唐九安, 常千军, 许作禄, 朱五泉, 陈淑芬. 宕昌水管倾斜仪测量结果的动态特征研究[J]. 华北地震科学, 1994, 12(4): 47-54.
引用本文: 唐九安, 常千军, 许作禄, 朱五泉, 陈淑芬. 宕昌水管倾斜仪测量结果的动态特征研究[J]. 华北地震科学, 1994, 12(4): 47-54.
Tang Jiuan, Chang Qianjun, Xu zuolu, Zhu Wuquan, Cheng Shufen. RESEARCH ON THE DYNAMIC PERFORMANCE OF MEASURING RESULTS OF WATER TUBE TILTMETER IN DANG CHANG[J]. North China Earthquake Sciences, 1994, 12(4): 47-54.
Citation: Tang Jiuan, Chang Qianjun, Xu zuolu, Zhu Wuquan, Cheng Shufen. RESEARCH ON THE DYNAMIC PERFORMANCE OF MEASURING RESULTS OF WATER TUBE TILTMETER IN DANG CHANG[J]. North China Earthquake Sciences, 1994, 12(4): 47-54.

宕昌水管倾斜仪测量结果的动态特征研究

RESEARCH ON THE DYNAMIC PERFORMANCE OF MEASURING RESULTS OF WATER TUBE TILTMETER IN DANG CHANG

  • 摘要: 介绍了甘肃省宕昌形变台FSQ型浮于水管倾斜仪1990.7~1994.3期间的测量结果,分析了该台倾斜固体潮潮汐因子和非潮汐曲线及其残差曲线的动态特征。

     

    Abstract: In this paper the results of Dang Chang Deformation station measured by FSQ——type water tubetiltmeter during 1990.7~1994.3 was introduced. The dynamic performance of the results is analysed.The results show that the mean square error of hour's reading values is less than 1×10-3"; the monthlyvariation range of tidal factors of O1 and M2 wave is less than 6%. Among the drift curve, there are threecomponent parts, namly:long series tendency component, annual variation component and residual component. The variational speed rate of the tilt vector in the long period component is 1.5"/a, and the direction towards S11°E. After 1992, there is an obviously anomaly in the non-tide residual curve. During1993~1994 the variation speed rate of the residual vector is 0.5"/a, and the direction toward N36°E.

     

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