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Study on the relationship between geothermal exploitation and seismic activity in Xi'an region
作者姓名:吴富春  宋立胜  朱兴国  王锋  景北科  董星宏  方炜  左永青
作者单位:WU Fu-chun1) SONG Li-sheng2) ZHU Xing-guo3) WANG Feng1) JING Bei-ke1) DONG Xing-hong1) FANG Wei1) ZUO Yong-qing2) 1) Seismological Bureau of Shaanxi Province,Xi(an 710068,China 2) The Landslide Office of Shaanxi Province,Xi(an 710068,China
基金项目:Project sponsored by the Landslide Office of Shaanxi Province,Society of Disaster Reduction of Shaanxi Province.
摘    要:IntroductionGeothermal energy is a new and clear energy resource. It is very useful in heating and generating electricity and medical treating. The Assembly of International Environmental Protection in 1992 predicted that the usage and development of geothermal energy would exceed the traditional energy such as oil and coal, and its developmental prospect will be very bright.There are great geothermal resources in Weihe basin. The average value of heat flow in Weihe basin is 7.88(10(2 W/m2…


Study on the relationship between geothermal exploitation and seismic activity in Xi'an region
WU Fu-chun SONG Li-sheng ZHU Xing-guo WANG Feng JING Bei-ke DONG Xing-hong FANG Wei ZUO Yong-qing Seismological Bureau of Shaanxi Province,Xi.Study on the relationship between geothermal exploitation and seismic activity in Xi''''an region[J].Acta Seismologica Sinica(English Edition),2001(4).
Authors:WU Fu-chun SONG Li-sheng ZHU Xing-guo WANG Feng JING Bei-ke DONG Xing-hong FANG Wei ZUO Yong-qing Seismological Bureau of Shaanxi Province  Xi
Institution:WU Fu-chun1) SONG Li-sheng2) ZHU Xing-guo3) WANG Feng1) JING Bei-ke1) DONG Xing-hong1) FANG Wei1) ZUO Yong-qing2) 1) Seismological Bureau of Shaanxi Province,Xi
Abstract:Based on the analysis of the induced earthquakes in China and abroad, we get some ideas about earthquakes induced by pumping water out of a well or injecting water into a well. The induced earthquakes usually occur near the well, and they are generally small earthquakes. The earthquake sources are shallow, and they belong to the main shock-after shock type of earthquake or the swarm-type of earthquake. The magnitude and the quantity of the induced earthquakes obviously depend on the pressure and the quantity of water pumped or injected. These earthquakes happen as soon as pumping or injecting occurrence, or after ten or twenty days, they may occur at the time of injecting mud or injecting high pressure water when a well is being drilled, or at the time when the ground water is being normally exploited. A large quantity of hot water has been exploited since 1990 in Xi(an, and the quantity of water exploited has been increasing year by year, as a result the groundwater level has been dropping with the water pumped out and the water level is high in summer and low in winter. The earthquakes in Xi(an region belong to the solitary-type and they spread outside Xi(an city where the wells are concentrated but no earthquake happens. The seismic frequency and the energy released have no relation with the quantity of water exploitation or the water level in the well. It is considered that geothermal exploitation does not induce earthquakes in and around Xi(an because of its specially geological condition.
Keywords:geothermal exploitation  induced earthquakes  relationship
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