Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (1): 217-225.doi: 10.13278/j.cnki.jjuese.20180281

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Hydro-Geological Characteristics and Demarcation of Gudui Spring Karst Groundwater System

Shen Haoyong, Liang Yongping, Zhao Chunhong, Tang Chunlei, Wang Zhiheng   

  1. Key Laboratory of Karst Dynamics, MNR&GZAR(Institute of Karst Geology, CAGS), Guilin 541004, Guangxi, China
  • Received:2018-11-02 Published:2020-02-11
  • Supported by:
    Supported by National Key R&D Program of China(2017YFC0406104),National Natural Science Foundation of China(41672253,41902256)and Project of China Geological Survey(DD20190334,DD20189807)

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Abstract: Gudui Spring is the only low medium temperature geothermal spring in Fenhe River basin. The research of hydro-geological characteristics and demarcation of karst groundwater system is the basis of karst groundwater resource evaluation. On the basis of the geological structural and hydro-geological characteristic analysis and karst groundwater circulation, the Gudui Spring karst groundwater system and subsystem are preliminarily delimited. The results show that the geological structures of the Gudui Spring karst system are complicated, and there are a lot of intrusive igneous rocks and buried faults. The overall geological structure of the system can be described as three uplifts and three subsides both in east-west and north-south directions. The recharge of karst groundwater is mainly from the precipitation of carbonate outcrop areas in Taer Mountain, Erfeng Mountain and Zhongtiao Mountain. Nanliang Spring and Haitou Spring are two local discharge areas;while Gudui Spring is the final discharge area. The boundary of Gudui Spring karst groundwater system and its hydrogeological nature are delimited by using the method of hydro-geological and groundwater circulation characteristic analysis. The area of Gudui Spring karst system is 2 942 km2 and can be divided into four relatively independent systems. The first is Taer Mountain-Jiuyuan Mountain Gudui Spring karst subsystem, the second is Foling Mountain-Gaoxian Haitou Spring karst subsystem, the third is Zhongtiao Mountain Nanliang Spring karst subsystem,and the last is Houma Basin deep circulation karst groundwater subsystem.

Key words: hydro-geological characteristic, karst groundwater system, Gudui Spring, c(Sr)/c(Ca)

CLC Number: 

  • P641
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