Tracing contamination in mining areas through sulfur and oxygen isotopes in groundwater sulfates: a case study from the Apuan Alps (Italy).

IF 3.2 3区 环境科学与生态学 Q3 ENGINEERING, ENVIRONMENTAL
Stefano Natali, Linda Franceschi, Roberto Giannecchini, Massimo D'Orazio, Antonio Delgado-Huertas, Giovanni Zanchetta, Marco Doveri
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引用次数: 0

Abstract

Groundwater contamination from legacy mining activities is a significant environmental concern, particularly in karst regions with vulnerable aquifers. This study investigates the isotopic composition of groundwater sulfates in a former mining area (Apuan Alps, Italy) to identify contamination sources and assess aquifer vulnerability. Sulfur and oxygen isotopes (δ34S and δ18O) of dissolved sulfates, combined with hydrochemical data, distinguish sulfide-derived sulfate, originating from acid mine drainage and sulfide oxidation, from sulfate released through evaporitic dissolution. The results show that some groundwater springs near mining sites are influenced by the oxidation of sulfide minerals and the dissolution of secondary Fe-Al-K sulfates, as evidenced by depleted δ34S and δ18O values and the presence of trace metals, including thallium. In contrast, other springs exhibit isotopically enriched δ34S and δ18O signatures, characteristic of the dissolution of Triassic evaporites, indicating deeper aquifers protected from mining-related contamination. Seasonal isotopic variations reveal the mixing of shallow and deep groundwater flow components, with dilution effects observed during recharge periods. These findings underscore the effectiveness of isotopic tools in tracing sulfate origin and highlight the risks of contamination in shallow karst systems.

通过地下水硫酸盐中的硫和氧同位素追踪矿区污染:来自Apuan Alps(意大利)的案例研究。
传统采矿活动造成的地下水污染是一个重大的环境问题,特别是在含水层脆弱的喀斯特地区。本研究调查了前矿区(意大利Apuan Alps)地下水硫酸盐的同位素组成,以确定污染源并评估含水层的脆弱性。溶解硫酸盐的硫氧同位素(δ34S和δ18O)结合水化学资料,区分了源自酸性矿井水和硫化物氧化的硫化物衍生硫酸盐与蒸发溶解释放的硫酸盐。结果表明:矿区附近部分地下水泉水受硫化矿物氧化和次生Fe-Al-K硫酸盐溶解的影响,δ34S和δ18O值枯竭,并存在铊等微量金属。相反,其他泉水表现出同位素富集的δ34S和δ18O特征,这是三叠纪蒸发岩溶解的特征,表明较深的含水层免受采矿相关污染的保护。季节性同位素变化揭示了浅层和深层地下水流动成分的混合,在补给期观察到稀释效应。这些发现强调了同位素工具在追踪硫酸盐来源方面的有效性,并强调了浅层岩溶系统污染的风险。
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来源期刊
Environmental Geochemistry and Health
Environmental Geochemistry and Health 环境科学-工程:环境
CiteScore
8.00
自引率
4.80%
发文量
279
审稿时长
4.2 months
期刊介绍: Environmental Geochemistry and Health publishes original research papers and review papers across the broad field of environmental geochemistry. Environmental geochemistry and health establishes and explains links between the natural or disturbed chemical composition of the earth’s surface and the health of plants, animals and people. Beneficial elements regulate or promote enzymatic and hormonal activity whereas other elements may be toxic. Bedrock geochemistry controls the composition of soil and hence that of water and vegetation. Environmental issues, such as pollution, arising from the extraction and use of mineral resources, are discussed. The effects of contaminants introduced into the earth’s geochemical systems are examined. Geochemical surveys of soil, water and plants show how major and trace elements are distributed geographically. Associated epidemiological studies reveal the possibility of causal links between the natural or disturbed geochemical environment and disease. Experimental research illuminates the nature or consequences of natural or disturbed geochemical processes. The journal particularly welcomes novel research linking environmental geochemistry and health issues on such topics as: heavy metals (including mercury), persistent organic pollutants (POPs), and mixed chemicals emitted through human activities, such as uncontrolled recycling of electronic-waste; waste recycling; surface-atmospheric interaction processes (natural and anthropogenic emissions, vertical transport, deposition, and physical-chemical interaction) of gases and aerosols; phytoremediation/restoration of contaminated sites; food contamination and safety; environmental effects of medicines; effects and toxicity of mixed pollutants; speciation of heavy metals/metalloids; effects of mining; disturbed geochemistry from human behavior, natural or man-made hazards; particle and nanoparticle toxicology; risk and the vulnerability of populations, etc.
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