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过河流域地表水-地下水-沉积物多功能系统中微量元素的分布、溯源、水质及风险评价。

Distribution, source identification, water quality, and risk assessment of trace elements in the surface-groundwater-sediments multifunctional system in Guohe River Basin.

机构信息

CAS Key Laboratory of Crust-Mantle Materials and Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, 230026, China.

CAS Key Laboratory of Crust-Mantle Materials and Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, 230026, China.

出版信息

J Environ Manage. 2024 Jun;361:121266. doi: 10.1016/j.jenvman.2024.121266. Epub 2024 May 29.

Abstract

Within the Huaihe River Basin, Guohe River, as its second-largest tributary, serves as a critical water supply source. Recent industrial and agricultural advancements have led to increased trace element contamination, adversely impacting the water quality within Guohe River Basin. Therefore, this study aimed to investigate the distribution characteristics, sources, water quality and risk assessment of trace elements in the surface water, groundwater, and sediments across the basin. The results showed that the spatial distribution of trace elements in the surface water and groundwater of Guohe River Basin was that most of the high concentrations appeared in Qiaocheng District of Bozhou City, the mean concentration of Fe in Guohe River sediments was the highest, the mean concentration of Sb was the lowest. The PMF source analysis results showed that the main source of trace elements in Guohe River Basin was natural geological processes, followed by human activities. The sodium adsorption ratio (SAR) indicated that the surface water samples of Guohe River in two seasons had high sodium and salinity hazards. The water quality index (WQI) showed that surface water and groundwater samples in the northwestern of Guohe River Basin had poor water quality. The results of the risk assessment showed that As and Mn posed great ecological risks to surface water and groundwater, respectively, and that F was the pollutant with the most potential health risk hazard in the basin. The Geo-accumulation index (I) results showed that Cd, Se and As should be taken seriously as the main contaminants of the sediments in Guohe River Basin. KEYWARDS: Trace elements; Source analysis; Sodium adsorption ratio; Water quality index; Risk assessment; Geo-accumulation index.

摘要

在淮河流域,郭河是其第二大支流,是重要的供水水源。近年来,工农业的发展导致了痕量元素的污染加剧,对郭河流域的水质产生了不利影响。因此,本研究旨在调查流域地表水、地下水和沉积物中痕量元素的分布特征、来源、水质和风险评估。结果表明,郭河地表水和地下水痕量元素的空间分布特征为:大部分高浓度出现在亳州市谯城区;郭河沉积物中 Fe 的平均浓度最高,Sb 的平均浓度最低。PMF 源分析结果表明,郭河流域痕量元素的主要来源是自然地质过程,其次是人为活动。钠吸附比(SAR)表明,郭河在两个季节的地表水样品具有高钠和高盐度危害。水质指数(WQI)表明,郭河西北部的地表水和地下水样品水质较差。风险评估结果表明,As 和 Mn 分别对地表水和地下水具有较大的生态风险,而 F 是流域内最具潜在健康风险危害的污染物。地积累指数(I)结果表明,Cd、Se 和 As 应被视为郭河沉积物的主要污染物。

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