Zhou Yu-Hang, Wang Can, Liu Hong-Chang, Xue Zhen, Nie Zhen-Yuan, Liu Yue, Wan Jiao-Li, Yang Yu, Shu Wen-Sheng, Xia Jin-Lan
Key Lab of Biometallurgy of Ministry of Education of China, School of Minerals Processing and Bioengineering, Central South University, Changsha, China.
School of Life Sciences, South China Normal University, Guangzhou, China.
Front Microbiol. 2022 Feb 9;12:819804. doi: 10.3389/fmicb.2021.819804. eCollection 2021.
It is well known that speciation transformations of As(III) vs. As(V) in acid mine drainage (AMD) are mainly driven by microbially mediated redox reactions of Fe and S. However, these processes are rarely investigated. In this study, columns containing mine water were inoculated with two typical acidophilic Fe/S-oxidizing/reducing bacteria [the chemoautotrophic and the heterotrophic ], and three typical energy substrates (Fe, S, and glucose) and two concentrations of As(III) (2.0 and 4.5 mM) were added. The correlation between Fe/S/As speciation transformation and bacterial depth distribution at three different depths, i.e., 15, 55, and 105 cm from the top of the columns, was comparatively investigated. The results show that the cell growth at the top and in the middle of the columns was much more significantly inhibited by the additions of As(III) than at the bottom, where the cell growth was promoted even on days 24-44. dominated over in most samples collected from the three depths, but the elevated proportions of were observed in the top and bottom column samples when 4.5 mM As(III) was added. Fe bio-oxidation and Fe reduction coupled to As(III) oxidation occurred for all three column depths. At the column top surfaces, jarosites were formed, and the addition of As(III) could lead to the formation of the amorphous FeAsO⋅2HO. Furthermore, the higher As(III) concentration could inhibit Fe bio-oxidation and the formation of FeAsO⋅2HO and jarosites. S oxidation coupled to Fe reduction occurred at the bottom of the columns, with the formations of FeAsO⋅2HO precipitate and S intermediates. The formed FeAsO⋅2HO and jarosites at the top and bottom of the columns could adsorb to and coprecipitate with As(III) and As(V), resulting in the transfer of As from solution to solid phases, thus further affecting As speciation transformation. The distribution difference of Fe/S energy substrates could apparently affect Fe/S/As speciation transformation and bacterial depth distribution between the top and bottom of the water columns. These findings are valuable for elucidating As fate and toxicity mediated by microbially driven Fe/S redox in AMD environments.
众所周知,酸性矿山排水(AMD)中As(III)与As(V)的形态转化主要由铁和硫的微生物介导氧化还原反应驱动。然而,这些过程很少被研究。在本研究中,向装有矿井水的柱体中接种了两种典型的嗜酸铁/硫氧化/还原细菌[化能自养菌和异养菌],并添加了三种典型的能量底物(铁、硫和葡萄糖)以及两种浓度的As(III)(2.0和4.5 mM)。比较研究了柱体顶部以下15、55和105 cm三个不同深度处铁/硫/砷形态转化与细菌深度分布之间的相关性。结果表明,与柱体底部相比,添加As(III)对柱体顶部和中部的细胞生长抑制作用更为显著,在柱体底部,即使在第24 - 44天细胞生长也得到促进。在从三个深度采集的大多数样品中, 占主导地位,但当添加4.5 mM As(III)时,在柱体顶部和底部样品中观察到 的比例升高。在所有三个柱体深度处均发生了铁生物氧化以及与As(III)氧化耦合的铁还原反应。在柱体顶部表面形成了黄钾铁矾,添加As(III)会导致形成无定形的FeAsO·2H₂O。此外,较高的As(III)浓度会抑制铁生物氧化以及FeAsO·2H₂O和黄钾铁矾的形成。在柱体底部发生了与铁还原耦合的硫氧化反应,形成了FeAsO·2H₂O沉淀和硫中间体。在柱体顶部和底部形成的FeAsO·2H₂O和黄钾铁矾可以吸附As(III)和As(V)并与之共沉淀,导致砷从溶液转移到固相,从而进一步影响砷的形态转化。铁/硫能量底物的分布差异显然会影响水柱顶部和底部之间的铁/硫/砷形态转化和细菌深度分布。这些发现对于阐明AMD环境中微生物驱动的铁/硫氧化还原介导的砷归宿和毒性具有重要价值。