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中国东部黄土高原集约化工业地区地下水水化学、来源识别和污染评价。

Groundwater hydrochemistry, source identification and pollution assessment in intensive industrial areas, eastern Chinese loess plateau.

机构信息

State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061, China; CAS Center for Excellence in Quaternary Science and Global Change, Xi'an, 710061, China.

Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China.

出版信息

Environ Pollut. 2021 Jun 1;278:116930. doi: 10.1016/j.envpol.2021.116930. Epub 2021 Mar 10.

Abstract

Groundwater is essential for regional ecological-economic system and is an important resource of drinking water, especially in the Chinese Loess Plateau (CLP), where is a typical water-limited ecosystem. Groundwater quality deterioration will affect water security and exacerbate the water shortages. Groundwater hydrochemistry, pollution source apportionment, quality and health risks were evaluated based on analysis of major ions and selected trace elements in seasonal samples of the Fen River Basin (FRB) in the eastern CLP. Groundwaters in the FRB were mainly HCO-Ca-Na water type with low dissolved solutes in upstream samples, high values in midstream samples and medium values in downstream samples. Solutes in upstream samples were mainly derived from carbonate weathering, while those in midstream and downstream samples came from silicate weathering, evaporites dissolution and anthropogenic sources. Self-organizing map (SOM) showed the hydrochemistry remained unchanged from dry to wet season for most sampling points. The seasonal variations of Ag, Cd, Ni, Pb, and Tl were significant due to anthropogenic input. High NO in upstream and downstream samples resulted primarily from sewage discharge, and high SO in midstream and downstream samples was from gypsum- and coal-related industries. In addition, anthropogenic input related to coal industries significantly aggravates pollution of As, Ni, Ag, Fe, and Mn. Influenced by evaporites and anthropogenic input, midstream samples had high salinity, total hardness and water quality indices (WQIs) and were unsuitable for irrigation or drinking purposes. Seasonal variation of WQI in the FRB was unsignificant except Jiaokou River sub-basin, where groundwater quality was worse in the wet season than the dry season due to coal mining. Great attention should be paid to the high non-carcinogenic risks of exposure to F, V, Mn, and Cr via dermal absorption, particularly for children. Overall, groundwater quality in the FRB was best in upstream, medium in midstream and worst in midstream based on different index. Groundwater quality is deteriorated by anthropogenic input and the sewage discharge in the FRB should be strictly controlled. Our report provides a reference for groundwater pollution evaluation and source identification in similar areas.

摘要

地下水是区域生态经济系统的基础,也是饮用水的重要资源,特别是在中国黄土高原(CLP),这里是典型的水资源受限生态系统。地下水水质恶化将影响水安全,并加剧水资源短缺。本研究基于对 CLP 东部汾河流域(FRB)季节性水样中主要离子和选定微量元素的分析,评估了地下水水化学、污染源分配、水质和健康风险。结果表明,FRB 地下水主要为 HCO-Ca-Na 水型,上游水样中溶解性溶质含量较低,中游水样中溶解性溶质含量较高,下游水样中溶解性溶质含量中等。上游水样中的溶质主要来源于碳酸盐风化,而中游和下游水样中的溶质则来自硅酸盐风化、蒸发盐溶解和人为源。自组织映射(SOM)表明,大多数采样点的水化学性质在干、湿季保持不变。由于人为输入,Ag、Cd、Ni、Pb 和 Tl 的季节性变化显著。上游和下游水样中高浓度的 NO 主要来自污水排放,中游和下游水样中高浓度的 SO 主要来自石膏和煤炭相关产业。此外,与煤炭产业相关的人为输入显著加剧了 As、Ni、Ag、Fe 和 Mn 的污染。受蒸发盐和人为输入的影响,中游水样具有高盐度、总硬度和水质指数(WQIs),不适合灌溉或饮用。除交口镇子流域外,FRB 的 WQI 季节性变化不显著,由于采煤,该子流域在雨季的水质比旱季差。由于皮肤接触,F、V、Mn 和 Cr 的非致癌风险较高,应特别注意儿童。总体而言,根据不同的指标,FRB 的地下水水质在上游最好,中游中等,下游最差。FRB 的地下水质量因人为输入和污水排放而恶化,应严格控制污水排放。本研究为类似地区的地下水污染评价和污染源识别提供了参考。

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