Unique characteristics of groundwater occurrence and its development and utilization model in the Wumeng Mountain area -a case study of the Zhaojue area

被引:0
|
作者
Fan L. [1 ,2 ]
Zou S. [2 ]
Xie Q. [1 ]
Lu L. [2 ]
Lin Y. [2 ]
Zhu D. [2 ]
Wang J. [2 ]
Zhou C. [2 ]
Li J. [3 ]
机构
[1] School of Environmental Science & Engineering, Guilin University of Technology, Guilin
[2] Institute of Karst Geology, Chinese Academy of Geological Sciences, Key Laboratory of Karst Dynamics, Ministry of Natural Resources & Guangxi, Guilin
[3] Hebei Key Laboratory of Water Quality Engineering and Comprehensive Utilization of Water Resources, Hebei University of Architecture, Zhangjiakou
来源
Dizhi Xuebao/Acta Geologica Sinica | 2021年 / 95卷 / 11期
关键词
Development and utilization mode; Groundwater; Occurrence regularity; Wumeng Mountain area; Zhaojue County;
D O I
10.19762/j.cnki.dizhixuebao.2021187
中图分类号
学科分类号
摘要
A comprehensive research approach using surface hydrogeology survey, hydrogeological drilling and groundwater resources development and utilization, found that the groundwater types in the study area are mainly bedrock fissure pore water, carbonate karst water, and Quaternary loose rock pore water as auxiliary, and the occurrence characteristics of different types of groundwater are summarized. The influence of geological structure on groundwater migration, storage, enrichment and discharge in the study area is clarified from the characteristics of fracture, fold and fracture development. Fracture crushing zone usually has water-blocking effect, while in the influence zone of one or both sides of the fault is often filled with water, and the groundwater discharge zone is easily formed along the development direction of fault zone. Secondary fault is the main structure controlling the deep hot water active channel in the research area. Syncline structure makes shallow fissure water and lower layer water enriched, forming syncline water storage basin. The near East-West tensile and X joint fissures are beneficial for the enrichment of groundwater. According to the main topography and aquifer characteristics, the study area is divided into three main types: intermountain basin, hilly area and karst area. Through the analysis and summary of groundwater occurrence characteristics and laws in each type of area, combined with the feasibility of development and utilization, three groundwater development and utilization modes are summarized: the drilling and pumping model of water storage structure in the intermountain basin, the regulation and storage model of surface spring pool in the hilly area, and the surface underground joint model of the reservoir formation of the depression and the underground river plugging hole in the karst mountainous area. The research results provide a scientific basis for improving the efficiency of groundwater development and utilization in the Wumeng Mountain area and solving the problem of water use in this area. © 2021, Science Press. All right reserved.
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页码:3544 / 3555
页数:11
相关论文
共 27 条
  • [1] Wei Chang, Kun Huang, Cheng Hu, Qing Wang, Ningtao Wang, Characteristics of the aquifer structure and groundwater conversion model in the northeastern Yunying basin, Hydrogeology and Engineering Geology, 46, 5, pp. 9-15, (2019)
  • [2] Geping Chen, The significance of the Karst groundwater exploitation in the drinking water security of the country, Guizhou Province, Guizhou Geology, 25, 1, pp. 6-10, (2008)
  • [3] Tao Hong, Yunqiu Xie, Qiwen Yu, Yi Zhao, Guangshuai Zhao, Lichao Yang, Hydrochemical characteristics study and genetic analysis of groundwater in a key region of the Wumeng Mountain, southwestern China, Earth and Environment, 44, 1, pp. 11-18, (2016)
  • [4] Zhongcheng Jiang, Riyuan Xia, Jian Shi, Jianguo Pei, Shiyi He, Bin Liang, The application effects and exploitation capacity of karst underground water resources in southwest china, Acta Geoscientica Sinica, 27, 5, pp. 495-502, (2006)
  • [5] Haoran Li, Yingjie Hao, Zi Lu, Characteristics of water resources in China and its impact on regional economy, Territory & Natural Resources Study, 4, pp. 63-65, (2007)
  • [6] Jiuyi Li, Lijuan Li, Water resources supporting capacity to regional socio-economic development of China, Acta Geographica Sinica, 67, 3, pp. 410-419, (2012)
  • [7] Xinbiao Liu, Occurrence characteristics of cretaceous groundwater and its resource attribute inLongdong basin, Groundwater, 32, 6, pp. 39-40, (2010)
  • [8] Xiaodong Pan, Jie Zeng, Kun Ren, Youjun Jiao, Cong Peng, Ganjiang Lan, Groundwater occurrence characteristics and drilling well models in karst slope zone, Bijie, Guizhou Province, Acta Geoscientica Sinica, 39, 5, pp. 97-103, (2018)
  • [9] Zuoqi Tang, Ruimin Li, Wenlang Qiao, Zhiqiang Yin, Qiong Liu, Wu Chen, Degang Zhao, A study of the environmental carrying capacity of groundwater resources in Southwest Karst mountain areas: a case study of Qixingguan District of Guizhou Province, Geological Bulletin of China, 39, 1, pp. 124-130, (2020)
  • [10] Xinfeng Wang, Mian Song, Lei Gong, Pan Xiao, Jin He, Yuanqing Liu, An analysis of characteristics of groundwater occurrence and typical model of water-storage structures in water-deficient areas of southern Jiangxi Province: a case study of Xingguo County, Acta Geoscientica Sinica, 39, 5, pp. 64-70, (2018)