首页> 外文期刊>Environmental Science & Technology >Impacts of Shewanella putrefaciens Strain CN-32 Cells and Extracellular Polymeric Substances on the Sorption of As(V) and As(lll) on Fe(lll)-(Hydr)oxides
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Impacts of Shewanella putrefaciens Strain CN-32 Cells and Extracellular Polymeric Substances on the Sorption of As(V) and As(lll) on Fe(lll)-(Hydr)oxides

机译:腐灵假单胞菌菌株CN-32细胞和细胞外聚合物对As(V)和As(III)吸附Fe(III)-(Hydr)氧化物的影响

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摘要

We investigated the effects of Shewanella putrefaciens cells and extracellular polymeric substances on the sorption of As(lll) and As(V) to goethite, ferrihydrite, and hematite at pH 7.0. Adsorption of As(lll) and As(V) at solution concentrations between 0.001 and 20 fiM decreased by 10 to 45% in the presence of 0.3 g L l EPS, with As(lll) being affected more strongly than As(V). Also, inactivated Shewanella cells induced desorption of As(V) from the Fe(lll)-(hydr)oxide mineral surfaces. ATR-FTIR studies of ternary As(V)-Shewanella-hematite systems indicated As(V) desorption concurrent with attachment of bacterial cells at the hematite surface, and showed evidence of inner-sphere coordination of bacterial phosphate and carboxylate groups at hematite surface sites. Competition between As(V) and bacterial phosphate and carboxylate groups for Fe(lll)-(oxyhydr)oxide surface sites is proposed as an important factor leading to increased solubility of As(V). The results from this study have implications for the solubility of As(V) in the soil rhizosphere and in geochemical systems undergoing microbially mediated reduction and indicate that the presence of sorbed oxyanions may affect Fe-reduction and biofilm development at mineral surfaces.
机译:我们研究了腐乳酸希瓦氏菌细胞和细胞外聚合物在pH 7.0时对As(III)和As(V)吸附于针铁矿,水铁矿和赤铁矿的影响。在0.3 g L l EPS的存在下,溶液浓度在0.001和20 fiM之间的As(III)和As(V)的吸附降低了10%至45%,其中As(III)的影响比As(V)更大。同样,灭活的希瓦氏菌细胞诱导As(V)从Fe(III)-(hydr)oxide矿物表面解吸。对三元As(V)-希瓦氏菌-赤铁矿体系的ATR-FTIR研究表明,As(V)的解吸与赤铁矿表面细菌细胞的附着同时发生,并显示了赤铁矿表面部位细菌磷酸盐和羧酸盐基团在球内的配位证据。提出As(V)与细菌磷酸根和羧酸根之间竞争Fe(III)-(羟基)氧化物表面位点的竞争是导致As(V)溶解度增加的重要因素。这项研究的结果对砷(V)在土壤根际和经历微生物介导的还原的地球化学系统中的溶解度有影响,并表明吸附的氧阴离子的存在可能会影响矿物表面的铁还原和生物膜的发育。

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  • 来源
    《Environmental Science & Technology》 |2011年第7期|p.2804-2810|共7页
  • 作者单位

    Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, CHN, CH-8092 Zurich, Switzerland;

    Department of Earth & Environmental Sciences, Rutgers University, Newark, New Jersey 07102, United States;

    Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, CHN, CH-8092 Zurich, Switzerland;

    Eawag, Swiss Federal Institute of Aquatic Science and Technology, CH-8600 Diibendorf, Switzerland;

    Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, CHN, CH-8092 Zurich, Switzerland;

  • 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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  • 正文语种 eng
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  • 入库时间 2022-08-17 14:03:34

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