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Solving the Cauchy problem
To obtain an explicit solution of the Cauchy
problem (-) for
equation (), it is convenient to apply the
following simple transform of the wavefield P:
| |
(22) |
Here the Heavyside function H is included to take into account the
causality of the reflection seismic gathers (note that the time
tn=0 corresponds to the direct wave arrival). We can extrapolate
Q as an even function to negative times, writing the reverse of
(A-22) as follows:
| |
(23) |
With the change of function (A-22), equation ()
transforms to
| |
(24) |
Applying the change of variables
| |
(25) |
and Fourier transform in the midpoint coordinate y
| |
(26) |
I further transform equation (A-24) to the canonical form of a
hyperbolic-type partial differential equation with two variables:
| |
(27) |
rim
Figure 1
Domain of dependence of a point in the transformed coordinate system.
|
| |
The initial value conditions () and () in the
space are defined on a hyperbola of the form
. Now the solution
of the Cauchy problem follows directly from Riemann's method ().
According to this method, the domain of dependence of each point
is a part of the hyperbola between the points
and (Figure A-1). If we let denote this curve, the solution takes an explicit integral form:
| |
|
| |
| (28) |
Here R is the Riemann's function of equation (A-27), which has
the known explicit analytical expression
| |
(29) |
where J0 is the Bessel function of zeroth order. Integrating by
parts and taking into account the connection of the variables on the
curve , we can simplify equation (A-28) to the form
| |
(30) |
where
| |
(31) |
| (32) |
Applying the explicit expression for the Riemann function R
(A-29) and performing the inverse transform of both the
function and the variables allows us to rewrite equations
(A-30), (A-31), and (A-32) in the original
coordinate system. This yields the integral offset continuation
operators in the domain
| |
(33) |
where
| |
(34) |
| (35) |
| |
(36) |
| (37) |
The inverse Fourier transforms of equations (A-34) and
(A-35) are reduced to analytically evaluated integrals
() to produce explicit integral operators in the
time-and-space domain
| |
(38) |
where
| |
(39) |
| (40) |
The range of integration in (A-39) and (A-40) is
defined by the inequality
| |
(41) |
Equations (A-38), (A-39), and (A-40)
coincide with (), (), and
() in the main text.
Next: The kinematics of offset
Up: Table of Contents
Previous: Second-order reflection traveltime derivatives
Stanford Exploration Project
12/30/2000