雄安新区地热水化学特征及其指示意义

刘明亮; 何曈; 吴启帆; 郭清海

doi:10.3799/dqkx.2019.270

Volume 45 Issue 6

Jun. 2020

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Liu Mingliang, He Tong, Wu Qifan, Guo Qinghai, 2020. Hydrogeochemistry of Geothermal Waters from Xiongan New Area and Its Indicating Significance. Earth Science, 45(6): 2221-2231. doi: 10.3799/dqkx.2019.270

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Liu Mingliang, He Tong, Wu Qifan, Guo Qinghai, 2020. Hydrogeochemistry of Geothermal Waters from Xiongan New Area and Its Indicating Significance. Earth Science, 45(6): 2221-2231. doi: 10.3799/dqkx.2019.270

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Hydrogeochemistry of Geothermal Waters from Xiongan New Area and Its Indicating Significance

doi: 10.3799/dqkx.2019.270

Liu Mingliang^{1, 2
,
,},
He Tong²,
Wu Qifan²,
Guo Qinghai^{2, 3
,
,}

1.
College of Resources and Environment, Yangtze University, Wuhan 430100, China
2.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

Received Date: 2019-07-12
Publish Date: 2020-06-15

Abstract

Abstract

Hydrogeochemical reaserch of geothermal fluids is an effective method to understand the formation mechanism, occurrence environment and circulation process of geothermal resources. Xiongan New Area, one of the typical low-temperature geothermal systems in the North China plain, is selected as the study area. In this study it is based on the analysis of water chemistry and isotopes, and aims: (1) to discuss the geochemical origin of main components in geothermal fluids, (2) to estimate the deep reservoir temperatures of geothermal waters, (3) to figure out the heat source beneath geothermal area and its genetic mechanism. The hydrochemical evidences imply that the main components in Xiongan geothermal waters are contributed by meteoric waters input and intense fluid-rock interactions at high reservoir temperatures, and several components of Wumishan Formation geothermal waters are from the dissolution of evaporation salt formed during the diagenetic process. The Ca-Mg and quartz geothermometer are suitable for estimating the reservoir temperature of Wumishan Formation geothermal waters, while that for Guantao Formation geothermal waters, the quartz geothermometer is much more appropriate. The calculated temperatures range from 76.4 to 90.6 ℃ and 66.2 to 71.3 ℃, respectively. The geothermal anomaly beneath Xiongan is likely to result from decay of radioactive elements in a specific tectonic setting.
- hydrogeochemistry,
- geochemical origin,
- geothermometer,
- geothermal anomaly,
- Xiongan New Area

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References(51)

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Hydrogeochemistry of Geothermal Waters from Xiongan New Area and Its Indicating Significance

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