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西安市地热水开采与地面沉降、地裂缝关系的分析
引用本文:吴富春,方炜,宋立胜,王锋,朱兴国,景北科,董星宏,左永青.西安市地热水开采与地面沉降、地裂缝关系的分析[J].地震地质,2002,24(2):234-240.
作者姓名:吴富春  方炜  宋立胜  王锋  朱兴国  景北科  董星宏  左永青
作者单位:1. 陕西省地震局,西安,710068
2. 陕西省滑坡办公室,西安,710068
3. 西安市矿产资源管理办公室,西安,710063
摘    要:西安市地面沉降和地裂缝在空间分布上有明显的一致性 ,它们的发展过程和强度变化在时间上也有明显的同步性。诱发地面沉降的主因是过量开采承压水导致承压水位下降 ,含水层介质的孔隙压力减小 ,黏性土层释水压密导致地面永久性的沉降 ,而且浅层的释水压密量大于深层 ;不均匀的地面沉降又诱发了地裂缝。无论是地热井水位或热水开采量的变化 ,还是分层沉降量的观测资料都表明 ,目前西安市深层热水开采还没有加剧西安市的地面沉降和地裂缝活动。控制并减少承压水的开采量 ,是减弱西安市地面沉降和地裂缝活动的最有效的方法

关 键 词:热水  承压水  开采  地面沉降  地裂缝
文章编号:0253-4967(2002)02-0234-07
修稿时间:2001年3月11日

ANALYSIS OF THE RELATIONSHIP AMONG GEOTHERMAL WATER EXPLOITATION, GROUND SUBSIDENCE AND GROUND FISSURES IN XI AN CITY, CHINA
WU Fu chun FANG Wei SONG Li sheng WANG Feng ZHU Xing guo JING Bei ke DONG Xing hong ZUO Yong qing Seismological Bureau of Shaanxi Province,Xi'an ,China Offic.ANALYSIS OF THE RELATIONSHIP AMONG GEOTHERMAL WATER EXPLOITATION, GROUND SUBSIDENCE AND GROUND FISSURES IN XI AN CITY, CHINA[J].Seismology and Geology,2002,24(2):234-240.
Authors:WU Fu chun FANG Wei SONG Li sheng WANG Feng ZHU Xing guo JING Bei ke DONG Xing hong ZUO Yong qing Seismological Bureau of Shaanxi Province  Xi'an  China Offic
Institution:WU Fu chun 1) FANG Wei 1) SONG Li sheng 2) WANG Feng 1) ZHU Xing guo 3) JING Bei ke 1) DONG Xing hong 1) ZUO Yong qing 2) 1)Seismological Bureau of Shaanxi Province,Xi'an 710068,China 2) Offic
Abstract:Xi an region is a geothermal anomaly zone. The geothermal exploitation in this region began in 1990, and has sped up since 1993. At present, there are 120 geothermal water wells with a depth of greater than 1 000m in this region, and this number is still increasing at a rate of 5 to 10 wells per year. Ground subsidence and ground fissures are two natural calamities peculiar to Xi an City. They are famous for long standing formation time, a vast involved range and causing the serious damage of a great numbe
Keywords:Geothermal water exploitation  Confined water  Ground subsidence  Ground fissures  
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