Groundwater Thermal Monitoring and Modeling

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Hydrogeology".

Deadline for manuscript submissions: 20 May 2025 | Viewed by 1242

Special Issue Editors


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Guest Editor
College of Geosciences, China University of Petroleum, Beijing, China
Interests: tectono-thermal evolution of sedimentation basins; geothermal resources
College of Water Science, Beijing Normal University, Beijing, China
Interests: isotope hydrology; groundwater-surface water interaction; groundwater dating; geothermics

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Guest Editor Assistant
College of Geosciences, China University of Petroleum, Beijing, China
Interests: geothermal engineering; geothermal reservoir modeling; reactive transport modeling

Special Issue Information

Dear Colleagues,

This Special Issue aims to explore the impact of rock thermal conductivity and paleo-geothermal field distribution on the groundwater thermal environment. We invite original research, reviews, and technical reports on topics including, but not limited to, rock thermal conductivity measurement methods, evaluation of prospects for geothermal resource exploitation, and the relationship between deep rock heat production rates and terrestrial heat flow.

We welcome submissions from experts and scholars in the fields of geology, hydrogeology, environmental science, and related disciplines to contribute to the latest advances in groundwater thermal monitoring and modeling, with a focus on geothermal resource development and environmental protection.

Prof. Chuanqing Zhu
Dr. Jie Li
Guest Editors

Dr. Yonghui Huang
Guest Editor Assistant

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Keywords

  • groundwater
  • thermal monitoring
  • modeling
  • rock thermal conductivity
  • geothermal field distribution
  • paleo-geothermal
  • environmental impact

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Published Papers (1 paper)

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Research

16 pages, 6854 KiB  
Article
Terrestrial Heat Flow and Lithospheric Thermal Structure of the Hubao Basin, North Central China
by Ziqin Gong, Wei Xu, Xiaoyin Tang, Genggeng Zhu, Yuliang Yang, Tianqi Guo and Sen Wang
Water 2024, 16(14), 1980; https://doi.org/10.3390/w16141980 - 12 Jul 2024
Viewed by 671
Abstract
The terrestrial heat flow and lithospheric thermal structure of sedimentary basins are crucial for understanding basin dynamics and assessing geothermal resources. This study computed the heat flow in the Hubao Basin using rock thermal conductivity and borehole temperature data. Combined with the geophysical [...] Read more.
The terrestrial heat flow and lithospheric thermal structure of sedimentary basins are crucial for understanding basin dynamics and assessing geothermal resources. This study computed the heat flow in the Hubao Basin using rock thermal conductivity and borehole temperature data. Combined with the geophysical profile of the Yinshan Orogenic Belt–Hubao Basin–Ordos Basin, the lithospheric thermal structure was studied, and the geodynamic mechanism is discussed. The results indicate that the heat flow in the Hubao Basin ranges from 64.0 to 73.8 mW/m2. The Moho temperature along the profile varies between 570 and 652 °C, and the thickness of the thermal lithosphere ranges from 122.7 to 138.8 km. Using the backstripping method to calculate the crust–mantle heat flow ratio, we find that this ratio in in the Hubao Basin is approximately 1, indicating a “warm crust, warm mantle” type of lithospheric thermal structure. This is related to the combined effects of extensional tectonics since the Late Jurassic and Early Cretaceous, westward subduction of the Pacific Plate, remote effects from the Indian Ocean Plate, and the development of deep-seated faults within the basin. The combined effects of lithospheric thinning and deep-seated faults have resulted in thermal anomalies in the Hubao Basin. Full article
(This article belongs to the Special Issue Groundwater Thermal Monitoring and Modeling)
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