测震数采仪记录的钻孔应变
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
采用测震仪数采器在昌平台站开展了高频采集实验,对原来1次/分钟采样的钻孔应变仪输出进行100次/秒采样,记录到大量丰富的信息。计算了高频采样获得的应变记录分钟值后,发现与原来的1次/分钟采样变化曲线趋势完全吻合。高频采样获得的应变地震波更加完整,细节更为清晰。通过应变地震波计算得到的震相参数,与前人所得结果一致。与十三陵地震台测震仪记录的地震波比较,二者的波谱相似,且应变地震波中还存在低频成份。
A seismometer acquisition has been used at the Changping Observing Station to gather the output of strainmeter.The original rate of the strainmeter of once per minute changed to 100 times per second for seismometer acquisition sampling.Plenty of higher frequency data are recorded and the minutely data calculated from seismometer acquisition are consistent with the original data sampled by strain acquisition.And more completed waveform are recorded through higher sampling.The seismic phase parameters calculated by strain earthquake waves of higher sampling rate are also consistent with predecessors.Spectrum of the strain earthquake waves are compared with seismic waves recorded by a seismometer at the Shisanling Seismic Station,and their trends are almost the same.Some lower frequency ingredients exist in strain waves.
引文
廖丽霞、陈昌泳、倪晓寅等,2009,不同型号仪器水位记震能力对比分析,地震研究,33(2),137~144。
    欧阳祖熙、李秉元、贾维九等,1988,一种钻井式地应力场测量系统,见:地壳构造与地壳应力文集(2),11~20,北京:地震出版社。
    舒优良、张世民,2004,周至深井水震波数字化记录与地震波记录的对比研究,地震地磁观测与研究,24(5),26~31。
    张凌空、牛安福,2009,Sacks体应变地震波的观测结果分析,大地测量与地球动力学,29(5),33~37。
    张子广、万迪堃、董守玉,1998,水震波与地震面波的对比研究及其应,地震,18(4),399~404。

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