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LI Shengtao, YUE Dongdong, FENG Zhaolong, SONG Jian, LIU Donglin, SONG Zhibin, HE Guolei, LONG Hui, HAO Wenjie, ZHANG Qiuxia. Sinoprobe and parameters study on deep karst geothermal reservoir in the Donglihu Area, Tianjin and its exploitable potential analysis[J]. GEOLOGY IN CHINA, 2022, 49(6): 1732-1746. DOI: 10.12029/gc20220603
Citation: LI Shengtao, YUE Dongdong, FENG Zhaolong, SONG Jian, LIU Donglin, SONG Zhibin, HE Guolei, LONG Hui, HAO Wenjie, ZHANG Qiuxia. Sinoprobe and parameters study on deep karst geothermal reservoir in the Donglihu Area, Tianjin and its exploitable potential analysis[J]. GEOLOGY IN CHINA, 2022, 49(6): 1732-1746. DOI: 10.12029/gc20220603
shu

Sinoprobe and parameters study on deep karst geothermal reservoir in the Donglihu Area, Tianjin and its exploitable potential analysis

  • 1.

    Center for Hydrogeology and Environmental Geology, China Geology Survey, Baoding 071051, Hebei, China

  • 2.

    Geological Environment Monitoring Engineering Technology Innovation Center of the Ministry of Natural Resources, Baoding 071051, Hebei, China

  • 3.

    Institute of Exploration Techniques, Chinese Academy of Geosciences, Langfang 065000, Hebei, China

  • 4.

    College of New Energy and Environment, Jilin University, Changchun 130026, Jilin, China

Funds: 

the National Key Research and Development Program 2018YFC0604305

the projects of China Geological Survey DD20190127

the projects of China Geological Survey DD20179621

the projects of China Geological Survey DD20221680

More Information
  • Author Bio:

    LI Shengtao, male, born in 1982, doctor candidate, professor level senior engineer, engaged in the research of hydrogeology, geothermal geology, and thermal storage engineering; E-mail: list07@mails.jlu.edu.cn

  • Corresponding author:

    LIU Donglin, male, born in 1985, master, senior engineer, engaged in the research of groundwater science and engineering, thermal storage engineering; E-mail: liudonglin967@126.com

  • Received Date: May 17, 2020
  • Revised Date: June 23, 2020
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • This paper is the result of geothermal resource survey engineering.

    Objective 

    Tianjin is abundant in geothermal resources with high utilization level, and section 4-3 in Wumishan Formation of Jixian system is the main development dolomite reservoir at present. With the development intensity of geothermal fluid increasing, the exploitation potential of some areas has reached the limit. Exploring the deep geothermal resources and increasing the allowable productions have become one of the effective ways to ensure the sustainable development of geothermal resources in Tianjin.

    Methods 

    Donglihu area is the key research region in this study. Deep geophysical detection had been carried out and geothermal scientific exploration well CGSD-01 had been drilled.

    Results 

    The main results are listed as follows: (1)CGSD-01 drilling encountered the section 2 of Wumishan Formation at 3715 m, a set of purplish red argillaceous dolomite with light gray fine-grained dolomite is developed at the bottom of the section 3 of Wumishan Formation overlying, the thickness is about 73 m, and the fissures are not developed, which can be considered as aquiclude or aquitard; (2)The completion depth of CGSD-01 is 4051.68 m, and the bottom temperature is 106℃, specific field is 1.53 m3/h·m, permeability is 0.40 m/d, conductivity is 48.69 m2/d; (3)The geothermal fluid type of the section 2 of Wumishan Formation is Cl·SO4·HCO3-Na, salinity is 1.7 g/L. It is preliminarily inferred that the geothermal water is originated from atmospheric precipitation, and mainly occurs mixing, cation alternating adsorption, carbonate dissolution, sulfate reduction, and does not reach equilibrium state; (4)The maximum outflow rate of CGSD-01 can be reach to 130 m3/h, and the temperature is 100℃, which can meet the heating load of 300 thousand square meters building area.

    Conclusions 

    The high-yield new reservoir section 2 in Wumishan Formation of Jixian system was exposed for the first time in the second space of deep thermal reservoir in Tianjin area, and the thermal reservoir structure and main parameters of the reservoir were proved up, showing a good resource prospect.

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