兰州市区地面脉动特征
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THE CHARACTERISTICS OF GROUND MICROTREMORS IN LANZHOU
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    摘要:

    为了进行兰州市区的场地小区划,在市区75个点上做了地面脉动观测。
    观测表明,地面脉动具有明显的区域性。市区不同地点的傅氏谱多少都有相似之处,多数谱峰值出现在0.3-0.45秒范围内。但是在兰州市的不同地段,谱形上也有一定的差别。根据谱形,可将市区划分为5个地区。由此可以想见,地面脉动特征取决于整个区域的综合自然条件,局部表土层的条件反居次要地位。
    地面脉动的最大幅值显然取决于表层较软土层,如黄土、亚粘土、亚砂土等的厚度,这些软土层的厚度越大,地面脉动的最大幅值也就越大。
    地面脉动观测结果可用之于场地土小区划分中去。

    Abstract:

    In order to realize microregionation of the site conditions in Lanzhou, the observation of ground microtremors was carried out in 75 points within this city.
    It is shown that the characteristics of ground microtremors are obviously regional. The Fourier spectra of different, points in Lanzhou are more or less alike with each other. The pikes of the majority of the Fourier spectra occur at 0.3-0.45 sec. But in different areas of Lanzhou there are some various characteristics in the spectra and according to the appearance of the spectra it is able to divide the whole area of this city into 5 regions. So it can be imagined that the characteristics of ground microtremors are dependent on the total natural conditions over the whole region rather than on the local subsoil conditions.
    The maximum amplitude of the ground microtremors at 9-11 in the morning is 0.5-1.5μ. The maximum amplitude of ground microtremors is obviously dependent on the thickness of the soft ground, such, as leoss, loam, silt ect.. The thicker the stratum of the soft ground, the greater the maximum amplitude of microtremors.
    The results of microtremors measurement can be used in the micro regionation of site conditions.

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孙崇绍.兰州市区地面脉动特征[J].地震工程学报,1981,3(1):61-71. Sun Chongshao. THE CHARACTERISTICS OF GROUND MICROTREMORS IN LANZHOU[J]. China Earthquake Engineering Journal,1981,3(1):61-71.

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  • 收稿日期:1980-08-10
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  • 在线发布日期: 2017-06-28