中国地下水中砷的来源、迁移、分布、毒理学效应及修复技术

IF 4.6 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
China Geology Pub Date : 2023-07-01 DOI:10.31035/cg2022086
Zhen Wang , Hua-ming Guo , Hai-yan Liu , Wei-min Zhang
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引用次数: 1

摘要

地下水砷含量高,严重威胁人类生命健康。长期饮用高砷地下水会导致皮肤癌症、癌症、癌症等多种病理变化。高砷地下水已成为我国乃至国际上最严重的环境地质问题之一。本文旨在通过大量文献调查,系统总结我国天然地下水中砷的来源、迁移、分布、毒性作用和处理技术。我国高砷地下水主要分布在干旱半干旱环境下的内陆盆地和湿润环境下的河流三角洲冲湖含水层,属于中性至弱碱性强还原性环境。地下水中As含量变化较大,以As(III)为主。我国高As地下水形成的主要机制是在有机质和原生微生物、碱性环境、强烈蒸发浓缩、长期水岩相互作用、地下水流速缓慢的作用下,铁、锰氧化物的溶解减少,促进了As在地下水中的不断迁移和富集。不同形式的砷的毒性存在明显差异。砷(III)的毒性远大于砷(V),后者被认为比砷酸甲酯(MMA)和砷酸二甲酯(DMA)毒性更大。进入体内的无机砷通过甲基化(解毒)和还原(活化)的组合进行代谢,并由一系列甲基转移酶和还原酶催化。目前,高砷地下水的修复方法主要有离子交换技术、膜过滤技术、生物处理技术、纳米复合吸附技术、电化学技术等。上述修复方法仍有一定的局限性,迫切需要开发具有更强除砷性能和可持续性的处理材料和技术手段。在未来各国科学家和政府的共同努力下,这一世界性的饮用水砷中毒问题将尽快得到解决。本文系统总结和讨论了天然高砷地下水的研究热点,可为我国乃至世界高砷地下水相关研究提供参考。©2023中国地质编辑部。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Source, migration, distribution, toxicological effects and remediation technologies of arsenic in groundwater in China

Groundwater with high arsenic (As) content seriously threatens human life and health. Drinking high-As groundwater for a long time will lead to various pathological changes such as skin cancer, liver cancer, and kidney cancer. High-As groundwater has become one of the most serious environmental geological problems in China and even internationally. This paper aims to systematically summarize the sources, migration, distribution, toxicological effects, and treatment techniques of As in natural groundwater in China based on a large number of literature surveys. High-As groundwater in China is mainly distributed in the inland basins in arid and semi-arid environments and the alluvial and lacustrine aquifers in river deltas in humid environments, which are in neutral to weakly alkaline and strongly reducing environments. The content of As in groundwater varies widely, and As(III) is the main form. The main mechanism of the formation of high-As groundwater in China is the reduced dissolution of Fe and Mn oxides under the action of organic matter and primary microorganisms, alkaline environment, intense evaporation and concentration, long-term water-rock interaction, and slow groundwater velocity, which promote the continuous migration and enrichment of As in groundwater. There are obvious differences in the toxicity of different forms of As. The toxic of As(III) is far more than As(V), which is considered to be more toxic than methyl arsenate (MMA) and dimethyl arsenate (DMA). Inorganic As entering the body is metabolized through a combination of methylation (detoxification) and reduction (activation) and catalyzed by a series of methyltransferases and reductases. At present, remediation methods for high-As groundwater mainly include ion exchange technology, membrane filtration technology, biological treatment technology, nanocomposite adsorption technology, electrochemical technology, and so on. All the above remediation methods still have certain limitations, and it is urgent to develop treatment materials and technical means with stronger As removal performance and sustainability. With the joint efforts of scientists and governments of various countries in the future, this worldwide problem of drinking-water As poisoning will be solved as soon as possible. This paper systematically summarizes and discusses the hot research results of natural high-As groundwater, which could provide a reference for the related research of high-As groundwater in China and even the world.

©2023 China Geology Editorial Office.

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来源期刊
China Geology
China Geology GEOLOGY-
CiteScore
7.80
自引率
11.10%
发文量
275
审稿时长
16 weeks
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