Fault-Affected Fluid Circulation Revealed by Hydrochemistry and Isotopes in a Large-Scale Utilized Geothermal Reservoir

Kong, Yanlong; Pang, Zhonghe; Pang, Jumei; Li, Jie; Lyu, Min; Pan, Sheng

Fault-Affected Fluid Circulation Revealed by Hydrochemistry and Isotopes in a Large-Scale Utilized Geothermal Reservoir

2020

Kong, Yanlong(Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics) | Pang, Zhonghe(Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics) | Pang, Jumei(China Institute for Geo-Environmental Monitoring, Beijing 100081) | Li, Jie(College of Water Sciences, Beijing Normal University) | Lyu, Min(Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics) | Pan, Sheng(Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics)

A new significant aspect in the utilization of hydrothermal energy in China is the large-scale exploitation using multiwells from a single geothermal site. This requires detailed hydrogeochemical investigations to gain insight about deep groundwater circulation. At the Xiongxian karst geothermal site in North China, where the demonstration project of large-scale utilization was conducted, 40 boreholes with depths from 1000 to 1800 m were drilled in a region of 50 km2. A total of 25 water samples were collected, and temperature loggings were conducted in 16 of these wells. At the site scale, the hydraulic head was observed to decline from SW to NE, i.e., orthogonal to that at the regional scale. Moreover, the geothermal groundwater temperature, borehole temperature gradient, and heat flow in the caprock all exhibited the same spatial trend with the groundwater head. Based on the hydrogeochemical and temperature logging data, this was explained by mixing of lateral recharging groundwater with ascending thermal fluids through the Xiongxian Fault, after excluding the causes of pumping activities and geologic structure. In addition, geothermal groundwater 81Kr age was estimated to be approximately 760 k yr, which is much older than the 14C age of 20 to 30 k yr. The older 81Kr age implies a low renewability of deep groundwater circulation, which should be considered in terms of sustainable management in relation to the large-scale utilization of geothermal resources.

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