中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sources and hydrogeochemical processes of groundwater under multiple water source recharge condition

文献类型:期刊论文

作者Gao, Heng1,2; Yang, Lihu1,2; Song, Xianfang1,2; Guo, Minli3; Li, Binghua2; Cui, Xu1,2
刊名SCIENCE OF THE TOTAL ENVIRONMENT
出版日期2023-12-10
卷号903页码:14
ISSN号0048-9697
关键词Multiple water sources recharge Groundwater Hydrogeochemical process MixSIAR Water and nitrate stable isotopes
DOI10.1016/j.scitotenv.2023.166660
通讯作者Yang, Lihu(yanglihu@igsnrr.ac.cn) ; Song, Xianfang(songxf@igsnrr.ac.cn)
英文摘要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 (delta H-2-H2O, delta O-18-(HO)-O-2, delta N-15-NO3-, and delta O-18-NO3-), 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 center dot K - Cl center dot SO4 type to Ca center dot Mg - HCO3 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 NO3- in groundwater, contributing up to 76-89 %, and reservoir discharge effectively reduced the contribution of RW. delta N-15-NO3- or delta O-18-NO3- in relation to NO3-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 NO3-. 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.
WOS关键词RECLAIMED WATER ; CHAOBAI RIVER ; AQUIFER ; NITRATE ; IDENTIFICATION ; INFILTRATION ; IMPACT ; HUAI
资助项目National Natural Science Foundation of China[42377064] ; National Natural Science Foundation of China[41730749]
WOS研究方向Environmental Sciences & Ecology
语种英语
出版者ELSEVIER
WOS记录号WOS:001158681300001
资助机构National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/202724]  
专题中国科学院地理科学与资源研究所
通讯作者Yang, Lihu; Song, Xianfang
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Beijing Water Sci & Technol Inst, Beijing Engn Tech Res Ctr Explorat & Utilizat Nonc, Beijing 100048, Peoples R China
推荐引用方式
GB/T 7714
Gao, Heng,Yang, Lihu,Song, Xianfang,et al. Sources and hydrogeochemical processes of groundwater under multiple water source recharge condition[J]. SCIENCE OF THE TOTAL ENVIRONMENT,2023,903:14.
APA Gao, Heng,Yang, Lihu,Song, Xianfang,Guo, Minli,Li, Binghua,&Cui, Xu.(2023).Sources and hydrogeochemical processes of groundwater under multiple water source recharge condition.SCIENCE OF THE TOTAL ENVIRONMENT,903,14.
MLA Gao, Heng,et al."Sources and hydrogeochemical processes of groundwater under multiple water source recharge condition".SCIENCE OF THE TOTAL ENVIRONMENT 903(2023):14.

入库方式: OAI收割

来源:地理科学与资源研究所

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