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Structural Control on Groundwater Distribution and Flow in the South of Ningxia Hui Autonomous Region, China

Fawang Zhang1,2, Zhantao Han1( ), Xinwei Hou1
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, China, 050061
Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China, 541004
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Abstract

Structural control on groundwater distribution and flow in the south of Ningxia Hui Autonomous Region, China was investigated and analyzed. Intensive geological movement in geological history has resulted in a complex tectonic structure, and a complex distribution and flow pattern of groundwater. Based on the hydrogeological investigation, 4 types of water bearing structure (WBS) were discovered: Porous WBS, Fissure WBS, Karst WBS and Fissure-porous WBS. These WBSs and their combinations provided the varied storage spaces and flowing channels for groundwater in SNHAR.

Keywords

The south of NingxiaWater bearing structureDistributionTypeCharacteristic of control water

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Journal of Groundwater Science and Engineering
Volume 1 Issue 2,
July 2013
Pages 1-8
DOI: 10.26599/JGSE.2013.9280013

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Cite this article:
Zhang F, Han Z, Hou X. Structural Control on Groundwater Distribution and Flow in the South of Ningxia Hui Autonomous Region, China. Journal of Groundwater Science and Engineering, 2013, 1(2): 1-8. https://doi.org/10.26599/JGSE.2013.9280013

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Published: 28 July 2013
© 2013 Journal of Groundwater Science and Engineering Editorial Office