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首页> 外文期刊>International Journal for Numerical and Analytical Methods in Geomechanics >The influence of the depth of the ground water table on free field road traffic-induced vibrations
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The influence of the depth of the ground water table on free field road traffic-induced vibrations

机译:地下水位深度对自由场道路交通诱发的振动的影响

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This paper describes the influence of seasonal variations of the ground water table on free field traffic-induced vibrations. The passage of a truck on two types of road unevenness is considered: a joint in a road pavement consisting of concrete plates and a speed bump with a sinusoidal profile. Free field vibrations are computed with a two-step solution procedure, where the computation of the vehicle axle loads is decoupled from the solution of the road-soil interaction problem. The impedance of the soil is calculated using a boundary element method, based on the Green's functions for a dry layer on top of a saturated half-space. It is demonstrated that, in the low-frequency range of interest, wave propagation in the saturated half-space can be modelled with an equivalent single phase medium as an alternative to Biot's poroelastic theory for saturated porous media. The relation between the free field velocity and the depth of the ground water table is dominated by three phenomena: (1) the compressibility of the soil decreases due to the presence of the pore water. (2) the ground water table introduces a layering of the soil which may cause resonance of the dry layer and (3) refracted P-waves in the dry layer interfere with surface waves. If the depth of the ground water table is large with respect to the wavelength of the vibrations in the soil, the response tends to the response of a dry half-space. The average free field velocity is equal to the velocity in the absence of ground water. If the depth of the ground water table is small with respect to the wavelength of the vibrations in the soil, the response tends to the response of a saturated half-space and resonance of the dry layer does not occur. The average free field velocity is smaller than the velocity in the absence of ground water. The interference of refracted P-waves and surface waves causes an additional oscillation of the response as a function of the excitation frequency and the distance between the road and the receiver.
机译:本文描述了地下水位的季节性变化对自由场交通诱发的振动的影响。考虑了卡车在两种类型的道路不平坦处的通过:由混凝土板组成的道路路面中的接缝和具有正弦曲线轮廓的减速带。自由场振动通过两步求解程序进行计算,其中车轴载荷的计算与路土相互作用问题的解决方案分离。土壤的阻抗是使用边界元法基于饱和半空间顶部干燥层的格林函数使用边界元法计算的。结果表明,在感兴趣的低频范围内,可以用等效的单相介质模拟饱和半空间中的波传播,以替代Biot饱和多孔介质的多孔弹性理论。自由场速度与地下水位深度之间的关系受以下三种现象支配:(1)由于孔隙水的存在,土壤的可压缩性降低。 (2)地下水位会引起土壤分层,这可能引起干层的共振,(3)干层中的折射P波会干扰表面波。如果地下水位的深度相对于土壤中振动的波长较大,则响应趋向于干燥半空间的响应。平均自由场速度等于没有地下水时的速度。如果地下水位的深度相对于土壤中振动的波长较小,则响应趋向于饱和半空间的响应,并且不会发生干层的共振。平均自由场速度小于没有地下水时的速度。折射的P波和表面波的干扰导致响应的附加振荡,该响应随激励频率和道路与接收器之间的距离而变化。

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