Earth Science Frontiers ›› 2021, Vol. 28 ›› Issue (1): 420-427.DOI: 10.13745/j.esf.sf.2020.7.8

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Identification and quantification of factors controlling hydrogen and oxygen isotopes of geothermal water: An example from the Guide Basin, Qinghai Province

DAI Wan1(), JIANG Xiaowei1,*(), LUO Yinfei2,3,4, ZHANG Hong1, LEI Yude2,3,4, TONG Jue2,3,4   

  1. 1. School of Water Resources and Environment, China University of Geosciences (Beijing), Beijing 100083, China
    2. Qinghai 906 Engineering Survey and Design Institute, Xining 810008, China
    3. Qinghai Bureau of Environmental Geology Exploration, Xining 810008, China
    4. Qinghai Provincial Key Laboratory of Environmental Geology, Xining 810008, China
  • Received:2020-03-29 Revised:2020-04-27 Online:2021-01-25 Published:2021-01-28
  • Contact: JIANG Xiaowei

Abstract:

Hydrogen and oxygen isotopes have been widely used in the study of geothermal fluid. However, due to the influences of multiple factors, the understanding of the processes controlling the hydrogen and oxygen isotopic compositions of geothermal water is often incomplete. Here, we conducted a case study on the geothermal water from the two faults along the margin of the Guide Basin. We collected water samples from five hot spring sites and compared the differences in hydrochemical components and geothermal reservoir temperatures of these samples. We found an approximate relationship between the degree of water-rock interaction and whether the sample deviates from the rainfall line. At the intensively studied Zhacangsi site, previous researchers have quantified the effect of cold water mixing in thermal water and determined the cold water mixing ratio. Based on this ratio, we estimated the magnitude of change in hydrogen and oxygen isotopes caused by cold water mixing and liquid-vapor separation. We also established the isotopic compositions of the geothermal water before water-rock interaction based on the effect of the interaction on the “oxygen shift”. The results were consistent with the isotopic compositions of geothermal water from sites with low degrees of water-rock interaction. The methods proposed in the current study can be applied to analyzing hydrogen and oxygen isotopes in other geothermal fields to enrich our understanding of the circulation process of geothermal fluid.

Key words: hydrogeochemical characteristics, hydrogen and oxygen isotopes, water-rock interaction, liquid-vapor separation, Zhacangsi

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