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Volume 30 Issue 4
Aug 2019
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Journal of Earth Science  > 2019  >  30(4): 870-878.
Xiuhua Zheng, Chenyang Duan, Bairu Xia, Yong Jiang, Jian Wen. Hydrogeochemical Modeling of the Shallow Thermal Water Evolution in Yangbajing Geothermal Field, Tibet. Journal of Earth Science, 2019, 30(4): 870-878. doi: 10.1007/s12583-016-0918-7
Citation: Xiuhua Zheng, Chenyang Duan, Bairu Xia, Yong Jiang, Jian Wen. Hydrogeochemical Modeling of the Shallow Thermal Water Evolution in Yangbajing Geothermal Field, Tibet. Journal of Earth Science, 2019, 30(4): 870-878. doi: 10.1007/s12583-016-0918-7
shu

Hydrogeochemical Modeling of the Shallow Thermal Water Evolution in Yangbajing Geothermal Field, Tibet

doi: 10.1007/s12583-016-0918-7
  • 1.

    School of Engineering and Technology, China University of Geosciences, Beijing 100083, China

  • 2.

    State Grid Lhasa Power Supply Company, Lhasa 850000, China

  • 3.

    Yangbajing Geothermal Power Station, State Grid Tibet Electric Power Company Limited, Lhasa 850000, China

Funds:

the China Geological Survey 121201112006

the National Natural Science Foundation of China 41572361

More Information
  • Corresponding author: Chenyang Duan
  • Received Date: 10 May 2016
  • Accepted Date: 27 Dec 2016
  • Publish Date: 01 Aug 2019
    Abstract
  • The exploitation of thermal water and the mix of cold water changed the properties of geofluid in shallow reservoir, which altered the concentration of the chemical constitutes and continuously built new water-rock reaction. This paper deduced reservoir pressure and temperature variation tendency from 2004 to 2013, analyzed the change of some components in the shallow reservoir water, and finally obtained the evolution of the shallow geothermal water with hydrogeochemical model. The results show the reservoir pressure decreased significantly compared with the slight decline of reservoir temperature, and much cold groundwater infiltrated into the shallow reservoir, which affected the solubility of SiO2 and led to precipitation, the increased CO2 in shallow reservoir promoted the dissolution of aluminosilicate. Calcite and kaolinite precipitation zone has extended to the north in the field, which influenced the porosity of the reservoir rock.

     

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