APPLIED GEOPHYSICS
 
        首页  |  版权声明  |  期刊介绍  |  编 委 会  |  收录情况  |  期刊订阅  |  下载中心  |  联系我们  |  English
应用地球物理  2025, Vol. 22 Issue (3): 698-710    DOI: 10.1007/s11770-025-1180-5
论文 最新目录 | 下期目录 | 过刊浏览 | 高级检索 Previous Articles  |  Next Articles  
冀南冠县断凹馆陶组热储成因模式及资源评价
王旭,李威,王海敏*,张东阳,陈淑文,鲍玲玲*
1. 河北省地质矿产资源勘查开发局第一地质大队,河北 邯郸 056000;2. 河北工程大学能源与环境工程学院,河北 邯郸 056038;3. 河北省暖通空调技术创新中心,河北 邯郸056038
Genetic model and resource evaluation of the Guantao Formation thermal reservoir in the Guanxian fault depression, southern Hebei
Xu Wang, Wei Li, Hai-min Wang,*, Dong-yang Zhang, Shu-wen Chen, and Ling-ling Bao,*
1. The First Geological Brigade of Hebei Geology and Mineral Resources Exploration Bureau, Handan 056000,Hebei, China 2. School of Energy and Environmental Engineering, Hebei University of Engineering, Handan 056038, Hebei, China 3. Hebei Provincial Heating, Ventilation and Air Conditioning Technology Innovation Center, Handan 056038, Hebei, China
 全文: PDF (0 KB)   HTML ( KB)   输出: BibTeX | EndNote (RIS)      背景资料
摘要 冠县断凹中低温地热资源丰富,研究地热系统的成因模式与资源量评价是实现地热资源高效开发利用的重要基础。本文结合区域资料和以往研究成果,基于区域地质构造,论述了地热地质条件、地温场特征、水化学特征并进行了分析,构建了研究区地热系统的概念模型,开展了地热资源量评价。结果表明,冠县断凹地热资源主要为馆陶组砂岩热储,地热水井口水温多在54~60 ℃,水化学类型以Cl·SO4-Na为主。地热水的来源整体接受西部太行山的大气降水补给,经深部热传导增温后,侧向补给给热储层。冠县断凹馆陶组砂岩热储地热资源量约620.10×1016J,每年可开采地热资源量为6 782×1012J,折合标煤23.14×104t。年开采地热资源量可满足地热供暖面积1800万m2,地热资源潜力大,开发利用价值高。
服务
把本文推荐给朋友
加入我的书架
加入引用管理器
E-mail Alert
RSS
作者相关文章
关键词冠县断凹   地热系统   砂岩热储   成因模式   资源量评价     
Abstract: Medium-low temperature geothermal resources are abundant in the Guanxian fault depression. An essential foundation for the effective development and use of geothermal resources is the study of the genetic model and resource assessment of the geothermal system. This study examines the geothermal geological circumstances, hydrochemical features, and geothermal fi eld characteristics based on the regional geological structure and prior research findings. The appraisal of geothermal resources is done, and a conceptual model of the geothermal system in the research area is built. The findings indicate that the Guan xian fault depression's geothermal resources are primarily Guantao Formation sandstone heat reservoirs. The geothermal water at the wellhead has a temperature between 54°C and 60 °C, and its primary chemistry is Cl·SO4-Na. Deep thermal conduction heats the geothermal water, which is then laterally supplied to the reservoir after being largely restored by air precipitation from the western Taihang Mountains. With an annual exploitable geothermal resource of 6,782×1012 J, or 23.14×104 tons of standard coal, the Guantao Formation sandstone reservoir in the Guanxian depression has a geothermal resource of about 620.10×1016 J. An area of 18 million m2 can be heated by geothermal extraction per year, demonstrating the potential for geothermal resources and their high development and use value.
Key wordsGuanxian County Fault-Bounded Depression    geothermal system    sand geothermal reservoir    genetic model    resource evaluation   
收稿日期: 2025-01-03;
基金资助:This research was funded by the Hebei Province Natural Resources Science and Technology Project (13000024P00F2D410443X).
通讯作者: 王海敏 (dzydwhm1001@163.com);鲍玲玲 (lingling5934@163.com).     E-mail: dzydwhm1001@163.com;lingling5934@163.com
作者简介: Wang Xu, a senior engineer, is currently working at the No.1 Geological Brigade of Hebei Bureau of Geology and Mineral Exploration and Development. He is mainly engaged in the research of geothermal development and utilization.
引用本文:   
. 冀南冠县断凹馆陶组热储成因模式及资源评价[J]. 应用地球物理, 2025, 22(3): 698-710.
. Genetic model and resource evaluation of the Guantao Formation thermal reservoir in the Guanxian fault depression, southern Hebei[J]. APPLIED GEOPHYSICS, 2025, 22(3): 698-710.
 
没有本文参考文献
[1] 范振宇,熊盛青,于长春,张贵宾,张心勇,胡斌. 中国东北寒区沉积型盆地地热系统与地热分布特征*[J]. 应用地球物理, 2020, 17(3): 321-337.
版权所有 © 2011 应用地球物理
技术支持 北京玛格泰克科技发展有限公司