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Volume 34 Issue 3
Jun.  2015
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Article Navigation >  CARSOLOGICA SINICA  > 2015  >  34(3): 209-216
LI Ming-li, DUO Ji, WANG Zhu, WU Guo-dong, JIANG Zhen-zhen, LIU Gao-ling. Hydrochemical characteristics and material sources of the Riduo thermal spring in Tibet[J]. CARSOLOGICA SINICA, 2015, 34(3): 209-216. doi: 10.11932/karst20150302
Citation: LI Ming-li, DUO Ji, WANG Zhu, WU Guo-dong, JIANG Zhen-zhen, LIU Gao-ling. Hydrochemical characteristics and material sources of the Riduo thermal spring in Tibet[J]. CARSOLOGICA SINICA, 2015, 34(3): 209-216. doi: 10.11932/karst20150302
shu

Hydrochemical characteristics and material sources of the Riduo thermal spring in Tibet

doi: 10.11932/karst20150302
  • 1.

    College of Earth Sciences，Chengdu University of Techenology/Lhasa Mineral Resources Supervise Test Centre，Ministry of Land and Resources

  • 2.

    College of Earth Sciences，Chengdu University of Techenology/Department of Land and Resources of Tibet Autonomous Region

  • 3.

    Lhasa Mineral Resources Supervise Test Centre，Ministry of Land and Resources

  • Publish Date: 2015-06-25
    Abstract
  • Hydrochemical characteristics of hot springs include geological, tectonic, fractured, alteration and hydro-environmental change information during the spring’s formation. So hot spring’s hydrochemistry analyze is the most important and basic method for hot spring formation and material source research. The Riduo spring is located in Riduo, Lhasa, Tibet. It occurs in Palaeocene Dianzhong Formation (E1d) and Lower Cretaceous Linbuzong Formation (K1l). The hydrochemical characteristics show the spring is neutral water with SO4·HCO3-Na. Its temperature is about 97.5-110.1 ℃. The positive ions are mainly Na+, Ca2+, and K+, while the negative ones are Cl-, SO42-, and HCO3-.The degree of mineralization is about 1 162-1 245 mg/L, with abundant of HBO2, H2SiO3, F, Li, Sr, Cs, and As, meeting the standard of physiotherapy (medical) hot spring quality. The characteristics are directly related to the deep water cycle, long-term underground residence (presumably greater than 48a) and intense water-rock interaction between the hot water and volcanic rock. Comprehensive study of hot spring’s hydrochemistry help to reveal the hot spring’s formation, and benefit the recourse rational use and protection.

     

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