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Numerical Modeling of Wave Equations Derived from the Generalized Continuum Mechanics Theory

机译:广义连续介质力学理论导之波动方程的数值模拟

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A trend in the development of geophysics is to seek wave theory closer to the physical reality and derive corresponding wave equations to achieve highly accurate forward modeling, imaging, and inversion of complex structures. The generalized continuum mechanics (GCM) theory enriches the context of the conventional continuum mechanics theory by introducing the additional characteristic length scale parameters to represent the microstructural properties of the medium, and the asymmetric elastic wave equations derived from GCM theory can handle the influence of heterogeneity of a medium caused by the microstructural interactions on the propagation of seismic waves. To date, there are few studies on the numerical and analytical solutions of the elastic wave equations derived from the GCM theory, especially in the frequency band of seismic exploration. In addition, there are few studies in the existing literature that incorporate multiple theories and methods of the GCM theory into an integrated frame. In this paper, we introduce the concept of the multi-scale microstructural interactions and construct the quantitative relationship between the characteristic length scale parameter of the medium and the characteristic length scale parameter of the micro-pore reflecting the micro-pore structures, and then integrate the modified couple stress theory and the one-parameter second strain gradient theory into a unified framework for numerical modeling and analysis.
机译:地球物理学发展的一个趋势是寻求更接近物理现实的波动理论,并推导相应的波动方程,以实现复杂结构的高精度正向建模、成像和反演。广义连续介质力学(GCM)理论通过引入额外的特征长度尺度参数来表示介质的微观结构特性,丰富了传统连续介质力学理论的背景,从GCM理论推导的非对称弹性波方程可以处理由微观结构相互作用引起的介质非均质性对地震波传播的影响。迄今为止,关于GCM理论推导的弹性波方程的数值解和解析解的研究很少,特别是在地震勘探的频段。此外,在现有文献中,很少有研究将GCM理论的多种理论和方法整合到一个综合框架中。本文介绍了多尺度微观结构相互作用的概念,构建了介质特征长度尺度参数与反映微孔结构的微孔特征长度尺度参数之间的定量关系,进而将修正的耦合应力理论和单参数二应变梯度理论整合到一个统一的数值建模分析框架中。

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