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Wave Dispersion Studies In Granular Media By Analytical And Analytical-numerical Methods

机译:解析和数值分析方法研究颗粒状介质中的波频散

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The phenomenon of wave dispersion in dry sand is studied both by purely analytical studies and by analytical-numerical experiments on the basis of gradient elastic and viscoelastic material models. These material models are employed in order to simulate the microstructural characteristics of dry sand. The analytical studies treat the material body as a one-dimensional (for the viscoelastic case) and three-dimensional (for the gradient elastic case) and for both material models provide explicit expressions for the velocity of propagation of harmonic compressional (P) and shear (S) waves. These velocities are found to be functions of frequency, i.e., dispersive. The analytical-numerical studies treat the material as a one-dimensional one and try to simulate P and S wave propagation along the axial direction of cylindrical dry sand specimens. Thus, a sinusoidal pulse with a specific frequency is applied at one end of the specimen and the response is determined at some other point by solving a transient dynamic boundary value problem with the aid of a numerical Laplace transform. This analytical-numerical experiment is repeated for various frequencies. Thus, one determines the velocities of P and S waves as functions of frequency, thereby proving again that wave propagation in dry sand is dispersive.
机译:在纯粹的解析研究和基于梯度弹性和粘弹性材料模型的解析数值实验的基础上,研究了干砂中的波分散现象。使用这些材料模型来模拟干砂的微观结构特征。分析研究将材料主体视为一维(对于粘弹性情况)和三维(对于梯度弹性情况),并且两种材料模型都为谐波压缩(P)和剪切的传播速度提供了明确的表达式。 (S)波。发现这些速度是频率的函数,即色散。解析数值研究将材料视为一维材料,并试图模拟P和S波沿圆柱状干砂样品轴向的传播。因此,在样品的一端施加具有特定频率的正弦脉冲,并通过数值拉普拉斯变换来解决瞬态动态边界值问题,从而在另一点确定响应。针对各种频率重复进行此分析数值实验。因此,人们可以将P波和S波的速度确定为频率的函数,从而再次证明波在干沙中的传播是分散的。

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