HYDROCHEMICAL CHARACTERISTICS OF GUANTAO GEOTHERMAL RESERVOIR IN EASTERN JIYUAN-KAIFENG SAG: Implication for Its Formation

ZHANG Meng; QIN Xiang-xi; HUANG Wen; SHI Lei; ZHENG Gang

doi:10.13686/j.cnki.dzyzy.2024.01.013

2024 Vol. 33, No. 1

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Article navigation > Geology and Resources > 2024 > 33(1): 106-114

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ZHANG Meng, QIN Xiang-xi, HUANG Wen, SHI Lei, ZHENG Gang. HYDROCHEMICAL CHARACTERISTICS OF GUANTAO GEOTHERMAL RESERVOIR IN EASTERN JIYUAN-KAIFENG SAG: Implication for Its Formation[J]. Geology and Resources, 2024, 33(1): 106-114. doi: 10.13686/j.cnki.dzyzy.2024.01.013

Citation:

ZHANG Meng, QIN Xiang-xi, HUANG Wen, SHI Lei, ZHENG Gang. HYDROCHEMICAL CHARACTERISTICS OF GUANTAO GEOTHERMAL RESERVOIR IN EASTERN JIYUAN-KAIFENG SAG: Implication for Its Formation[J]. Geology and Resources, 2024, 33(1): 106-114. doi: 10.13686/j.cnki.dzyzy.2024.01.013

HYDROCHEMICAL CHARACTERISTICS OF GUANTAO GEOTHERMAL RESERVOIR IN EASTERN JIYUAN-KAIFENG SAG: Implication for Its Formation

1.
Zhejiang Loopmaster Energy Science & Technology Co., Ltd., Hangzhou 310051, China
2.
Donghua University, Shanghai 201620, China
3.
Lily Group Co., Ltd., Hangzhou 311228, China
4.
Zhejiang Land Consolidation and Rehabilitation Center, Hangzhou 310012, China
5.
Cangzhou Loopmaste New Energy Science &Technology Co., Ltd., Cangzhou 061000, Hebei Province, China

Received Date: 24 November 2022

Revised Date: 11 January 2023

Publish Date: 25 February 2024

Abstract

Abstract

The analysis of geothermal water of Guantao Formation in eastern Jiyuan-Kaifeng sag shows that the geothermal water is hydrochemically neutral water, salt water and extra-hard water, mainly Cl-Na type, and its chemical characteristics, controlling factors and characteristic coefficients are significantly different from those in upper Minghuazhen Formation, Quaternary groundwater and surface water. The geothermal water in Guantao Formation is sedimentary type of lixiviation water in continental salt rock strata, occurred in sandstone pores, with regional faults and fissures as channels for heat conduction and migration, and terrestrial heat flow for heat conduction and warming, accompanied by constant lixiviation, evaporation and concentration. On the other hand, due to the well sealed geothermal reservoir, the migration of geothermal water is much stagnant, which contribute to the complete reducibility and higher concentration degree of geothermal water. Compared with Kaifeng-Lankao fault depression, the geothermal water in Guantao Formation of Kaifeng fault uplift shows higher degree of reducibility and concentration.
- geothermal resources /
- Guantao Formation /
- hydrochemistry /
- groundwater /
- geothermal reservoir /
- Jiyuan-Kaifeng sag /
- Henan Province

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References

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