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首页> 外文期刊>International journal of numerical analysis and modeling >ON THE COMPARISON OF PROPERTIES OF RAYLEIGH WAVES IN ELASTIC AND VISCOELASTIC MEDIA
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ON THE COMPARISON OF PROPERTIES OF RAYLEIGH WAVES IN ELASTIC AND VISCOELASTIC MEDIA

机译:弹性与粘弹性介质中瑞雷波特性的比较

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Dispersion properties of Rayleigh-type surface waves are widely used in environmental and engineering geophysics to image and characterize a shallow subsurface. In this paper, we numerically study the Rayleigh-type surface waves and their properties in 2D viscoelastic media. A finite difference method in a time-space domain is proposed, with an unsplit convolutional perfectly matched layer (C-PML) absorbing boundary condition. For two models that have analytical expressions of wave fields/dispersion curves, we calculate their wave fields and compare the analytical and numerical solutions to demonstrate the validity of this method. For the case where a medium has a high Poisson's ratio, say 0.49, traditional finite difference methods with a PML boundary condition are not stable when modeling Rayleigh waves but the proposed method is stable. For a laterally heterogeneous viscoelastic media model (Model 1) and a two-layer viscoelastic media model (Model 2) with a cavity, we use this method to obtain their corresponding Rayleigh waves. For several quality factors, the dispersion properties of these Rayleigh waves are analyzed. The results of Model 1 show that in a shallow subsurface, the phase velocity of a fundamental mode of the Rayleigh waves increases considerably with a quality factor Q decreasing; the phase velocity increases with Poisson's ratio increasing. The results of Model 2 indicate that the energy of higher modes of the Rayleigh waves become strong when Q decreases.
机译:瑞利型表面波的色散特性在环境和工程地球物理学中被广泛使用,以成像和表征浅层地下。在本文中,我们对二维粘弹性介质中的瑞利型表面波及其特性进行了数值研究。提出了一种时空域的有限差分方法,该方法具有吸收边界条件的未分裂卷积完美匹配层(C-PML)。对于两个具有波场/弥散曲线解析表达式的模型,我们计算了它们的波场,并比较了解析解和数值解,以证明该方法的有效性。对于泊松比较高的介质(例如0.49),在建模瑞利波时,具有PML边界条件的传统有限差分方法不稳定,但建议的方法是稳定的。对于横向异质粘弹性介质模型(模型1)和带腔的两层粘弹性介质模型(模型2),我们使用这种方法来获得它们相应的瑞利波。对于几个质量因子,分析了这些瑞利波的色散特性。模型1的结果表明,在较浅的地下,瑞利波基本模的相速度随质量因数Q的减小而显着增加。相速度随泊松比的增加而增加。模型2的结果表明,当Q减小时,瑞利波的较高模的能量变强。

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