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引用本文:刘序俨,李军,郑小菁,王林.???????λ?????????????????[J].大地测量与地球动力学,2009,29(3):28-33.
作者姓名:刘序俨  李军  郑小菁  王林
作者单位:福建省地震局,福州,350003
基金项目:中国地震局老专家科研基金 
摘    要:???λ????????????????????????????????峱????????????????????λ???????????????????λ??????????·?????????????????????????????????M2???????????????λ?????????????????????????????????????????λ?????????????Ms8.0????????????????????????????沨??????????沨???????????λ????????????????????λ??????????????????????????????????????????????????????沨?????????????????λ???????????1??????????

关 键 词:???λ  ?????沨  ???  ???  ?????  

RESPONSE OF WELL LEVEL TO CRUST BODY STRAIN CAUSED BY WENCHUAN M s8.0 EARTHQUAKE
Liu Xuyan,Li Jun,Zheng Xiaojing,Wang Lin.RESPONSE OF WELL LEVEL TO CRUST BODY STRAIN CAUSED BY WENCHUAN M s8.0 EARTHQUAKE[J].Journal of Geodesy and Geodynamics,2009,29(3):28-33.
Authors:Liu Xuyan  Li Jun  Zheng Xiaojing  Wang Lin
Institution:Earthquake Administration of Fujian;Fuzhou 350003
Abstract:The well water level system is a natural body strain gauge. Taking the theoretical earth tide value of body strain as the input of the system and digital observations of well level of the system as the output, the harmonic analysis results of the digital observation of well level computed with Venidikov’s harmonic analysis method is transfer function(sensitivity) of the well level system. The paper takes the amplitude factor of wave M2 as the theoretical calibration value η of well level system.The water level shock wave excited by Wenchuan s8.0 earthquake is calculated by use of the minute values of water level of five wells in May,2008. Meanwhile, the Rayleigh wave data including the maximum amplitude of radial and vertical displacement and its periods,are recorded by seismograph.Body strain wave excited by Wenchuan earthquake is calculated with displacement divergence formula. The result is the volume strain from seismograph which is high frequency is ten times bigger than the one from well water level system which is low frequency.The difference between them is discussed at last.
Keywords:well level  surface waves  theoretical calibration value  water-level shock wave  volume strain wave  
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