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A modified wave equation with diffusion effects and its application as a smoothing scheme for seismic wave propagation simulations

机译:具有扩散效应的修正波动方程及其在地震波传播模拟中的平滑方案

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We present a new modified wave equation and apply it to develop a smoothing scheme for seismic wave propagation simulations. With mathematical rigour we show that the solution of the new equation, which is derived as an analog of the advection-diffusion equation, can be obtained by the spatial convolution between a solution of the wave equation and the heat kernel and has a finite propagation speed and a diffusion effect. Using numerical experiments we show that the smoothing scheme based on the modified wave equation has the following advantages. Firstly, it preserves the characteristics of the wave equation such as wave propagation speed. Secondly, it selectively removes the short-wavelength components of the solution. Lastly, the energy decreases slowly after the short-wavelength components have been removed. Since our smoothing scheme can be implemented by adding simple correction terms to usual schemes, it can easily be applied to the seismic wave equation.
机译:我们提出了一个新的修改后的波动方程,并将其应用于开发地震波传播模拟的平滑方案。通过严格的数学计算,我们证明了通过对流扩散方程和热核之间的空间卷积可以获得新方程的解,该方程是对流扩散方程的模拟,它的传播速度是有限的和扩散效果。通过数值实验表明,基于改进波动方程的平滑方案具有以下优点。首先,它保留了波动方程的特性,例如波传播速度。其次,它有选择地去除溶液的短波长成分。最后,在去除短波长分量之后,能量缓慢降低。由于我们的平滑方案可以通过在常规方案中添加简单的校正项来实现,因此可以轻松地将其应用于地震波方程。

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