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在洪泛区含水层的氧化还原过渡带中,磷酸盐固定动力学及其与砷吸附的相互作用:来自越南红河三角洲的见解。

Phosphate immobilisation dynamics and interaction with arsenic sorption at redox transition zones in floodplain aquifers: Insights from the Red River Delta, Vietnam.

机构信息

Geoecology, Eberhard Karls University Tübingen, 72070 Tübingen, Germany.

Geoecology, Eberhard Karls University Tübingen, 72070 Tübingen, Germany.

出版信息

J Hazard Mater. 2021 Jun 5;411:125128. doi: 10.1016/j.jhazmat.2021.125128. Epub 2021 Jan 14.

Abstract

Although phosphate (PO) may play a decisive role in enriching toxic arsenic (As) in the groundwater of many Asian deltas, knowledge gaps exist regarding its interactions with As. This study investigates the simultaneous immobilisation of PO and As in aquifer sediments at a redox transition zone in the Red River Delta of Vietnam. The majority of PO and As was found to be structurally bound in layers of Fe(III)-(oxyhydr)oxide precipitates, indicating that their formation represents a dominant immobilisation mechanism. This immobilisation was also closely linked to sorption. In the surface sorbed sediment pools, the molar ratios of total P to As were one order of magnitude higher than found in groundwater, reflecting a preferential sorption of PO over As. However, this competitive sorption was largely dependent on the presence of Fe(III)-(oxyhydr)oxides. Ongoing contact of the aquifer sediments with iron-reducing groundwater resulted in the reductive dissolution of weakly crystalline Fe(III)-(oxyhydr)oxides, which was accompanied by decreased competition for sorption sites between PO and As. Our results emphasise that, to be successful in the medium and long term, remediation approaches and management strategies need to consider competitive sorption between PO and As and dynamics of the biogeochemical Fe-cycle.

摘要

尽管磷酸盐 (PO) 可能在许多亚洲三角洲地区富含地下水有毒砷 (As) 方面起着决定性作用,但目前仍存在其与 As 相互作用的知识空白。本研究调查了越南红河三角洲氧化还原过渡带含水层沉积物中 PO 和 As 的同时固定。研究发现,大部分 PO 和 As 都被固定在铁 (III)-(氧氢)氧化物沉淀物的层中,这表明它们的形成代表了一种主要的固定化机制。这种固定化也与吸附密切相关。在表层吸附沉积物中,总磷与砷的摩尔比比地下水高一个数量级,反映了 PO 对 As 的优先吸附。然而,这种竞争吸附在很大程度上取决于铁 (III)-(氧氢)氧化物的存在。含水层沉积物与还原地下水的持续接触导致弱晶型铁 (III)-(氧氢)氧化物的还原溶解,这伴随着 PO 和 As 之间吸附位竞争的减少。我们的研究结果强调,为了在中长期取得成功,修复方法和管理策略需要考虑 PO 和 As 之间的竞争吸附以及生物地球化学 Fe 循环的动态。

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