汤池一号井水震波与地震波的对比分析

英文篇名：Comparative research between water shock wave and seismic wave in Tangchi No.1 well
中文刊名：地震地磁观测与研究
英文刊名：Seismological and Geomagnetic Observation and Research
作者：于磊 ; 戚浩 ; 朱方保 ; 汪世仙 ; 赵桂宝
英文作者：Yu Lei~(1)) ; Qi Hao~(2)) ; Zhu Fangbao~(3)) ; Wang Shixian~(3))and Zhao Guibao~(1)) 1)Jiashan Seismic Station ; Anhui Province 239461 ; China 2)Earthquake Administration of Anhui Province ; Heifei 230031 ; China 3)Lujiang Seismic Station ; Anhui Province 231511 ; China
中文关键词：水位 ; 地震波 ; 波形
英文关键词：water lever ; seismic wave recordings ; waveform
出版日期：2011-02-25
机构：嘉山地震台;安徽省地震局;庐江地震台;
年：2011
期：01
出版单位：地震地磁观测与研究

摘要

水震波是地震波引起的井孔水位的振荡现象。利用同一地质单元内的水震波与地震面波资料进行对比研究,分析出水震波与地震波数据上的异同,同时运用地震波与水震波的数据异同,探求两者数据在应用方面的联系,以更好理解两者的对比关系,本课题估算出水位对含水层应力应变的响应"格值",通过对庐江地震台等井的井水位观测资料分析,结合白山数字化地震波信号,估算"格值"为2.443×10~(-12)/cm,即汤池一号井观测含水层垂直应变量为2.443×10~(12)/cm时,井水位变化1 cm,在计算过程中加深对比关系的理解。
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.

引文

刘澜波,郑香嫒,彭贵荣,等.地震波引起洼里井水位震荡的初步分析[J].地震,1983,5:12-19．
    舒优良,张世民,等.周至深井水震波数字化记录与地震波记录的对比研究[J].地震地磁观测与研究,2003,24(5) :26-31
    汪成民,车用太,万迪堑,等.地下水微动态研究[J].北京:地震出版社,1988．
    张昭栋,王尤培,郑金涵,等.井孔变径与水井含水层系统对地震波的响应[J].华北地震科学,1992,10(3) :66-74．
    张子广,万迪堃,董守玉,等.水震波与地震面波的对比研究及其应用[J].地震,1998,18(4) :399-404．