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Arsenic remediation through magnetite based in situ immobilization

机译:基于原位固定化的磁铁矿砷补救

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The remediation of arsenic-contaminated aquifers is a formidable challenge to achieve in part because geochemical conditions often do not favor the stabilization of arsenic within the solid phase.A promising remedial approach involves stimulating iron mineral transformations that immobilize arsenic through sorption or precipitation.Despite intense research,the current immobilization methods are still often ineffective,in part because many iron minerals are susceptible to redox gradients common in subsurface environments.We have been conducting a series of studies to illustrate the potential of nanoparticulate magnetite (Fe3O4) to sequester arsenic.Magnetite is stable under most redox conditions in aquifers,and able to co-precipitate and adsorb arsenic.Here,we present results from microcosm and column experiments using sediments and groundwater from U.S.Superfund sites,and from reactive transport modelling.All these results demonstrate that in situ formation of nanoparticulate magnetite can be achieved by the combination of nitrate and ferrous iron,and that it shold be feasible to produce an in situ reactive filter by such nitrate-iron(II) co-injection and immobilize arsenic in contaminated aquifers.
机译:砷污染的含水层的修复是一个艰巨的挑战,因为地球化学条件往往不赞成在固相中砷的稳定性。有前途的补救方法涉及刺激通过吸附或降水固定砷的铁矿物转化。分别激烈研究,目前的固定方法仍然是无效的,部分原因是许多铁矿物质易于在地下环境中常见的氧化还原梯度。我们一直在进行一系列研究以说明纳米颗粒磁铁矿(Fe3O4)的潜力来螯合砷。在含水层中大多数氧化还原条件下稳定,并且能够共析出和吸附砷。:我们将微观和柱实验从Ussuperfund遗址的沉积物和地下水进行了结果,并从反应性运输型效果中提出。所有这些结果表明了纳米颗粒磁铁矿的原位形成可以通过硝酸铁和铁的组合来实现,并且它可以通过这种硝酸盐 - 铁(II)共注射并在受污染的含水层中固定砷来生产原位反应性过滤器。

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