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Interaction of Surface Water and Groundwater Influenced by Groundwater Over-Extraction, Waste Water Discharge and Water Transfer in Xiong'an New Area, China
Zhu, Meijia1,2; Wang, Shiqin1; Kong, Xiaole1,2; Zheng, Wenbo1; Feng, Wenzhao1,2,3; Zhang, Xianfu4; Yuan, Ruiqiang5; Song, Xianfang6; Sprenger, Matthias7,8
2019-03-15
Source PublicationWATER
ISSN2073-4441
Volume11Issue:3Pages:23
Corresponding AuthorWang, Shiqin(sqwang@sjziam.ac.cn)
AbstractUnderstanding the interaction of surface water and groundwater affected by anthropogenic activities is of great importance for water resource and water quality management. The Xiong'an New Area, located in the North China Plain, has been designated a new building area by China's government. Groundwater has been over pumped and artificial water was transferred to meet the water supply in this region. Therefore, the natural interaction of surface water and groundwater has been greatly changed and there has been a complex impact of the groundwater from anthropogenic activities. In this study, we used water chemical ions and stable isotopes of delta H-2 and delta O-18 to assess the interaction of surface water and groundwater in the Xiong'an New Area. We carried out field surveys and water sampling of the Fu River (domestic waste water discharge), Lake Baiyangdian (artificial water transfer), and the underlying groundwater along the water bodies. Results show that the artificial surface water (discharged and transferred) became the major recharge source for the local groundwater due to the decline of groundwater table. We used groundwater table observations, end-member mixing analysis of the stable isotopic composition and chloride tracers to estimate the contributions of different recharge sources to the local groundwater. Due to the over pumping of groundwater, the lateral groundwater recharge was dominant with a contribution ratio ranging from 12% to 78% in the upper reach of the river (Sections 1-3). However, the contribution of lateral groundwater recharge was estimated to be negligible with respect to the artificial water recharge from Lake Baiyangdian. Seepage from the Fu River contributed a significant amount of water to the connecting aquifer, with a contribution ranging from 14% to 75% along the river. The extent of the river influence into the aquifer ranges as far as 1400 m to the south and 400 m to the north of the Fu River. Estimations based on isotopic fractionation shows that about 22.3% of Lake Baiyangdian water was lost by evaporation. By using the stable isotopes of oxygen and hydrogen in the lake water, an influencing range of 16 km west of the lake was determined. The interaction of the surface water and groundwater is completely changed by anthropogenic activities, such as groundwater over pumping, waste water discharge and water transfer. The switched interaction of surface water and groundwater has a significant implication on water resources management.
Keywordsurface water-groundwater interaction anthropogenic activities groundwater over-exploitation groundwater recharge end-member mixing analysis (EMMA) North China Plain Xiong'an New Area
DOI10.3390/w11030539
WOS KeywordSTABLE-ISOTOPES ; TAIHANG MOUNTAINS ; HYDROGEN ISOTOPES ; ALLUVIAL AQUIFER ; MASS-BALANCE ; RIVER-BASIN ; RECHARGE ; EVOLUTION ; REGION ; IMPACTS
Indexed BySCI
Language英语
Funding ProjectNational Key R&D Program of China[2018YFC0406502] ; National Key R&D Program of China[2018YFD0800306] ; National Key R&D Program of China[2016YFD0800100] ; Key R&D Program of Hebei[18273604D] ; Program of National Natural Science Foundation of China[41471028] ; 100-Talent Project of Chinese Academy of Sciences
Funding OrganizationNational Key R&D Program of China ; Key R&D Program of Hebei ; Program of National Natural Science Foundation of China ; 100-Talent Project of Chinese Academy of Sciences
WOS Research AreaWater Resources
WOS SubjectWater Resources
WOS IDWOS:000464536400004
PublisherMDPI
Citation statistics
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/48262
Collection中国科学院地理科学与资源研究所
Corresponding AuthorWang, Shiqin
Affiliation1.Chinese Acad Sci, Inst Genet & Dev Biol, Ctr Agr Resources Res, Key Lab Agr Water Resources, Shijiazhuang 050021, Hebei, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Hebei GEO Univ, Sch Land Resources & Urban Rural Planning, 136 East Huaian Rd, Shijiazhuang 050031, Hebei, Peoples R China
4.Hebei GEO Univ, Sch Water Resources & Environm, 136 East Huaian Rd, Shijiazhuang 050031, Hebei, Peoples R China
5.Shanxi Univ, Sch Environm Sci & Resources, Taiyuan 030006, Peoples R China
6.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
7.CSIC, IDAEA, Inst Environm Assessment & Water Res, ES-08034 Barcelona, Spain
8.North Carolina State Univ, Dept Forestry & Environm Resources, Raleigh, NC 27695 USA
Recommended Citation
GB/T 7714
Zhu, Meijia,Wang, Shiqin,Kong, Xiaole,et al. Interaction of Surface Water and Groundwater Influenced by Groundwater Over-Extraction, Waste Water Discharge and Water Transfer in Xiong'an New Area, China[J]. WATER,2019,11(3):23.
APA Zhu, Meijia.,Wang, Shiqin.,Kong, Xiaole.,Zheng, Wenbo.,Feng, Wenzhao.,...&Sprenger, Matthias.(2019).Interaction of Surface Water and Groundwater Influenced by Groundwater Over-Extraction, Waste Water Discharge and Water Transfer in Xiong'an New Area, China.WATER,11(3),23.
MLA Zhu, Meijia,et al."Interaction of Surface Water and Groundwater Influenced by Groundwater Over-Extraction, Waste Water Discharge and Water Transfer in Xiong'an New Area, China".WATER 11.3(2019):23.
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