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Simultaneous Release of Fe and As during the Reductive Dissolution of Pb-As Jarosite by Shewanella putrefaciens CN32

机译:腐烂希瓦氏菌CN32还原Pb-As黄铁矿中Fe和As的同时释放

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摘要

Jarosites are produced during metallurgical processing, on oxidized sulfide deposits, and in acid mine drainage environments. Despite the environmental relevance of jarosites, few studies have examined their biogeochemical stability. This study demonstrates the simultaneous reduction of structural Fe(Ⅲ) and aqueous As(Ⅴ) during the dissolution of synthetic Pb-As jarosite (PbFe_3(SO_4,AsO_4)_2(OH)_6) by Shewanella putrefaciens using batch experiments under anaerobic circumneutral conditions. Fe(Ⅲ) reduction occurred immediately in inoculated samples while As(Ⅴ) reduction was observed after 72 h. XANES spectra showed As(Ⅲ) (14.7%) in the solid phase at 168 h coincident with decreased aqueous As(Ⅴ). At 336 h, XANES spectra and aqueous speciation analysis demonstrated 20.2% and 3.0% of total As was present as As(Ⅲ) in the solid and aqueous phase, respectively. In contrast, 12.4% of total Fe was present as aqueous Fe(Ⅱ) and was below the detection limits of XANES in the solid phase. TEM-EDS analysis at 336 h showed secondary precipitates enriched in Fe and O with minor amounts of As and Pb. Based on experimental data and thermodynamic modeling, we suggest that structural Fe(Ⅲ) reduction was thermodynamically driven while aqueous As(Ⅴ) reduction was triggered by detoxification induced to offset the high As(V) (328 μM) concentrations released during dissolution.
机译:在冶金过程中,氧化的硫化物沉积物上以及酸性矿山排水环境中都产生了铁矾。尽管与黄铁矿在环境方面相关,但很少有研究检查其生物地球化学稳定性。这项研究表明在厌氧性环境条件下使用腐乳假单胞菌分解了合成的Pb-As黄钾铁矾(PbFe_3(SO_4,AsO_4)_2(OH)_6)的过程中同时还原了结构Fe(Ⅲ)和As(Ⅴ)水溶液。接种样品中Fe(Ⅲ)立即还原,而72h后As(Ⅴ)还原。 XANES谱图显示168 h固相中As(Ⅲ)(14.7%)与含水As(Ⅴ)降低同时发生。在336 h,XANES光谱和水形态分析表明,固相和水相中分别以As(Ⅲ)形式存在的总As占20.2%和3.0%。相比之下,Fe(Ⅱ)的水溶液中总铁含量为12.4%,低于固相中XANES的检出限。 336 h的TEM-EDS分析表明,次生沉淀物富含Fe和O,以及少量的As和Pb。根据实验数据和热力学模型,我们认为热力学驱动结构Fe(Ⅲ)的还原,而排毒则触发了As(Ⅴ)水溶液的还原,以抵消溶解过程中释放的高As(V)(328μM)浓度。

著录项

  • 来源
    《Environmental Science & Technology》 |2012年第23期|12823-12831|共9页
  • 作者单位

    Great Lakes Institute for Environmental Research, University of Windsor, Windsor, Ontario N9B 3P4, Canada,Ecohydrology Research Group, Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario N2L 3G1, Canada;

    Great Lakes Institute for Environmental Research, University of Windsor, Windsor, Ontario N9B 3P4, Canada;

    Department of Mineralogy, The Natural History Museum, Cromwell Road, London, SW7 5BD, U.K.,Davy Faraday Research Laboratory, The Royal Institution of Great Britain, 21 Albemarle Street, London, W1S 4BS, U.K.,Department of Earth and Planetary Sciences, Birkbeck, University of London, Malet Street, London, WC1E 7HX, U.K.;

    Department of Earth and Planetary Sciences, Birkbeck, University of London, Malet Street, London, WC1E 7HX, U.K;

    Department of Mineralogy, The Natural History Museum, Cromwell Road, London, SW7 5BD, U.K.;

    Davy Faraday Research Laboratory, The Royal Institution of Great Britain, 21 Albemarle Street, London, W1S 4BS, U.K.;

    Davy Faraday Research Laboratory, The Royal Institution of Great Britain, 21 Albemarle Street, London, W1S 4BS, U.K.;

    Great Lakes Institute for Environmental Research, University of Windsor, Windsor, Ontario N9B 3P4, Canada;

    Great Lakes Institute for Environmental Research, University of Windsor, Windsor, Ontario N9B 3P4, Canada;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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