如矿山关闭)会降低地下水位并增加泥炭中的氧气可用性,这可能导致结合的亚砷酸盐重新氧化和再移动。