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土壤和地下水中的镉:综述

Cadmium in soils and groundwater: A review.

作者信息

Kubier Andreas, Wilkin Richard T, Pichler Thomas

机构信息

University of Bremen, Department of Geosciences, D-28359, Bremen, Germany.

U.S. Environmental Protection Agency, Office of Research and Development, National Risk Management Research Laboratory, Ada, OK, 74820, USA.

出版信息

Appl Geochem. 2019 Sep 1;108:1-16. doi: 10.1016/j.apgeochem.2019.104388.

Abstract

Cadmium (Cd) is a non-essential trace element that is widely distributed in the environment. Both geogenic and anthropogenic sources can elevate Cd concentrations in soils and groundwater, which are important for maintaining healthy supplies of food and safe drinking water. Elevated Cd doses are carcinogenic to humans. The WHO Guidelines for Drinking-Water Quality recommend a guideline value for Cd of 3 μg/L. Important anthropogenic Cd sources include mining, atmospheric deposition of combustion emissions, and the use of Cd-containing fertilizers. We document several cases of Cd pollution in soil and groundwater based on worldwide accounts. Besides anthropogenic Cd sources, Cd is also incorporated into sulfides, carbonates, and phosphorites resulting in elevated Cd concentrations in associated rock types. The crustal median Cd content is 0.2 mg/kg. In soils, Cd occurs at concentrations of 0.01 to 1 mg/kg with a worldwide mean of 0.36 mg/kg. Weathering can lead to Cd concentrations up to 5 μg/L in soil water and up to 1 μg/L in groundwater. In aqueous solutions, Cd generally occurs as the divalent Cd and it is mobilized mainly in oxic, acidic conditions. Cadmium sorption is enhanced by the presence of high amounts of hydrous oxides, clay minerals, and organic matter, and its mobility is further influenced by pH, the redox state, and ionic strength of the solution. However, Cd can remain in solution as water-soluble complexes with anions, such as CdCl and Cd(SO) , and dissolved organic matter while sorption and precipitation decrease the aqueous concentration of most other heavy metals. As a consequence, Cd is one of the most mobile heavy metals in the environment. The elevated mobilization potential, e.g., through competition and ligand induced desorption, is the reason for faster Cd release from soil into groundwater than other heavy metals. The goal of this study was to present a broad overview of the origin and concentration of Cd in groundwater, and its reaction pathways in aquatic environments. To gain an overview of the hydrochemical behavior of Cd, cases of Cd pollution in soil and groundwater, studies investigating Cd release, and information about the legal framework were compiled.

摘要

镉(Cd)是一种非必需的微量元素,广泛分布于环境中。地质源和人为源均可提高土壤和地下水中的镉浓度,这对于维持健康的食物供应和安全的饮用水至关重要。高剂量的镉对人类具有致癌性。世界卫生组织《饮用水水质准则》建议镉的准则值为3μg/L。重要的人为镉源包括采矿、燃烧排放的大气沉降以及含镉肥料的使用。我们基于全球记录文件了几起土壤和地下水镉污染的案例。除了人为镉源外,镉还会结合到硫化物、碳酸盐和磷矿中,导致相关岩石类型中的镉浓度升高。地壳中镉的中位数含量为0.2mg/kg。在土壤中,镉的浓度为0.01至1mg/kg,全球平均值为0.36mg/kg。风化可导致土壤水中镉浓度高达5μg/L,地下水中高达1μg/L。在水溶液中,镉通常以二价镉的形式存在,主要在有氧、酸性条件下被活化。大量水合氧化物、粘土矿物和有机物的存在会增强镉的吸附作用,溶液的pH值、氧化还原状态和离子强度会进一步影响其迁移性。然而,镉可以与阴离子(如CdCl和Cd(SO))以及溶解有机物形成水溶性络合物而留在溶液中,而吸附和沉淀会降低大多数其他重金属的水溶液浓度。因此,镉是环境中迁移性最强的重金属之一。例如,通过竞争和配体诱导解吸提高的活化潜力,是镉比其他重金属更快地从土壤释放到地下水中的原因。本研究的目的是全面概述地下水中镉的来源和浓度及其在水生环境中的反应途径。为了了解镉的水化学行为,汇编了土壤和地下水镉污染案例、研究镉释放的研究以及法律框架信息。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/616b/7147761/5bcdef0c387c/nihms-1570863-f0001.jpg

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