摘要
本文根据深井记录的水位固体潮和水震波资料,分析了深井积分含水层岩石体应变的作用,研究了深井积分含水层岩石体应变的机理,指出深井仅能积分井孔周圈一定范围内含水层岩石的体应变量.并且,讨论了深井积分含水层岩石体应变的主要控制因素.
Based on the records of water level changes caused by earth tides and seismic waves observed in deep wells, this paper has analyzed the uses of the volumetric strain of aquifer integrated by a deep well and studied its mechanism. It is concluded that the deep well can only integrate the volumetric strain of aquifer within the limited area around the well. In addition, the major factors influencing the volumetric strain of aquifer integrated by a deep well have been discussed.
出处
《地震学刊》
CSCD
1991年第3期59-64,共6页
Journal of Seismology
