Genetic Analysis of Chenjiazhuang Spring in Yongding River, Beijing

WANG Xinjuan; HAN Liru; LU Zhongyang; HAN Xu; LIU Yin; XU Miaojuan

doi:10.12401/j.nwg.2023163

2024 Vol. 57, No. 3

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Article navigation > Northwestern Geology > 2024 > 57(3): 262-271

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WANG Xinjuan, HAN Liru, LU Zhongyang, HAN Xu, LIU Yin, XU Miaojuan. 2024. Genetic Analysis of Chenjiazhuang Spring in Yongding River, Beijing. Northwestern Geology, 57(3): 262-271. doi: 10.12401/j.nwg.2023163

Citation:

WANG Xinjuan, HAN Liru, LU Zhongyang, HAN Xu, LIU Yin, XU Miaojuan. 2024. Genetic Analysis of Chenjiazhuang Spring in Yongding River, Beijing. Northwestern Geology, 57(3): 262-271. doi: 10.12401/j.nwg.2023163

Genetic Analysis of Chenjiazhuang Spring in Yongding River, Beijing

1.
Beijing Geological Environment Monitoring Institute, Beijing 100195, China
2.
Mengcun Hui Autonomous County Water Bureau, Cangzhou 061400, Hebei, China

Received Date: 06 March 2023

Revised Date: 31 July 2023

Accepted Date: 17 August 2023

Publish Date: 20 June 2024

Abstract

Abstract

Chenjiazhuang Spring is located on the Yongding River. Since the ecological environment improvement project of Yongding River was carried out, the spring flowed out in 2019. In order to protect and manage Chenjiazhuang Spring, realize the ecological environment management of Yongding River and regional water resources strategic reserve, spring origin analysis and spring domain division were carried out.The recharge source, recharge elevation and recharge temperature of the spring were obtained by testing and analyzing the isotope and hydrochemistry samples of rainwater, river water and groundwater in the spring area; On the basis of the above analysis, combined with the regional geological and hydrogeological conditions, delimit the spring catchment area. The results show that the Chenjiazhuang spring exists in the Ordovician limestone aquifer,the regional karst groundwater recharge source is atmospheric precipitation and Yongding River water, the spring is an exposed erosion overflow spring, the spring recharge elevation is 736 m, the recharge temperature is 13.12 ℃, the catchment area of the spring is 30.6 km².
- groundwater /
- spring /
- isotope /
- hydrochemical /
- formation mechanism /
- Beijing

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References

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