Hydrogeochemical and health implications of rare earth elements in groundwater: A review

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Huaming Guo , Haiyan Liu , Olivier Pourret , Myongchol Ri , Zhen Wang
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Abstract

Rare earth elements (REEs) are increasingly accumulated in groundwater due to anthropogenic activities, but their fate, hydrogeochemical behavior, and health impacts remain poorly understood and regulated. We have systematically reviewed the scientific literature over the last decades concerning sources, geochemical processes, potential tracer, and health impacts of REEs in groundwaters. REEs in groundwaters are mainly sourced from bedrock and occasionally from anthropogenic activities. Geochemical processes, including redox processes, complexation, adsorption, and desorption, modify REE signatures in groundwater. Redox conditions can change the redox state of Ce and result in anomalies, which can reflect redox processes in groundwater systems. We systematically concluded that REE concentrations and patterns can be used to delineate sources and geochemical processes of geogenic redox-sensitive elements in groundwater (such as arsenic and uranium). Anthropogenic REEs from wastewater, fertilizer, mining, and solid waste can be introduced into groundwater systems, which disturbs the natural REE signatures. We disentangled that delineating groundwater contamination and tracing related geochemical processes can be beneficial from differentiating geogenic REE signatures from anthropogenic REE disturbance. Long-term consumption of low-dose REE-bearing drinking water is suggested to cause diverse significant damage to human health. Novel investigations are required to perform on pathways of REE intake, potential mitigation measures, and drinking water guidelines for REE concentrations to minimize their health impacts. Future studies are needed to better understand environmental behavior and epidemiological impacts of anthropogenic REEs in groundwaters.

Abstract Image

地下水中稀土元素的水文地球化学和健康意义:综述
由于人类活动,稀土元素(ree)在地下水中的积累越来越多,但它们的命运、水文地球化学行为以及对健康的影响仍然知之甚少。我们系统地回顾了过去几十年来有关地下水中稀土元素来源、地球化学过程、潜在示踪剂和健康影响的科学文献。地下水中的稀土元素主要来源于基岩,偶尔也来源于人为活动。地球化学过程,包括氧化还原过程、络合作用、吸附和解吸作用,改变了地下水中的稀土元素特征。氧化还原条件可以改变Ce的氧化还原状态并产生异常,这些异常可以反映地下水系统中的氧化还原过程。系统地总结了稀土元素浓度和模式可以用来描述地下水中地质氧化还原敏感元素(如砷和铀)的来源和地球化学过程。来自废水、肥料、采矿和固体废物的人为稀土元素可以引入地下水系统,从而干扰自然稀土元素特征。研究表明,区分地球成因稀土元素特征和人为稀土元素干扰有助于圈定地下水污染和示踪相关地球化学过程。长期饮用低剂量含稀土的饮用水对人体健康造成多种严重损害。需要对稀土元素摄入途径、潜在的缓解措施和饮用水稀土元素浓度指南进行新的调查,以尽量减少其对健康的影响。未来的研究需要更好地了解地下水中人为稀土元素的环境行为和流行病学影响。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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