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Volume 41 Issue 1
Jan.  2022
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Article Navigation >  Bulletin of Geological Science and Technology  > 2022  >  41(1): 278-287, 299
Sun Hongli, Wang Guiling, Lin Wenjing. Distribution characteristics and enrichment mechanism of TDS geothermal water in Xining Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(1): 278-287, 299. doi: 10.19509/j.cnki.dzkq.2021.0079
Citation: Sun Hongli, Wang Guiling, Lin Wenjing. Distribution characteristics and enrichment mechanism of TDS geothermal water in Xining Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(1): 278-287, 299. doi: 10.19509/j.cnki.dzkq.2021.0079
shu

Distribution characteristics and enrichment mechanism of TDS geothermal water in Xining Basin

doi: 10.19509/j.cnki.dzkq.2021.0079
  • Received Date: 20 Mar 2021
    Available Online: 02 Mar 2022
    Abstract
  • The high concentration of TDS in most of the geothermal water in Xining Basin greatly restricted the availability of geothermal water.In order to provide reference value for the later development and utilization of geothermal resources, the enrichment mechanisms of TDS were identified.Based on the analysis of major and trace components of hot and cold underground water along the line from Yaoshuitan to central basin, the distribution characteristics and enrichment mechanism of TDS in the basin were discussed.It was shown that the groundwater changed from fresh water to brine with hydrochemical types changed from HCO3-Ca·Mg to SO4·Cl-Na and SO4-Na, characterized by continental sedimentary water.The metamorphic degree gradually increased from the edge to the central part of the basin.The enrichment mechanisms of TDS were also significantly different in different regions of the basin.On the margin, the precipitation infiltration, minerals' dissolution and mixing among different aquifer were the dominated mechanisms; In Huangshui transitional zone, evaporation, mixing and water-rock interaction were the main mechanisms; while in the central basin, the dominated factors were the mixing of deep sediments or saline material upwelling with hydrothermal from the deep and the water-rock interaction in closed environment.

     

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