801 Institute of Hydrogeology and Engineering Geology, Shandong Provincial Bureau of Geology & Mineral Resources, Jinan, 250014, Shandong, China.
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, 266590, Shandong, China.
Environ Monit Assess. 2024 May 5;196(6):512. doi: 10.1007/s10661-024-12669-0.
To gain a comprehensive understanding of the hydrochemical characteristics, controlling factors, and water quality of groundwater in the main stream area of Yishu River (MSYR), a study was conducted using water quality data collected during both the dry and wet seasons. Through statistical analysis, hydrochemical methods, fuzzy comprehensive evaluation, and health risk evaluation modeling, the water chemical characteristics of the main stream area of Yishu River were studied, and the water quality of the area was comprehensively evaluated. The findings indicate that HCO and Ca are the predominant anions and cations in the MSYR during the dry and wet seasons, respectively. Moreover, anion concentration in groundwater follows HCO > SO > NO > Cl, while cations are ranked as Ca > Na > Mg > K. Overall, the groundwater manifests as weakly alkaline and is predominantly classified as hard-fresh water. During the wet season, there is greater groundwater leaching and filtration, with rock and soil materials more readily transferred to groundwater, and the concentrations of main chemical components in groundwater are higher than those during the dry season, and the hydrochemical types are primarily characterized as HCO-Ca·Mg and SO·Cl-Ca·Mg types. These results also suggest that the chemical composition of the groundwater in the MSYR is influenced mainly by water-rock interaction. The primary ions originate from the dissolution of silicate rock and carbonate rock minerals, while cation exchange plays a critical role in the hydrogeochemical process. Groundwater in the MSYR is classified mostly as class II water, indicating that it is generally of good quality. However, areas with high levels of class IV and V water are present locally, and NO concentration is a crucial factor affecting groundwater quality. In the wet season, more groundwater and stronger mobility lead to greater mobility of NO and wider diffusion. Therefore, the risk evaluation model shows that nitrate health risk index is higher in the wet season than it is in the dry season, with children being more vulnerable to health risks than adults. To study groundwater in this area, its hydrochemical characteristics, water quality, and health risk assessment are of great practical significance for ensuring water safety for residents and stable development of social economy.
为全面了解伊舒河流域(MSYR)干流区地下水的水化学特征、控制因素及水质状况,利用枯、丰水期采集的水质资料,采用数理统计、水化学方法、模糊综合评价和健康风险评价模型,对伊舒河流域干流区水化学特征进行了研究,并对该区域的水质进行了综合评价。结果表明:枯、丰水期伊舒河流域干流区的优势阴离子和阳离子分别为 HCO 和 Ca。地下水中阴离子浓度依次为 HCO > SO > NO > Cl,阳离子浓度依次为 Ca > Na > Mg > K。整体上,地下水呈弱碱性,主要为硬淡水。丰水期地下水淋溶和过滤作用较强,岩土材料更易向地下水转移,地下水中主要化学成分浓度高于枯水期,水化学类型主要为 HCO-Ca·Mg 和 SO·Cl-Ca·Mg 型。研究结果表明,伊舒河流域干流区地下水的化学组成主要受水-岩相互作用的影响。主要离子来源于硅酸盐岩和碳酸盐岩矿物的溶解,阳离子交换在水地球化学过程中起关键作用。伊舒河流域干流区地下水多属Ⅱ类水,水质总体良好,但局部地区存在Ⅳ、Ⅴ类水,NO 浓度是影响地下水质量的关键因素。丰水期,更多的地下水和更强的流动性导致 NO 迁移性增强,扩散范围更广,因此风险评价模型表明丰水期硝酸盐健康风险指数高于枯水期,儿童比成人更易受到健康风险的影响。研究该区域地下水,对保障居民用水安全和社会经济稳定发展具有重要的现实意义。