地下流体水位观测地震前兆机理研究
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摘要
本文主要研究锦州沈家台汤池子观测站地下流体数字化水位的年、月、日动态特征及数字化资料映震性能分析。检验理论固体潮与实际观测水位的潮汐因子、相对误差,排除气压对水位观测的干扰因素,识别水位观测水动态中较大幅度的脉冲和突变、阶变、潮汐畸变,水位上升打破年变等因素,提高利用地下流体观测地震前兆的监测效能。
This paper studies Jinzhou Shenjia seismic station,Tang Chizi observatories on the ground floor of digital fluid level of the year,month,day and dynamic features of digital video shock performance analysis of the data.Testing theory and the actual tide water level observation of the tidal factor,the relative error,the air pressure rule out the possibility of interference with the water level observation,identification of water level observation in a larger dynamic pulse and mutations,change stage,tidal distortion,to break up the water level in change,and so on Factors that increase the use of underground fluid earthquake precursor observation to monitor the performance.
引文
「1」车用太,赵文忠.京津冀地区井水位的数字化观测及其地震前兆监测效能评估.地震,2006,26(4):103-112.
    「2」张昱,李春森.甘肃及邻区数字化水位观测资料的应用与地震监测效能评估.地震,2008,28(3):103-109.
    「3」张昱,钟美轿.平凉C11井地下流体数字化观测资料的分析.地震,2008,28(4):128-135.
    「4」樊星,符茂飞.海口市向荣村井水位数字化观测资料的动态曲线重叠处理方法.国际地震动态.2008(2):26-31.

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