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A METHOD OF ESTIMATION OF ELASTIC PROPERTIES AND THICKNESSES OF SOIL LAYERS USING VERTICAL HARMONIC LOADING ON GROUND SURFACE AND ITS NUMERICAL VERIFICATION

机译:地面竖向竖向荷载估算土层弹性特性和厚度的方法及其数值验证

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摘要

This paper presents a new method that may achieve a more accurate and lower cost estimation of elastic properties and thicknesses of soil deposits. The kernel of the proposed method, being independent of the usually adopted assumption that only one Rayleigh wave mode is dominant, is to use the near field characteristics of all types of P-SV wave motions on the surface of elastic multi-layered half space generated by the vertical harmonic load applied on its surface. The near field wave motions are accurately simulated by the stiffness matrix method as one of more powerful numerical solutions, and then the following two physical quantities, which can be observable in the field, are used in inversion analysis: (1) the predominant frequency for which the dynamic vertical displacement on the soil surface takes a maximum value, and (2) the frequency variation of the phase velocity at a point on the soil surface near the vertical harmonic load. The phase velocity used in the proposed method is a local quantity varying with the location from the vertical load, because of using all types of waves and their modes. To demonstrate the capability and reliability of the proposed method, the numerical examples are presented by using regular and irregular soil profiles.
机译:本文提出了一种新方法,该方法可以更准确,更低成本地估算土壤沉积物的弹性和厚度。所提出方法的核心与通常采用的仅一种瑞利波模式占主导地位的假设无关,是利用所产生的弹性多层半空间表面上所有类型的P-SV波运动的近场特性。通过施加在其表面上的垂直谐波负载。作为刚度矩阵解决方案之一,通过刚度矩阵方法可以精确地模拟近场波运动,然后在反演分析中使用以下两个可以在现场观察到的物理量:(1)地震波的主要频率其中在土壤表面的动态垂直位移取最大值,(2)在垂直谐波载荷附近的土壤表面上某一点的相速度的频率变化。由于使用了所有类型的波及其波型,因此在所提方法中使用的相速度是一个局部量,该量随垂直载荷的位置而变化。为了证明所提方法的能力和可靠性,通过使用规则和不规则土壤剖面给出了数值实例。

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