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So far our research group has focused largely on
traveltime and ray trajectories. In my research I will solve
for traveltime, ray trajectories, and displacement amplitudes, but the
emphasis will be on obtaining new results related to the
amplitudes.
According to Slawinski (2003), the transport equation
for inhomogeneous elastic media is derived from
equation (5); it reads thus:
|
(6) |
I will review the recent literature for existing
methods of solving the transport equation so that amplitude
information from such methods can be compared to my
Fourier-integral operator solutions and, in at least one
test case, to a full numerical solution of equations (5).
Only if such existing methods seem inadequate will I
devise new methods to solve the transport equation
or to improve on existing methods. Otherwise I will
focus on solving equations (5).
A new method
will involve Fourier-integral operators, which I plan
to apply starting in Spring 2004. This procedure should
prove fruitful since Fourier-integral operators are applicable to
non-elliptic problems such as equations (5) and gracefully
handle propagation of singularities, and are a powerful
modern mathematical tool for analyzing PDEs. I shall
apply Fourier-integral operators
directly to the analysis of equations of motion (5)
rather than to the transport equation. I hope to show
that this analysis extends the results of past analyses of
the transport equation with new amplitude (and perhaps
other) information that better matches subtleties in
real data over known geology, and in a
finite-difference or finite-element numerical
solution of at least one test model.
Next: Standard method of characteristics
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David Dalton
2004-04-20