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嗜酸微生物介导的三价铁还原与元素硫或连四硫酸盐氧化耦合的速率及硫中间体的检测。

Rates of iron(III) reduction coupled to elemental sulfur or tetrathionate oxidation by acidophilic microorganisms and detection of sulfur intermediates.

机构信息

Federal Institute for Geosciences and Natural Resources (BGR), Stilleweg2, 30655 Hannover, Germany.

Federal Institute for Geosciences and Natural Resources (BGR), Stilleweg2, 30655 Hannover, Germany.

出版信息

Res Microbiol. 2024 Jan-Feb;175(1-2):104110. doi: 10.1016/j.resmic.2023.104110. Epub 2023 Aug 4.

Abstract

Bioleaching processes and acid mine drainage (AMD) generation are mainly driven by aerobic microbial iron(II) and inorganic sulfur/compound oxidation. Dissimilatory iron(III) reduction coupled to sulfur/compound oxidation (DIRSO) by acidophilic microorganisms has been described for anaerobic cultures, but iron reduction was observed under aerobic conditions as well. Aim of this study was to explore reaction rates and mechanisms of this process. Cell-specific iron(III) reduction rates for different Acidithiobacillus (At.) strains during batch culture growth or stationary phase with iron(III) (∼40 mM) as electron acceptor and elemental sulfur or tetrathionate as electron donor (1% or 5 mM, respectively) were determined. The rates were highest under anaerobic conditions for the At. ferrooxidans type strain with 6.8 × 10 and 1.1 × 10 reduced iron(III) ions per second per cell for growth on elemental sulfur and tetrathionate, respectively. The iron(III) reduction rates were somehow lower for the anaerobically sulfur grown archaeon Ferroplasma acidiphilum, and lowest for the sulfur grown At. caldus type strain under aerobic conditions (1.7 × 10 and 7.3 × 10 reduced iron(III) ions per second per cell, respectively). The rates for five strains of At. thiooxidans (aerobe) were in between those for At. ferrooxidans (anaerobe) and At. caldus (aerobe). There was no pronounced pH dependence of iron(III) reduction rates in the range of pH 1.0-1.9 for the type strains of all species but rates increased with increasing pH for four other At. thiooxidans strains. Thiosulfate as sulfur intermediate was found for At. ferrooxidans during anaerobic growths on tetrathionate and iron(III) but not during anaerobic growths on elemental sulfur and iron(III), and a small concentration was measured during aerobic growths on tetrathionate without iron(III). For the At. thiooxidans type strain thiosulfate was found with tetrathionate grown cells under aerobic conditions in presence and absence of iron(III), but not with sulfur grown cells. Evidence for hydrogen sulfide production at low pH was found for the At. ferrooxidans as well as the At. thiooxidans type strains during microaerophilic growth on elemental sulfur and for At. ferrooxidans during anaerobic growths on tetrathionate and iron(III). The occurrence of sulfur compound intermediates supports the hypothesis that chemical reduction of iron(III) ions takes place by sulfur compounds released by the microbial cells.

摘要

生物浸出过程和酸性矿山排水 (AMD) 的产生主要由需氧微生物亚铁 (II) 和无机硫/化合物氧化驱动。好氧微生物的异化铁 (III) 还原与硫/化合物氧化偶联 (DIRSO) 已在厌氧培养物中得到描述,但在好氧条件下也观察到铁还原。本研究旨在探索该过程的反应速率和机制。在分批培养生长或静止阶段,用铁 (III)(约 40 mM)作为电子受体,用元素硫或连四硫酸盐作为电子供体(分别为 1%或 5 mM),测定了不同嗜酸硫杆菌 (At.) 菌株的细胞特异性铁 (III) 还原率。在铁 (III) 还原率方面,对于以元素硫和连四硫酸盐为电子供体的 At. ferrooxidans 型菌株,在厌氧条件下最高,分别为每秒每细胞 6.8×10 和 1.1×10 个还原铁 (III) 离子。对于厌氧生长的硫杆菌 Ferroplasma acidiphilum,铁 (III) 还原率略低,而在好氧条件下,以硫为生长基质的 At. caldus 型菌株最低(分别为每秒每细胞 1.7×10 和 7.3×10 个还原铁 (III) 离子)。五种 At. thiooxidans 菌株(需氧菌)的铁 (III) 还原率介于 At. ferrooxidans(厌氧菌)和 At. caldus(需氧菌)之间。对于所有种的典型菌株,铁 (III) 还原率在 pH 1.0-1.9 范围内没有明显的 pH 依赖性,但对于其他四种 At. thiooxidans 菌株,铁 (III) 还原率随 pH 的增加而增加。在厌氧条件下,在连四硫酸盐和铁 (III) 上生长时发现了硫代硫酸盐作为硫中间体,但在厌氧条件下,在元素硫和铁 (III) 上生长时则没有发现,在有氧条件下,在没有铁 (III) 的情况下,在连四硫酸盐上生长时也测量到了少量的硫代硫酸盐。对于 At. thiooxidans 典型菌株,在有氧条件下,用连四硫酸盐培养细胞时,无论是否存在铁 (III),都发现了硫代硫酸盐,但在以硫为生长基质的细胞中则没有发现。在微需氧条件下,以元素硫为生长基质的 At. ferrooxidans 以及 At. thiooxidans 典型菌株在微需氧条件下生长时以及在厌氧条件下以连四硫酸盐和铁 (III) 生长时,都发现了硫化氢的产生证据。硫化合物中间产物的存在支持了这样一种假设,即铁 (III) 离子的化学还原是由微生物细胞释放的硫化合物发生的。

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