Geothermal Power Generation Potential in the Eastern Linqing Depression
China has been the leading country worldwide in direct geothermal utilization for a rather long time, which has contributed significantly to reducing carbon emissions. But the installed capacity of geothermal power generation in China is very small, and there are only a few geothermal power plants i...
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Published in | Acta geologica Sinica (Beijing) Vol. 95; no. 6; pp. 1870 - 1881 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
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01.12.2021
Shandong Provincial Research Center of Groundwater Conservation and Restoration,Jinan 250013,China%Shandong Provincial Research Center of Geothermal Resources and Reinjection,Dezhou,Shandong 253072,China Shandong Provincial Bureau of Geology and Mineral Resources (SPBGM),Jinan 250013,China The Second Institute of Hydrogeology and Engineering Geology,SPBGM,Dezhou,Shangdong 253072,China%Shandong Provincial Research Center of Groundwater Conservation and Restoration,Jinan 250013,China 5801 Institute of Hydrogeology and Engineering Geology,SPBGM,Jinan 250014,China Shandong Provincial Research Center of Geothermal Resources and Reinjection,Dezhou,Shandong 253072,China |
Edition | English ed. |
Subjects | |
Online Access | Get full text |
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Summary: | China has been the leading country worldwide in direct geothermal utilization for a rather long time, which has contributed significantly to reducing carbon emissions. But the installed capacity of geothermal power generation in China is very small, and there are only a few geothermal power plants in China, specifically in Tibet, including the well‐known Yangbajing geothermal power plant. Therefore, it is anticipated that more high‐temperature geothermal resources will be discovered in order to promote China's power generation. There is potential for high‐enthalpy geothermal in the Eastern Linqing Depression in Shandong Province, where geothermal energy is stored in Ordovician and Cambrian carbonate strata. Based on the geothermal gradient in Cenozoic strata and the depth of the target geothermal reservoir, the temperature distribution pattern of the reservoir was analyzed, and two “sweet points” were identified in the Yucheng geothermal field and the Guanxian geothermal field, where the reservoir temperature is predicted to be higher than 200°C at a depth of less than 8000 m. Due to the low karst fissure ratio and the insufficient geothermal fluid in the geothermal reservoir, it is recommended that an enhanced geothermal system be set up, to increase the permeability of the natural fracture system in the carbonate formations and provide sufficient fluid for power generation through reinjection of used geothermal fluid. The power generation capacity of the two geothermal fields was estimated using a volumetric method, revealing a power generation capacity of 1621.02 MWe for the Yucheng geothermal field, and 1287.19 MWe for the Guanxian geothermal field. |
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Bibliography: | ZHAO Jichu, male, born in 1975 in Shaodong county, Hunan province. He obtained his Master degree in geological engineering from China University of Geosciences (Beijing), He is a senior geologist in geothermal, groundwater and environmental geology. His research mainly focuses on geothermal geology survey and geothermal energy utilization. E‐mail About the first and corresponding author About the corresponding author kangfengxin@126.com KANG Fengxin, male, born in 1968 in Zhaoyuan city, Shandong Province. He obtained his Ph.D. in hydrogeology from China University of Geosciences (Wuhan). He is a professor of hydrogeology and geothermal energy at SPBGM. His research involves groundwater resources and geothermal energy. E‐mail . 597943119@qq.com |
ISSN: | 1000-9515 1755-6724 |
DOI: | 10.1111/1755-6724.14877 |