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会昌地震台相同测点倾斜固体潮观测之对比分析
引用本文:赵爱平,李传江,周红艳,吴敏.会昌地震台相同测点倾斜固体潮观测之对比分析[J].华南地震,2012(2):121-132.
作者姓名:赵爱平  李传江  周红艳  吴敏
作者单位:江西省地震局
基金项目:江西省地震局2009~2010年度“新世纪优秀人才”基金专项;2010年度中国地震局三结合课题“相同测点不同仪器的地倾斜观测之对比研究”
摘    要:通过对会昌地震台2007-07~2011-06相同测点倾斜固体潮资料的对比分析,可以看出垂直摆资料质量稍优于水管仪资料,两种资料存在着一定的可比性。其主要的相同之处表现在于年变趋势动态、日变形态和降雨、强远震波动、潮汐因子的时间同步性上;而NS向线性倾变、潮汐因子定量化和高频信号频谱等方面存在一定差异。这种差异主要可能为观测山洞的环境条件和仪器工作特性的不同。为改善地倾斜资料高频信息记录能力,建议提高仪器采样率和改进仪器频率响应设计。

关 键 词:会昌地震台  倾斜固体潮  相同测点  潮汐因子  趋势分析  同震形变波

Contrastive Analysis on the Earth’s Tidal Tilt from the Same Observation Point in Huichang Seismic Station
ZHAO Aiping,LI Chuanjiang,ZHOU Hongyan,WU Min.Contrastive Analysis on the Earth’s Tidal Tilt from the Same Observation Point in Huichang Seismic Station[J].South China Journal of Seismology,2012(2):121-132.
Authors:ZHAO Aiping  LI Chuanjiang  ZHOU Hongyan  WU Min
Institution:(Earthquake Administration of Jiangxi Province,Nanchang 330039,China)
Abstract:Through contrastive analysis on the Earth’s tidal tilt data from Jul.2007 to Jun.2011 between DSQ water pipe and VS Vertical pendulum tiltometers in Huichang Seismic Station,the paper concludes that the quality of the vertical pendulum data is slightly superior to that of the water pipe data,in view of certain comparability between the two.The two said data are similar in the annual variation trend,daily variation form,as well as the time synchronization of the rainfall,wave motion of strong and distant earthquakes and the tidal factors,but are different in terms of NS-oriented linear tilt change,quantification of tidal factors and frequency spectrum of high frequency signals.These differences are probably caused mainly by different environmental conditions of the observation cave and performance characteristics of the instruments.As a result,it is suggested to improve the sampling rate and frequency response design of the observation instruments,so as to improve our capability to record high frequency information for the ground tilt data.
Keywords:Huichang Seismic Station  Earth’s Tidal Tilt  the Same Observation Point  Tidal Factor  Trend Analysis  Coseismic Deformation Wave
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