胡君春, 郭纯青. 石家庄凹陷地热资源研究[J]. 地质与资源, 2008, 17(4): 297-301. DOI: 10.13686/j.cnki.dzyzy.2008.04.007
    引用本文: 胡君春, 郭纯青. 石家庄凹陷地热资源研究[J]. 地质与资源, 2008, 17(4): 297-301. DOI: 10.13686/j.cnki.dzyzy.2008.04.007
    HU Jun-chun, GUO Chun-qing. STUDY ON THE GEOTHERMAL WATER RESOURCE IN SHIJIAZHUANG DEPRESSION[J]. Geology and Resources, 2008, 17(4): 297-301. DOI: 10.13686/j.cnki.dzyzy.2008.04.007
    Citation: HU Jun-chun, GUO Chun-qing. STUDY ON THE GEOTHERMAL WATER RESOURCE IN SHIJIAZHUANG DEPRESSION[J]. Geology and Resources, 2008, 17(4): 297-301. DOI: 10.13686/j.cnki.dzyzy.2008.04.007

    石家庄凹陷地热资源研究

    STUDY ON THE GEOTHERMAL WATER RESOURCE IN SHIJIAZHUANG DEPRESSION

    • 摘要: 地热资源作为一种洁净环保能源被开发利用在石家庄有着悠久的历史.为评估地热资源开发潜力和前景,从石家庄凹陷区地热地质条件、已知地热信息及水文地球化学过程跟踪,归纳出地热水化学类型,分析石家庄地区地热水的形成时代、热储温度、热水动态特征,并对热水补给来源进行同位素分析.结果表明参与混合的冷水年代久远,地热水水温稳定,水量大,有较大开发潜力.

       

      Abstract: The geothermal resources have been exploited in Shijiangzhuang depression for a long history. Hydrochemistry and isotopic tracing studies are carried out for the geothermal fields in order to assess the heat energy potentials and the exploration prospect. Analysis on the geological background, available geothermal information and buried condition of hot water, as well as geochemical and isotopic characteristics of the water from geochemical dill holes, rainwater and surface water, indicates that the underground thermal water in Shijiangzhuang depression is characterized by constant temperature and large amount, with a great economic potential.

       

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