广东省龙门岩溶热储温度计算及流体演化特征

王思佳; 张敏; 黄学莲; 韩永杰; 何沛欣; 王帅; 祁士华

doi:10.3799/dqkx.2022.430

Volume 49 Issue 3

Mar. 2024

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Article Navigation > Earth Science > 2024 > 49(3): 992-1004

Wang Sijia, Zhang Min, Huang Xuelian, Han Yongjie, He Peixin, Wang Shuai, Qi Shihua, 2024. Geothermometry Calculation and Geothermal Fluid Evolution of Karst Geothermal Reservoir in Longmen County, Guangdong Province. Earth Science, 49(3): 992-1004. doi: 10.3799/dqkx.2022.430

Citation:

Wang Sijia, Zhang Min, Huang Xuelian, Han Yongjie, He Peixin, Wang Shuai, Qi Shihua, 2024. Geothermometry Calculation and Geothermal Fluid Evolution of Karst Geothermal Reservoir in Longmen County, Guangdong Province. Earth Science, 49(3): 992-1004. doi: 10.3799/dqkx.2022.430

Citation:

Wang Sijia, Zhang Min, Huang Xuelian, Han Yongjie, He Peixin, Wang Shuai, Qi Shihua, 2024. Geothermometry Calculation and Geothermal Fluid Evolution of Karst Geothermal Reservoir in Longmen County, Guangdong Province. Earth Science, 49(3): 992-1004. doi: 10.3799/dqkx.2022.430

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Geothermometry Calculation and Geothermal Fluid Evolution of Karst Geothermal Reservoir in Longmen County, Guangdong Province

doi: 10.3799/dqkx.2022.430

Wang Sijia^{1
,
,},
Zhang Min²,
Huang Xuelian³,
Han Yongjie¹,
He Peixin²,
Wang Shuai^{3, 4},
Qi Shihua^{1, 3
,
,
,}

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
2.
Nonferrous Metals Geological Bureau of Guangdong Province 935 Battalion, Huizhou 516001, China
3.
School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
4.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2022-07-22
Available Online: 2024-04-12
Publish Date: 2024-03-25

Abstract

Abstract

Karst geothermal systems hold enormous potential for geothermal exploitation. The Maxing and Gepi geothermal anomaly areas are typical geothermal fields in Longmen County, Guangdong Province. The temperature and fluid evolution of geothermal reservoir can be clarified, with the analysis of ion ratio relationship, δD and δ¹⁸O isotopes, and geothermal thermometers et.al. It is indicated that silicate minerals, carbonate minerals such as calcite dissolution, and accompanying cation exchange control the hydrochemistry evolution, thus forming slightly alkaline HCO₃-type geothermal water with lower TDS in the study area. The results suggest that atmospheric precipitation is the main recharge source. The reservoir temperature is 105.0-148.0 ℃ and 101.5-131.0 ℃ for Maxing and Gepi geothermal reservoir respectively, with a lower temperature during upwelling caused by mixing with cold water up to 44.2% and 48.5% dilution. In this case, a conceptual model for geothermal fluid evolution is proposed based on the geothermal water hydrochemistry and reservoir temperature characteristics.
- karst geothermal water,
- hydrochemistry,
- geothermal reservoir temperature,
- conceptual model,
- geothermal energy

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References(48)

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Geothermometry Calculation and Geothermal Fluid Evolution of Karst Geothermal Reservoir in Longmen County, Guangdong Province

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