A Comprehensive Study on the Hydrogeochemical and Isotope Characteristics and Genetic Mechanism of Geothermal Water in the Northern Jinan Region

Zongjun Gao, Mengyuan Hao, Jiutan Liu (), Qiang Li, Menghan Tan and Yiru Niu
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Zongjun Gao: College Of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
Mengyuan Hao: College Of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
Jiutan Liu: College Of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
Qiang Li: College Of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
Menghan Tan: College Of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
Yiru Niu: College Of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China

Energies, 2023, vol. 16, issue 22, 1-17

Abstract: Geothermal water (GW) resources are highly valued as clean, renewable energy sources. In this study, a comprehensive analysis of water chemistry and isotope data from 25 GW samples was conducted to gain insights into the hydrochemical characteristics and formation mechanisms of the GW in the northern Jinan region (NJR). Statistical analysis and hydrochemical methods were employed for relevant analysis. The findings reveal that the GW in the NJR exhibits high salinity, with an average total dissolved solids (TDS) concentration of 9009.00 mg/L. The major ions identified are Na + and Cl − , with mean concentrations of 2829.73 mg/L and 4425.77 mg/L, respectively, resulting in a hydrochemical type of Cl − Na. The analysis of δ 2 H and δ 18 O isotopes indicates that the GW originates from atmospheric precipitation that undergoes deep cycling and interaction with older groundwater. The composition of 3 H suggests that the GW in the NJR is a mixture of waters, while radiocarbon dating ( 14 C) suggests that the recharge of the GW may have occurred in the late Pleistocene era. The GW in the NJR is classified as partially equilibrated waters. The temperature range of geothermal reservoirs is 57.13 to 99.74 °C. The hydrochemical components primarily result from water–rock interactions, including silicate weathering, cation exchange, as well as carbonate weathering and the dissolution of halite and gypsum. Moreover, taking into account the hydrogeological conditions, hydrochemistry, and isotope analysis, a conceptual model of the geothermal reservoir in the NJR was developed. The research findings serve as a valuable reference and foundation for the development and utilization of geothermal resources in the Jinan region. These originate from the Taiyi mountains in the south or the Taihang mountains in the west, and experience deep circulation and long runoff times. This study provides a reference for the sustainable development and utilization of regional geothermal resources.

Keywords: hydrochemical characteristics; isotope composition; genetic mechanism; GW; northern Jinan region (search for similar items in EconPapers)
JEL-codes: Q Q0 Q4 Q40 Q41 Q42 Q43 Q47 Q48 Q49 (search for similar items in EconPapers)
Date: 2023
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