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In-situ formation of Fe(II)-sulfide coatings on aquifer sediments to remediate high arsenic groundwater

机译:原位形成Fe(II) - 含水层沉积物涂料,以修复高砷地下水

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A field test was conducted to evaluate a novel technology of in-situ remediation of high arsenic aquifer based on microbially-stimulated Fe(II)-sulfide coating formation under reducing conditions. After multiple supply of FeSO_4 into the aquifer for 25 days, groundwater arsenic decreased from an initial concentration of 593 μg/L to 159 μg/L, and further lowered to 136 μg/L 30 days later after field implementation. Microbial sulfate reduction produced high aqueous sulfide that reacted with Fe(II) to firstly form mackinawite on sediment surfaces. Aqueous arsenic was sequestered via surface adsorption and co-precipitation with mackinawite that could be transformed to arsenic-bearing pyrite. Furthermore, As(V) can be reduced by sulfide into As(III) to facilitate its incorporation into the newly-formed Fe(II)- sulfide phases in the environment of enhanced reducing condition.
机译:进行了基于微生物刺激的Fe(II) - 在还原条件下的微生物刺激的Fe(II) - 硫化物涂层的原位修复的新技术试验。在将FeSO_4多次供应到含水层中25天后,地下水砷从初始浓度降低593μg/ L至159μg/ L,并在现场实施后30天后进一步降至136μg/ L.微生物硫酸盐还原产生高硫化物水溶液,其与Fe(II)反应首先在沉积物表面上形成MackInawite。通过表面吸附和含有MackInawite的共沉淀来沉淀砷水溶液,其可以转化为致砷黄铁矿。此外,如(v)可以通过硫化物作为(III)来减少,以促进其在增强的还原条件的环境中掺入新形成的Fe(II) - 硫化物相中。

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