Gao Heng, Yang Lihu, Song Xianfang, Guo Minli, Li Binghua, Cui Xu
Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Beijing Water Science and Technology Institute, Beijing Engineering Technique Research Center for Exploration and Utilization of Non-Conventional Water Resources and Water Use Efficiency, Beijing 100048, China.
Sci Total Environ. 2023 Dec 10;903:166660. doi: 10.1016/j.scitotenv.2023.166660. Epub 2023 Aug 31.
Ecological water replenishment (EWR) is an essential approach for improving the quantity and quality of regional water. The Chaobai River is a major river in Beijing that is replenished with water from multiple sources, including reclaimed water (RW), the South-North Water Transfer Project (SNTP), reservoir discharge (RD). The effects of multiple water source recharge (MWSR) on groundwater quality remain unclear. In this study, hydrochemical ions, isotopes (δH-HO, δO-HO, δN-NO, and δO-NO), mixing stable isotope analysis in R (MixSIAR), and hydrogeochemical modeling were used to quantify the contributions and impacts of different water sources on groundwater and to propose a conceptual model. The results showed that during the period before reservoir discharge, RW and SNTP accounted for 38 %-41 % and 54 % of the groundwater in their corresponding recharge areas, respectively. The groundwater in the RW recharge area contained high levels of Na and Cl leading to the precipitation of halite, and was the main factor for the spatial variation in groundwater hydrochemical components. The surface water changed from Na·K - Cl·SO type to Ca·Mg - HCO type which was similar to groundwater after reservoir discharge. RD accounted for 30 % of the groundwater; however, it did not change the hydrochemical type of groundwater. Dual nitrate stable isotopes and MixSIAR demonstrated that RW was the primary source of NO in groundwater, contributing up to 76-89 %, and reservoir discharge effectively reduced the contribution of RW. δN-NO or δO-NO in relation to NO-N suggests that denitrification is the main biogeochemical process of nitrogen in groundwater, whereas water recharge from the SNTP and RD reduces denitrification and dilutes NO. This study provides insights into the impact of anthropogenically controlled ecological water replenishment from different water sources on groundwater and guides the reasonable allocation of water resources.
生态补水是改善区域水量和水质的重要途径。潮白河是北京的一条主要河流,其水源补给来自多个方面,包括再生水、南水北调工程以及水库泄水。多水源补给对地下水水质的影响尚不清楚。本研究利用水化学离子、同位素(δH-H₂O、δ¹⁸O-H₂O、δ¹⁵N-NO₃和δ¹⁸O-NO₃)、R中的混合稳定同位素分析(MixSIAR)以及水文地球化学模型,量化不同水源对地下水的贡献和影响,并提出一个概念模型。结果表明,在水库泄水前的时期,再生水和南水北调工程分别占其相应补给区地下水的38%-41%和54%。再生水补给区的地下水中Na和Cl含量较高,导致石盐沉淀,是地下水中水化学成分空间变化的主要因素。地表水从Na·K-Cl·SO₄型转变为Ca·Mg-HCO₃型,与水库泄水后的地下水相似。水库泄水占地下水的30%;然而,它并没有改变地下水的水化学类型。双硝酸盐稳定同位素和MixSIAR表明,再生水是地下水中NO₃的主要来源,贡献率高达76%-89%,而水库泄水有效地降低了再生水的贡献率。δ¹⁵N-NO₃或δ¹⁸O-NO₃与NO₃-N的关系表明,反硝化作用是地下水中氮的主要生物地球化学过程,而南水北调工程和水库泄水的补水减少了反硝化作用并稀释了NO₃。本研究为不同水源的人为控制生态补水对地下水的影响提供了见解,并指导水资源的合理配置。