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Bulletin of Chinese Academy of Sciences (Chinese Version)

Authors

Pang Zhonghe, Geothermal Resources Research Center, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China; Department of Hydrogeology and Geothermal Resources, College of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
Kong Yanlong, Geothermal Resources Research Center, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China; Department of Hydrogeology and Geothermal Resources, College of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
Pang Jumei, Geothermal Resources Research Center, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China
Hu Shengbiao, Geothermal Resources Research Center, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China; Department of Hydrogeology and Geothermal Resources, College of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
Wang Jiyang, Geothermal Resources Research Center, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China; Department of Hydrogeology and Geothermal Resources, College of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

Keywords

Xiongan New Area; large scale karstic geothermal reservoirs; geothermal district heating; large scale geothermal use; reinjection technology; geothermal tracing; monitoring of geothermal reservoirs

Document Type

Article

Abstract

Xiongan New Area is rich in geothermal resources, which may play a key role in the construction of ecological civilization. The shallow geothermal energy ( < 200 m), and deep geothermal energy stored in sandstone and karstic reservoirs are rich and suitable for exploition and utilization. The deep carbonate geothermal resources is particularly large and easy to be exploited. Geothermal resource stored in super deep layer (>3000 m) is also of good potential. The Xiongxian City located in the Xiongan New Area, has pioneered in the large-scale district heating using karstic geothermal resources, which is the largest single project in the world that has a total geothermal heating capacity of 4.5×10 6 m 2. The author believes that the exploration of geothermal resources in the future should be enhanced, especially in super-deep geothermal resource exploration. On the use of geothermal energy, we should make full use of the shallow geothermal energy, adjust measures to local conditions, and make rational allocation of shallow and deep geothermal resources. In addition, we should also pay attention to environmental protection, and coordinate the relationship between geothermal resources and other energy. At the same time, we should widely apply the technique taking advantage of storage function of geothermal reservoirs, and gradually construct the new development pattern of clean energy that geothermal energy is used as main body and others are complementary energy.

First page

1224

Last Page

1230

Language

Chinese

Publisher

Bulletin of Chinese Academy of Sciences

References

庞忠和, 胡圣标, 汪集暘.中国地热能发展路线图.科技导报, 2012, 30(32):18-24.

陈墨香.华北地热.北京:科学出版社, 1988.

陈墨香, 黄歌山, 张文仁, 等.冀中牛驼镇凸起地温场的特点及地下热水的开发利用.地质科学, 1982, (3):239-252.

陈墨香, 汪集暘, 王缉安, 等.华北断陷盆地地热场特征及其形成机制.地质学报, 1990, 64(1):80-90.

王贵玲. 地热能助力雄安新区生态城市建设. 海利丰2017第九届中国国际地源热泵行业高层论坛. [2017-10-26]. http://www.dyrbw.com/news/show.php?itemid=73404.

Duan Z F, Pang Z H, Wang X Y. Sustainability evaluation of limestone geothermal reservoirs with extended production histories in Beijing and Tianjin, China. Geothermics, 2011, 40(2):125-135.

Pang Z H, Pang J M, Kong Y L, et al. Large karstic geothermal reservoirs in sedimentary basins in China:Genesis, energy potential and optimal exploitation//Proceedings of the World Geothermal Congress 2015. Melbourne, 2015. https://pangea.stanford.edu/ERE/db/WGC/papers/WGC/2015/32010.pdf.

Yang F T, Liu S L, Liu J X, et al. Combined monte carlo simulation and geological modeling for geothermal resource assessment:a case study of the Xiongxian geothermal field, China//Proceedings of the World Geothermal Congress 2015. Melbourne, 2015. https://pangea.stanford.edu/ERE/db/WGC/papers/WGC/2015/16040.pdf.

庞忠和, 胡圣标, 王社教, 等. 地热系统与地热资源. 见: 汪集暘, 等. 地热学及其应用. 北京: 科学出版社, 2015: 257-372.

Kong Y L, Pang Z H, Pang J M, et al. Stable isotopes of deep groundwater in the Xiongxian geothermal field. Procedia Earth & Planetary Science, 2017, 17:512-515.

Kong Y L, Pang Z H, Pang J M, et al. Deep groundwater cycle in Xiongxian geothermal field//Proceedings of the World Geothermal Congress 2015. Melbourne, 2015. https://pangea.stanford.edu/ERE/db/WGC/papers/WGC/2015/15045.pdf.

Kong Y L, Pang Z H, Shao H B, et al. Recent studies on hydrothermal systems in China:a review. Geothermal Energy, 2014, 2(1):19.

Wang S F, Pang Z H, Liu J R, et al. Origin and evolution characteristics of geothermal water in the Niutuozhen geothermal field, North China Plain. Journal of Earth Science, 2013, 24(6):891-902.

王树芳.水热过程示踪与模拟及地热资源优化开采-以华北牛驼镇地热田为例.北京:中国科学院地质与地球物理研究所, 2011.

庞菊梅, 庞忠和, 孔彦龙, 等.岩溶热储井间连通性的示踪研究.地质科学, 2014, 49(3):915-923.

Pang J M. Reinjection into well ST0902 and tracer testing in the Xiongxian geothermal field, Hebei Province, China//Reports 2010 of geothermal training programme, United Nations University. Reykjavik, 2010:493-524. http://os.is/gogn/unu-gtp-report/UNUGTP-2010-25.pdf.

Kong Y L, Pang Z H, Shao H B, et al. Optimization of welldoublet placement in geothermal reservoirs using numerical simulation and economic analysis. Environmental Earth Sciences, 2017, 76(3):118.

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