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Remediation of arsenic-contaminated groundwater by in-situ stimulating biogenic precipitation of iron sulfides

机译:通过原位刺激硫化铁的生物沉淀来修复受砷污染的地下水

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Severe health problems due to elevated arsenic (As) in groundwater have made it urgent to develop cost-effective technologies for As removal. This field experimental study tested the feasibility of in-situ As immobilization via As incorporation into newly formed biogenic Fe(II) sulfides in a typical As-affected strongly reducing aquifer at the central part of Datong Basin, China. After periodic supply of FeSO4 into the aquifer for 25 d to stimulate microbial sulfate reduction, dissolved sulfide concentrations increased during the experiment, but the supplied Fe(II) reacted quickly with sulfide to form Fe(II)sulfides existing majorly as mackinawite as well as a small amount of pyrite-like minerals in sediments, thereby restricting sulfide build-up in groundwater. After the completion of field experiment, groundwater As concentration decreased from an initial average value of 593 mu g/L to 159 mu g/L, with an overall As removal rate of 73%, and it further declined to 136 mu g/L a adding the removal rate up to 77% in 30 d after the experiment. The arsenite/As-total ratio gradually increased over time, making arsenite to be the predominant species in groundwater residual As. The good correlations between dissolved Fe(II), sulfide and As concentrations, the increased abundance of As in newly-formed Fe sulfides as well as the reactive-transport modeling results all indicate that As could have been adsorbed onto and co precipitated with Fe(II)-sulfide coatings once microbial sulfate reduction was stimulated after FeSO4 supply. Under the strongly reducing conditions, sulfide may facilitate arsenate reduction into arsenite and promote As incorporation into pyrite or arsenopyrite. Therefore, the major mechanisms for the in situ As-contaminated groundwater remediation can be As surface-adsorption on and co-precipitation with Fe(II) sulfides produced during the experimental period. (C) 2016 Published by Elsevier Ltd.
机译:由于地下水中砷(As)含量升高而造成的严重健康问题,迫切需要开发具有成本效益的砷去除技术。这项现场实验研究测试了在中国大同盆地中部典型的受As影响的强烈还原含水层中,通过将As掺入新形成的生物成因的Fe(II)硫化物中来原位固定As的可行性。在将FeSO4定期供应到含水层中25天以刺激微生物硫酸盐的还原之后,在实验过程中溶解的硫化物浓度增加,但是供应的Fe(II)与硫化物迅速反应形成主要以马基钠石形式存在的Fe(II)硫化物。沉积物中少量的类似黄铁矿的矿物,从而限制了地下水中硫化物的积累。田间试验结束后,地下水中砷的浓度从初始平均值593μg/ L降至159μg/ L,总砷去除率为73%,并进一步降至136μg/ L a。实验后30天内,去除率高达77%。砷/总砷的比例随时间逐渐增加,使砷成为地下水残留砷中的主要物质。溶解的Fe(II),硫化物和As浓度之间的良好相关性,新形成的Fe硫化物中As的丰度增加以及反应迁移模型结果均表明As可能已吸附在Fe(上)上并与Fe(下)共沉淀。 II)-硫化物涂层,一旦供给FeSO 4刺激微生物硫酸盐还原。在强还原条件下,硫化物可促进砷酸盐还原成亚砷酸盐并促进As掺入黄铁矿或毒砂中。因此,原位被砷污染的地下水修复的主要机理可能是As在实验期间对Fe(II)硫化物的表面吸附和与之共沉淀。 (C)2016由Elsevier Ltd.出版

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