三峡井网井水位对汶川8.0级地震的同震响应特征研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
系统分析了三峡井网8口井水位对汶川8.0级地震的同震响应及其后效特征,揭示出这些特征因井而异,其差异性在井孔结构相似的条件下主要取决于井点的构造部位、观测含水层的地下水埋藏类型、含水层的导水系数等条件;深入研究了井水位同震后效特征中残留阶升与阶降的力学含义及其地震预测意义,并用仙女山断裂带上近期地震活动验证了残留阶升区可能是未来地震危险区的科学推论.
We systematically analyzed coseismic well level response in Three Gorges well-network and its post-seismic characteristic to MS8.0 Wenchuan earthquake. The result indicates that each well has its characteristic of itself. In the condition of similar borehole configuration, the difference lies on site structure of the well, imbed type of monitoring layer, transmissivity of aquifer system. We studied mechanical mechanism of coseismic and post-seismic step-rise and step-drop, and its significance in earthquake prediction. Using recent seismic activity on the Xiannüshan fault, we has validated the scientific deduction that the remained step-rise zone may be potential zone with earthquake danger.
引文
①中国地震局地下流体学科组汶川地震总结,2008年9月.
    车用太,鱼金子,刘五洲,易立新,徐峰,李介成,孙天林.2002.三峡井网的布设与观测井建设[J].地震地质,24(3):423-433.
    车用太,刘五洲,颜萍,刘喜兰,刘成龙.2004.三峡井网地下流体动态在水库蓄水前后的变化[J].大地测量与地球动力学.24(2):14-22.
    车用太,鱼金子.2006.地震地下流体学[M].北京:地震出版社:379-386.
    付虹,刘丽芳,王世芹,万登堡.2002.地方震及近震地下水同震震后效应研究[J].地震,22(4):55-66.
    黄辅琼,迟恭财,徐桂明.2000.大陆地下流体对台湾南投7.6级地震的响应研究[J].地震,20(增刊):119-125.
    李家明,姚运生,梅建昌,张卫华.2006.DSW-01型水位仪在三峡井网中应用[J].大地测量与地球动力学,26(4):121-125.
    刘五洲,鱼金子,车用太,刘喜兰,姚运生,颜萍.2003.三峡井网地下流体动态与映震能力的初步分析[J].地震地质,25(4):632-639.
    杨竹转,邓志辉,陶京玲,谷元珠,王志敏,刘成龙.2007.北京塔院井数字化观测水温的同震效应研究[J].地震学报,29(2):203-213.
    中国地震局监测预报司.2005.地下流体对苏门答腊8.7级地震的响应特征[M].北京:地震出版社:131-258.
    Kitagawa Y,Koizumi N,Tsuskutta T.1996.Comparison of post-seismic groundwater temperature changes with earth-quake-induced volumetric strain release:Yudani hot spring,Japan[J].Geophys Res Lett,23(22):3147-3150.
    Roeloffs E A.1998.Persistent water level changes in a well near Parkfield California,due to1ocal and distant earth-quakes[J].J Geophys Res,103(B1):869-889.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心