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Frequency-domain Green's function in homogeneous media

Using the forward Fourier transformation equation A-2, the wave equation for pressure in a homogeneous medium with $ c(\mathbf{x})=c_0$ is written in the frequency-domain as

$\displaystyle \partial^2_i P + \frac{\omega^2}{c_0^2} P = 0.$ (65)

The frequency-domain Green's function $ G = G(\mathbf{x},\mathbf{x}_s,\omega)$ is defined by introducing an impulsive point source acting at $ t=0$ and $ \mathbf{x}=\mathbf{x}_s$ on the right-hand side of equation A-4 as follows:

$\displaystyle \partial^2_{i} G + \frac{\omega^2}{c_0^2} G = -\delta(\mathbf{x}-\mathbf{x}_s).$ (66)

The Green's function solution for two-dimensional space, under the far field approximation can be obtained as

$\displaystyle G(\mathbf{x},\mathbf{x}_s,\omega) = \frac{1}{\sqrt{8\pi\omega c_0...
...\left\vert \mathbf{x}-\mathbf{x}_s \right\vert + \frac{\pi}{4} \right] \right).$ (67)

A source function is easily included by multiplication with the frequency-domain source function. A measurement, $ P_A(\omega)$, at a station located at $ \mathbf{x}_A$ of a source at $ \mathbf{x}_s$ emitting a source function $ s(\omega)$ is obtained as follows:

$\displaystyle P_A = G(\mathbf{x}_A,\mathbf{x}_s,\omega)s(\omega).$ (68)

The sources in this paper are simulated emitting zero-phase Ricker wavelets with center frequency $ \omega_0$. The frequency-domain expression used is

$\displaystyle s(\omega) = \frac{2 \omega^2}{\sqrt{\pi}  \omega_0^3} \mathrm{exp}\left( -\frac{\omega^2}{\omega_0^2} \right).$ (69)


next up previous [pdf]

Next: Green's function in the Up: Wave equation and Green's Previous: Fourier Transformations

2009-05-05