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Volume 1 Issue 3
Sep.  2014
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Zong-jun Gao, Yong-gui Liu. 2013: Groundwater Flow Driven by Heat. Journal of Groundwater Science and Engineering, 1(3): 22-27.
Citation: Zong-jun Gao, Yong-gui Liu. 2013: Groundwater Flow Driven by Heat. Journal of Groundwater Science and Engineering, 1(3): 22-27.

Groundwater Flow Driven by Heat

  • The temperature of groundwater will be increasing gradually while it is recharged and infiltrated down to the depth because of the geothermal gradient. So the density of water is smaller and smaller. The author puts forward the heat-driving mechanism that the movement of the groundwater is caused by the density differences from different temperatures. Based on this idea, the author proposes the short range recharge model of geothermal water in flat terrain hilly area. The model explains the coexistence mechanism of recharge and discharge (hot springs) zones can be at the same altitude. Considering that the temperature is an important driving force of groundwater movement, the paper puts forward and demonstrates that the hot springs can expose at higher lands while the recharge zone being situated lower lying areas.
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  • Tóth J. Groundwater As a Geologic Agent: An Overview of the Causes, Processes and Manifestations [J]. Hydrogeology Journal, 1999, 7:1-14
    Completion Report Taiyang Village, Yangcun Town, Hejin city City [R], 2013.08
    Zong-jun Gao, Demonstration of Underground Water Variation and Its Significance [J]. Journal of Shandong University of Science and Technology (NATURAL SCIENCE EDITION), 2013, 32 (2): 17-24
    GB/T11615-2010. Geologic Exploration Standard of Geothermal Resources [S]. Beijing:
    The Second Shanxi Institute of Geological Engineering Investigation. Geothermal Well
    Chinese Standard Press, 2011.01
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