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REVIEW OF LITWEQ OPERATOR

LITWEQ method is based on the scalar wave equation for variable velocity media,  
 \begin{displaymath}
{\partial^2 P\over\partial x^2}+{\partial^2 P\over\partial z^2}= 
{1\over v^2(x, z)}~{\partial^2 P\over\partial t^2} .\end{displaymath} (1)

The basic idea in this method is to rewrite the 2-D scalar wave equation in a new coordinate system. This allows us to produce uniformly space grids and to approximate the solution of (1) by using finite difference. First, let's define an auxiliary variable $\tau$ sometimes called pseudo-depth,
\begin{displaymath}
\tau=\int_0^z{1\over v(x,\theta)}d\theta.\end{displaymath} (2)

Second, let's define a reference velocity to measure the lateral velocity variation in the media:
\begin{displaymath}
{1\over v^2(z)}={1\over nx} \sum_{i=1}^{nx}{1\over v^2(x_{i},z)} ,\end{displaymath} (3)
where nx represents the number of points in the common mid point direction. With the definitions above it is possible to rewrite (1) in terms of (2) and (3) as

\begin{eqnarray}
{\partial^2 P\over\partial x^2}+{1\over v^2(\tau)}
({\partial^2...
 ...v^2(x,\tau)}-{1\over v^2(\tau)})
{\partial^2 P\over\partial t^2} ,\end{eqnarray} (4)
where $v(\tau)$ and $v(x,\tau)$ are the corresponding v(z) and v(x,z) using the definition of $\tau$.

Equation (4) is defined on the $(X, \tau, t)$ domain which is independent of the velocity. This is because we have already integrated along it when defining $\tau$ in (2). Now, we are ready to define a linear transformation (independent of the velocity) that incorporates the solutions of (4) along their characteristic lines. The linear transformation is:
\begin{eqnarray}
t_1 = \frac{1}{\sqrt{2}} (\tau + t) , \\ t_2 = \frac{1}{\sqrt{2}} (\tau - t) .\end{eqnarray} (1)
(2)

Using the chain rule for scalar fields is easy to show the following relations for this particular transformation,
\begin{eqnarray}
{\partial\over\partial\tau} & = & {1\over\sqrt{2}}({\partial\ov...
 ...1}\partial t_{2}} + 
{1\over 2}{\partial^2\over\partial t_{2}^2} .\end{eqnarray} (1)
(2)
(3)

Finally, using (5) and substituting (6) in (4) we get the LITWEQ operator:
\begin{eqnarray}
{\partial^2 P\over\partial x^2} + {2\over v^2(\tau)}
{\partial^...
 ...ial t_{1}\partial t_{2}} + 
{\partial^2 P\over\partial t_{2}^2}) .\end{eqnarray}
(7)

A detailed derivation of (7) is presented in Li (1986).


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Next: IMPLEMENTATION OF LITWEQ BY Up: Mujica: Wavefield extrapolation in Previous: Introduction
Stanford Exploration Project
11/17/1997