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Cadmium in soils and groundwater: A review

机译:土壤和地下水中的镉:综述

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摘要

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 mu g/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 mu g/L in soil water and up to 1 mu g/L in groundwater. In aqueous solutions, Cd generally occurs as the divalent Cd2+ 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(SO4)(2)(2-), 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.
机译:镉(CD)是一种非必要的痕量元件,广泛分布在环境中。造工和人为源均可提高土壤和地下水中的CD浓度,这对于维持健康的食品和安全饮用水是重要的。升高的Cd剂量是人类的致癌物质。饮用水质指令推荐了3 mu g / l的CD的指导性值。重要的人体化CD源包括采矿,大气沉积燃烧排放,以及使用含CD的肥料。我们根据全球账户记录土壤和地下水中的几例。除了人为Cd来源外,CD还掺入硫化物,碳酸盐和磷酸盐中,得到相关岩石类型中的CD浓度升高。地壳中值CD含量为0.2mg / kg。在土壤中,CD以0.01至1mg / kg的浓度发生,全球平均值为0.36mg / kg。风化可以导致在土壤水中高达5μg/ l的Cd浓度,在地下水中高达1μg/ l。在水溶液中,CD通常作为二价CD2 +发生,并且它主要在氧酸性条件下动员。通过存在大量的含水氧化物,粘土矿物和有机物质,增强了镉吸附,其迁移率进一步受到溶液的氧化还原状态和离子强度的影响。然而,CD可以保留在溶液中,作为水溶性复合物,其阴离子如CdCl +和Cd(SO 4)(2)(2)(2)(2)(2)(2-),而吸附和沉淀降低了大多数其他重金属的水性浓度。因此,CD是环境中最移动的重金属之一。升高的动员电位,例如,通过竞争和配体诱导的解吸,是从土壤中加快CD释放到地下水的原因而不是其他重金属。本研究的目的是概述地下水中CD的起源和浓度,以及水产环境中的反应途径。为了概述CD的水化学行为,土壤和地下水的CD污染病例,研究调查CD释放以及法律框架的信息。

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