陈绍绪, 杜锡武. 地倾斜观测的温度干扰[J]. 华北地震科学, 1985, 3(2): 82-89.
引用本文: 陈绍绪, 杜锡武. 地倾斜观测的温度干扰[J]. 华北地震科学, 1985, 3(2): 82-89.
Chen Shaoxu, Du Xiwu. TEMPERATURE INTERFERENCE OF CRUSTAL TILT OBSERVATION[J]. North China Earthquake Sciences, 1985, 3(2): 82-89.
Citation: Chen Shaoxu, Du Xiwu. TEMPERATURE INTERFERENCE OF CRUSTAL TILT OBSERVATION[J]. North China Earthquake Sciences, 1985, 3(2): 82-89.

地倾斜观测的温度干扰

TEMPERATURE INTERFERENCE OF CRUSTAL TILT OBSERVATION

  • 摘要: 地倾斜观测的温度干扰分为太阳照射引起的热倾斜和室温变化影响两部分。木文从热膨胀的角度推导了热倾斜的计算公式。地层的热倾斜除了与地面温度变化幅度、岩石的性质,洞室的覆盖厚度有关以外,地形的坡度也是一个重要因素。但是即使地形坡度很陡的情况下,覆盖厚度达30米以后,热倾斜的年变化幅度可以保证小于0.02秒。我们以张家口台站为例,说明室温变化是山洞内倾斜仪的主要干扰。估算了短周期室温变化引起仪器本身及仪器墩的倾斜量。
    地倾斜观测的温度干扰有两种方式:一是由大气温度的变化在地层中传导的不均匀性所产生的所谓"热倾斜",二是仪器洞内室温变化对仪器或墩基的直接影响。本文试图对这两种干扰的量级作一初步探讨。

     

    Abstract: Temperature interference of crustal tilt observation may be divided into two parts, heat tilt due to the sun shine and effect of the room temperature variation.In this paper, the analytical expressions for heat tilt are derived from the heat expension principle.beat tilt in surface layer is related to the slope of geography besides the amplitude of temperature variation of the ground, physical properties of rock and thickness of hole.But when thickness exceeds 30 meters, the annual amplitude of the heat tilt must be less than 0.02 second, although the slope of the geography is big.we take Zhangjiakou station as an example to show that room temperature variation is an important interference for tiltmeter inside the hole.Tilt quantities of the tiltmeter itself and instrument pier caused by short-period room tempcrature variation are estimated.

     

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