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亚砷酸二甲酯与水铁矿共沉淀对Fe(II)诱导的矿物转化及亚砷酸二甲酯释放的影响

Effects of dimethylarsenate coprecipitation with ferrihydrite on Fe(II)-induced mineral transformation and the release of dimethylarsenate.

作者信息

Chen Yi, Quan Yueyang, Liu Yipu, Yuan Meng, Wang Jiaqi, Chen Chuan, Huang Chuanqin, Fang Xiaoyu, Zhang Jing, Feng Xionghan, Tan Wenfeng, Li Jiangshan, Yin Hui

机构信息

Key Laboratory of Arable Land Conservation (Middle and Lower Reaches of Yangtse River), Ministry of Agriculture and Rural Affairs, College of Resources and Environment, Huazhong Agricultural University, Wuhan, 430070, China; Hubei Key Laboratory of Soil Environment and Pollution Remediation, College of Resources and Environment, Wuhan, 430070, China.

Jiangsu Key Laboratory for Organic Waste Utilization, Jiangsu Collaborative Innovation Center for Solid Organic Waste Resource Utilization, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, 210095, China.

出版信息

Environ Pollut. 2025 Feb 15;367:125593. doi: 10.1016/j.envpol.2024.125593. Epub 2024 Dec 27.

Abstract

Organoarsenicals are toxic pollutants of global concern, and their environmental geochemical behavior might be greatly controlled by iron (Fe) (hydr)oxides through coprecipitation, which is rarely investigated. Here, the effects of the incorporation of dimethylarsenate (DMAs(V)), a typical organoarsenical, into the ferrihydrite (Fh) structure on the mineral physicochemical properties and Fe(II)-induced phase transformation of DMAs(V)-Fh coprecipitates with As/Fe molar ratios up to 0.0876 ± 0.0036 under anoxic conditions and the accompanying DMAs(V) release were investigated. The presence of DMAs(V) during Fh formation gradually decreases the mineral crystallinity. With increasing DMAs(V) content, the specific surface areas of the coprecipitates are decreased owing to particle aggregation, while the micropore sizes are negligible changed. Fourier transformed infrared (FTIR) and As K-edge X-ray absorption near-edge structure (XANES) and extended X-ray absorption fine structure (EXAFS) spectroscopy show that, part of DMAs(V) binds to Fh surfaces in the coprecipitates by forming bidentate binuclear inner-sphere complexes through As-O-Fe bonds. During the reaction of the coprecipitate with 1 mM Fe(II) for 336 h, DMAs(V) inhibits the Fh transformation to goethite. No goethite forms at pH 4; at pH 7 low content of DMAs(V) hinders the further conversion of lepidocrocite to goethite, while high content of DMAs(V) completely inhibits goethite formation. DMAs(V) in the coprecipitate is continuously released into the solution, with the released proportion being generally increased with the increase of DMAs(V) content, pH and Fe(II) addition, probably owing to the desorption of weak inner- and outer-sphere DMAs(V) complexes bound on the Fh surfaces upon the Fh aging and transformation to lepidocrocite and goethite. These results provide deep insights into the fate and mobility of organoarsenical pollutants mediated by Fe (hydr)oxides in natural environments, and help design effective and ecofriendly remediation strategies for As polluted soils and sediments.

摘要

有机砷化合物是全球关注的有毒污染物,其环境地球化学行为可能受到铁(Fe)(氢)氧化物共沉淀的极大控制,而这方面的研究很少。在此,研究了典型有机砷化合物二甲基砷酸(DMAs(V))掺入水铁矿(Fh)结构对矿物物理化学性质以及在缺氧条件下As/Fe摩尔比高达0.0876±0.0036的DMAs(V)-Fh共沉淀物中Fe(II)诱导的相变以及伴随的DMAs(V)释放的影响。Fh形成过程中DMAs(V)的存在逐渐降低矿物结晶度。随着DMAs(V)含量增加,由于颗粒聚集,共沉淀物的比表面积减小,而微孔尺寸变化可忽略不计。傅里叶变换红外光谱(FTIR)、As K边X射线吸收近边结构(XANES)和扩展X射线吸收精细结构(EXAFS)光谱表明,部分DMAs(V)通过As-O-Fe键形成双齿双核内球络合物,与共沉淀物中的Fh表面结合。在共沉淀物与1 mM Fe(II)反应336小时期间,DMAs(V)抑制Fh向针铁矿的转化。在pH 4时不形成针铁矿;在pH 7时,低含量的DMAs(V)阻碍纤铁矿进一步转化为针铁矿,而高含量的DMAs(V)完全抑制针铁矿形成。共沉淀物中的DMAs(V)不断释放到溶液中,释放比例通常随DMAs(V)含量、pH值和Fe(II)添加量的增加而增加,这可能是由于Fh老化以及向纤铁矿和针铁矿转化时,结合在Fh表面的弱内球和外球DMAs(V)络合物的解吸。这些结果为自然环境中由铁(氢)氧化物介导的有机砷污染物的归宿和迁移提供了深入见解,并有助于设计针对砷污染土壤和沉积物的有效且环保的修复策略。

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