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水动力条件下草酸存在时铁氧化物中砷的迁移。

Arsenic mobilization from iron oxides in the presence of oxalic acid under hydrodynamic conditions.

机构信息

Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY 10964, United States; School of Earth Sciences, University of Western Australia, 35 Stirling Highway, Perth, WA 6009, Australia.

Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY 10964, United States.

出版信息

Chemosphere. 2018 Dec;212:219-227. doi: 10.1016/j.chemosphere.2018.08.058. Epub 2018 Aug 14.

Abstract

Oxalic acid potentially enhances pump-and-treat for groundwater As remediation by accelerating mobilization. This study examines how oxalic acid mobilizes As from Fe(III)-oxide coated sand under hydrodynamic conditions. Four columns were packed with metal-substituted ferrihydrite or goethite to 1% Fe, presorbed to 50% As surface coverage, and reacted with pH = 2.2 artificial groundwater amended with 10 mM oxalic acid at 1 m day. Arsenic elution was affected by both As and Fe speciation. Although the As(V) columns experienced faster substrate dissolution, As(V) elution was delayed by re-adsorption, whereas As(III) elution was rapid due to pH decrease that prevented re-adsorption. Cr-ferrihydrite and Ni-goethite dissolved both effectively initially but then diverged. The Cr-ferrihydrite columns experienced continuous stoichiometric Fe and Cr release, and As release could be sustained. The Ni-goethite columns initially experienced nonstoichiometric Fe and Ni release, and As release was extensive. Such release, however, was not sustained. We hypothesized that Ni-goethite contained sites with distinct reactivity, and oxalic acid targeted readily-dissolved, sorption-dense sites. Our data indicate that oxalic acid-enhanced pump-and-treat methods would be easier to apply to aquifers dominated by As(III), requiring less amendment to be injected; such oxalic acid-enhanced methods remove reactive sediment Fe and As, potentially preventing future groundwater contamination.

摘要

草酸可能通过加速迁移来增强地下水砷修复的抽吸处理。本研究考察了草酸在水动力条件下如何将砷从氧化铁涂层砂中动员起来。四个柱子填充了金属取代的水铁矿或针铁矿,达到 1%的铁含量,预吸附到 50%的砷表面覆盖度,并与 pH=2.2 的人工地下水反应,该地下水用 10mM 草酸和 1m 天的速率进行了修正。砷洗脱受到砷和铁形态的影响。虽然 As(V)柱经历了更快的基质溶解,但由于 pH 下降阻止了再吸附,As(V)的洗脱被延迟,而 As(III)的洗脱则由于 pH 下降而迅速发生。Cr-水铁矿和 Ni-针铁矿最初都有效地溶解,但随后出现分歧。Cr-水铁矿柱经历了连续的化学计量的 Fe 和 Cr 释放,因此可以维持砷的释放。Ni-针铁矿柱最初经历了非化学计量的 Fe 和 Ni 释放,并且砷的释放很广泛。然而,这种释放无法持续。我们假设 Ni-针铁矿含有具有不同反应性的位点,而草酸则针对易于溶解、吸附密集的位点。我们的数据表明,草酸增强的抽吸处理方法将更容易应用于主要由 As(III)控制的含水层,需要注入的修正剂更少;这种草酸增强的方法去除了反应性的沉积物 Fe 和 As,可能防止未来的地下水污染。

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