首页> 外文会议>Coupled site and soil-structure interaction effects with application to seismic risk mitigation >ON THE INFLUENCE OF SATURATION AND FREQUENCY ON MONOCHROMATIC PLANE WAVES IN UNSATURATED SOILS
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ON THE INFLUENCE OF SATURATION AND FREQUENCY ON MONOCHROMATIC PLANE WAVES IN UNSATURATED SOILS

机译:饱和度和频率对非饱和土壤单相平面波的影响

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The propagation of sound waves in partially saturated sandstone is investigated by use of a macroscopic linear model which is based on the two-component model of Biot and on the Simple Mixture Model by Wilmanski. The considered porous medium consists of a deformable skeleton and two compressible pore fluids (water and air).rnThe wave analysis of the poroelastic model reveals the existence of four body waves: three longitudinal waves, P1, P2, P3, and one shear wave, S. The dependence of their phase velocities and attenuations on the saturation and on the frequency is studied and compared to experimental observations and the sound velocity of suspensions.
机译:利用宏观线性模型对声波在部分饱和砂岩中的传播进行了研究,该模型基于Biot的二元模型和Wilmanski的Simple Mixture模型。所考虑的多孔介质由可变形的骨架和两种可压缩的孔隙流体(水和空气)组成。多孔弹性模型的波分析表明存在四种体波:三个纵波P1,P2,P3和一个剪切波, S.研究了它们的相速度和衰减对饱和度和频率的依赖性,并将其与实验观察结果和悬架的声速进行了比较。

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