吉林西部地下水氟、砷区域分布控制过程评价

IF 2.8 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES
Mingqian Li, He Wang, Hongbiao Gu, Jiang Sun, Baoming Chi
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引用次数: 0

摘要

地下水是一个地区的重要资源,地下水中F和As的高含量会严重影响区域的生态稳定。吉林西部平原地下水位128米,氟和砷含量超过世界卫生组织(WHO)安全饮用标准。为了评价控制F和As在含水层区域分布的主要过程,选取了225口不同深度的井进行了平原地下水采样分析。地下水中F和As的浓度范围分别为0.16 ~ 7.99µg/L和1 ~ 310µg/L。约33%和20%的样品分别超过了世界卫生组织的F (1.5 mg/L)和As(10µg/L)限值。F与As无显著相关。在平原中部,霍林河流域上游地下水As浓度较高,下游地下水F浓度较高。F和As的来源和富集主要来自广泛的自然过程,几乎没有人为影响的迹象。F和As的区域分布受以霍林河上游为主的水文地质控制和以霍林河中下游为主的水文地球化学控制两个过程的控制。控制研究区F和As分布和运移的主要水文地球化学过程是碳酸盐岩的溶蚀(HCO3−可能作为吸附竞争对手)、pH的升高和阳离子交换(Na+的释放和Ca2+的吸附)。蒸散发作用仅影响局部浅层地下水F和As浓度的富集过程。人为开采地下水是中深层地下水中氟和砷运移的主要原因。高浓度含氟砷地下水与未污染地下水的混合是未来研究的一个潜在问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of processes controlling the regional distribution of fluoride and arsenic in groundwater of the Western Jilin Province, Northeast China

Groundwater is a critical resource for a locality, and high F and As contents in groundwater can substantially impact regional ecological stability. The Western Plain of Jilin has groundwater > 128 m, and F and As levels exceed the World Health Organization’s (WHO) safe drinking levels. To assess the primary processes controlling the regional distribution of F and As in the aquifer, 225 wells at varying depths were selected and analyzed for groundwater sampling in the plain. Concentration ranges of F and As in the groundwater were 0.16–7.99 and 1–310 µg/L, respectively. Approximately 33% and 20% of the samples exceeded the WHO limit for F (1.5 mg/L) and As (10 µg/L), respectively. F and As were not significantly correlated. In the central part of the plain, the groundwater upstream of the Huolin River Basin had higher As concentrations, whereas the groundwater downstream had higher F concentrations. The sources and enrichment of F and As predominantly resulted from widespread natural processes with little signs of anthropogenic influence. Regional of F and As distributions are controlled by two processes: hydrogeological controls primarily in the upstream region of the Huolin River and hydrogeochemical controls mainly occurring in the middle and downstream areas of the river. The primary hydrogeochemical processes controlling F and As distribution and migration in the study area are the dissolution of carbonate rock (where HCO3 may act as a sorption competitor), an increase in pH, and cation exchange (release of Na+ and adsorption of Ca2+). Evapotranspiration only influences the enrichment process of F and As concentrations in localized shallow groundwater. Human–induced groundwater extraction is the primary cause of F and As migration in medium and deep groundwater. The mixing of highly concentrated F- and As-containing groundwater with uncontaminated groundwater presents a potential problem for future research.

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来源期刊
Environmental Earth Sciences
Environmental Earth Sciences 环境科学-地球科学综合
CiteScore
5.10
自引率
3.60%
发文量
494
审稿时长
8.3 months
期刊介绍: Environmental Earth Sciences is an international multidisciplinary journal concerned with all aspects of interaction between humans, natural resources, ecosystems, special climates or unique geographic zones, and the earth: Water and soil contamination caused by waste management and disposal practices Environmental problems associated with transportation by land, air, or water Geological processes that may impact biosystems or humans Man-made or naturally occurring geological or hydrological hazards Environmental problems associated with the recovery of materials from the earth Environmental problems caused by extraction of minerals, coal, and ores, as well as oil and gas, water and alternative energy sources Environmental impacts of exploration and recultivation – Environmental impacts of hazardous materials Management of environmental data and information in data banks and information systems Dissemination of knowledge on techniques, methods, approaches and experiences to improve and remediate the environment In pursuit of these topics, the geoscientific disciplines are invited to contribute their knowledge and experience. Major disciplines include: hydrogeology, hydrochemistry, geochemistry, geophysics, engineering geology, remediation science, natural resources management, environmental climatology and biota, environmental geography, soil science and geomicrobiology.
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