Recharge sources, model and development potential of typical tectonic karst groundwater in the eastern Qinghai−Xizang Plateau

MA Jianfei; LI Xiangquan; ZHANG Chunchao; FU Changchang; XIE Xiaoguo; WANG Xiaogang; LI Xinze; ZHANG Dengfei; BAI Zhanxue; WANG Zhenxing

doi:10.12029/gc20220416004

2025 Vol. 52, No. 1

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Article navigation > Geology in China > 2025 > 52(1): 347-361

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MA Jianfei, LI Xiangquan, ZHANG Chunchao, FU Changchang, XIE Xiaoguo, WANG Xiaogang, LI Xinze, ZHANG Dengfei, BAI Zhanxue, WANG Zhenxing. 2025. Recharge sources, model and development potential of typical tectonic karst groundwater in the eastern Qinghai−Xizang Plateau[J]. Geology in China, 52(1): 347-361. doi: 10.12029/gc20220416004

Citation:

MA Jianfei, LI Xiangquan, ZHANG Chunchao, FU Changchang, XIE Xiaoguo, WANG Xiaogang, LI Xinze, ZHANG Dengfei, BAI Zhanxue, WANG Zhenxing. 2025. Recharge sources, model and development potential of typical tectonic karst groundwater in the eastern Qinghai−Xizang Plateau[J]. Geology in China, 52(1): 347-361. doi: 10.12029/gc20220416004

Recharge sources, model and development potential of typical tectonic karst groundwater in the eastern Qinghai−Xizang Plateau

1.
Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang 050061, Hebei, China
2.
Key Laboratory of Groundwater Sciences and Engineering, Ministry of Natural Resources, Shijiazhuang 050061, Hebei, China
3.
Chengdu Center of Hydrogeology and Engineering Geology, SBGEEMR, Chengdu 610081, Sichuan, China
4.
Sichuan Huadi Construction Engineering Co., Ltd, Chengdu 610081, Sichuan, China
5.
Sichuan Institute of Uranium Geological Survey, Chengdu 610052, Sichuan, China
6.
Department of Geology, State Key Laboratory of Continental Dynamics, Northwest University, Xi’an 710069, Shaanxi, China

Fund Project: Supported by the projects of China Geological Survey (No. DD20211374, No. DD20221812, No.DD20230537), Chinese Academy of Geological Sciences (No. SK202205).

More Information

Author Bio: MA Jianfei, male, born in 1987, associate researcher, engaged in research on hydrogeology and engineering geology; E-mail: majianfei@mail.cgs.gov.cn

Received Date: 16 April 2022

Revised Date: 02 June 2022

Publish Date: 25 January 2025

Abstract

Abstract

This paper is the result of hydrogeological survey engineering.
Objective
There are many tectonic karst areas with complex karst hydrogeological structures, diverse recharge sources, and abundant groundwater in the eastern part of the Qinghai−Xizang Plateau. Analyses and research of the recharge sources and details about the controls on groundwater cycling in the tectonic karst on the plateau are important for guiding the development and utilization of karst water resources, protecting the ecology, and preventing and reducing disasters.
Methods
Using information from field investigations, flow measurements, hydrochemistry and stable isotope analysis, we analyzed the groundwater recharge sources in the karst areas in the eastern part of the Qinghai−Xizang Plateau, considered the factors that influenced the recharge sources and recharge progress, and made recommendations for the development and utilization of the groundwater.
Results
Atmospheric precipitation was the main recharge source of the main karst springs on the eastern Qinghai−Xizang Plateau. There were four main recharge modes, including direct recharge through high−level fissures, continuous recharge from high−level lakes, continuous seepage recharge in catchment depressions, and river seepage.
Conclusions
The different recharge modes in the eastern Qinghai−Xizang Plateau developed over sustained time periods because of the coupling of internal factors, such as the history of the karst formation and its evolution, the geological structure, and the lithologic combination, and external factors, such as the meteorology, the landforms, and glacier movements. From our analysis of the characteristics of the water quality and quantity of the karst springs, we developed three categories for the development and utilization of the groundwater resource, namely karst springs with water quality in classes Ⅰ–Ⅲ, the development and utilization of which can be expanded; brackish water, which can be developed and utilized after mixing with other water; and salt water, which can be transformed and used for developing tourism.
- eastern Qinghai−Xizang Plateau /
- geological safety risk investigation and evaluation /
- tectonic karst /
- groundwater /
- recharge source /
- supply mode /
- karst hydrogeology /
- development and utilization /
- hydrogeological survey engineering

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References

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