1D harmonic response of layered inhomogeneous soil: Analytical investigation

被引:63
作者
Rovithis, E. N. [2 ]
Parashakis, H. [3 ]
Mylonakis, G. E. [1 ]
机构
[1] Univ Patras, Dept Civil Engn, Patras 26500, Greece
[2] Inst Engn Seismol & Earthquake Engn ITSAK, Thessaloniki 55102, Greece
[3] Technol Educ Inst Crete, Dept Civil Works, Iraklion, Greece
关键词
ELASTIC-WAVES; MEDIA;
D O I
10.1016/j.soildyn.2011.01.007
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The seismic response of inhomogeneous soil deposits is explored analytically by means of one-dimensional viscoelastic wave propagation theory. The problem under investigation comprises of a continuously inhomogeneous stratum over a homogeneous layer of higher stiffness, with the excitation defined in terms of vertically propagating harmonic S waves imposed at the base of the system. A generalized parabolic function is employed to describe the variable shear wave propagation velocity in the inhomogeneous layer. The problem is treated analytically leading to an exact solution of the Bessel type for the natural frequencies, mode shapes and base-to-surface response transfer function. The model is validated using available theoretical solutions and finite-element analyses. Results are presented in the form of normalized graphs demonstrating the effect of salient model parameters such as layer thickness, impedance contrast between surface and base layer, rate of inhomogeneity and hysteretic damping ratio. Equivalent homogeneous soil approximations are examined. The effect of vanishing shear wave propagation velocity near soil surface on shear strains and displacements is explored by asymptotic analyses. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:879 / 890
页数:12
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