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Efficient 3D frequency response modeling with spectral accuracy by the rapid expansion method

机译:快速扩展方法,有效的3D频率响应建模和频谱精度

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摘要

Frequency responses of seismic wave propagation can be obtained either by directly solving the frequency domain wave equations or by transforming the time domain wavefields using the Fourier transform. The former approach requires solving systems of linear equations, which becomes progressively difficult to tackle for larger scale models and for higher frequency components. On the contrary, the latter approach can be efficiently implemented using explicit time integration methods in conjunction with running summations as the computation progresses. Commonly used explicit time integration methods correspond to the truncated Taylor series approximations that can cause significant errors for large time steps. The rapid expansion method (REM) uses the Chebyshev expansion and offers an optimal solution to the second-order-in-time wave equations. When applying the Fourier transform to the time domain wavefield solution computed by the REM, we can derive a frequency response modeling formula that has the same form as the original time domain REM equation but with different summation coefficients. In particular, the summation coefficients for the frequency response modeling formula corresponds to the Fourier transform of those for the time domain modeling equation. As a result, we can directly compute frequency responses from the Chebyshev expansion polynomials rather than the time domain wavefield snapshots as do other time domain frequency response modeling methods. When combined with the pseudospectral method in space, this new frequency response modeling method can produce spectrally accurate results with high efficiency.
机译:地震波传播的频率响应可以通过直接求解频域波方程或通过使用傅立叶变换来变换时域波场来获得。前一种方法需要求解线性方程组,对于大型模型和较高频率的分量,这逐渐变得难以解决。相反,随着计算的进行,可以使用显式时间积分方法结合运行求和有效地实现后一种方法。常用的显式时间积分方法对应于截断的泰勒级数逼近,对于较大的时间步长,泰勒级数逼近会导致明显的误差。快速扩展方法(REM)使用Chebyshev展开,并为二阶时间波动方程提供了最佳解决方案。将傅里叶变换应用于由REM计算的时域波场解时,我们可以得出频率响应建模公式,该公式的形式与原始时域REM方程相同,但总和系数不同。特别地,用于频率响应建模公式的求和系数对应于用于时域建模方程式的求和系数。结果,我们可以像其他时域频率响应建模方法一样,直接从切比雪夫展开多项式计算频率响应,而不是时域波场快照。当与空间伪频谱方法结合使用时,这种新的频率响应建模方法可以高效地产生频谱精确的结果。

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