地震地磁观测与研究2011，Vol.32Issue(1)：54-58,5.DOI:10.3969/j.issn.1003-3246.2011.01.010
汤池一号井水震波与地震波的对比分析
Comparative research between water shock wave and seismic wave in Tangchi No. 1 well
摘要
Abstract
water shock wave is the waving of borehole water level that causes by seismic wave. Comparing the data of water wave and seismic wave in the same geological unit, we can analyze the differences between water wave and seismic data. In order to get a better understanding of the relativities between them, we can also explore the application of the relativities between the data. In the study, the response to lattice-valued that water to aquifer stress-strain is estimated. Considering the observation of well water level of some wells such as in Lujiang seismic station, and digital seismic signal of Baishan, we can estimate the lattice-valued is 2. 443× 10-12/cm, that is, when observed aquifer's vertical strain of Tangchi No. 1 Well is 2. 443×10-12/cm, the change of well water level is 1 cm. In this way, we can have a deep understanding of relativities.关键词
水位/地震波/波形Key words
water lever/ seismic wave recordings/ waveform引用本文复制引用
于磊,戚浩,朱方保,汪世仙,赵桂宝..汤池一号井水震波与地震波的对比分析[J].地震地磁观测与研究,2011,32(1):54-58,5.基金项目
安微省地震局局科研合同制项目经费资助 （）
