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Nonlinear Traveltime Tomographyby Submitted to the Department of Earth, Atmospheric, and Planetary Sciences on May 21, 1993 in partial fulfillment of the requirements for the degree of Doctor of Philosophy ABSTRACT
In this thesis we develop a procedure for performing tomography in a physically
meaningful way; i.e., reconstructing seismic velocities from traveltime data
such that the traveltimes are fit over physically meaningful raypaths. Not only
do we provide a method for obtaining reconstructions, but we also characterize
the uncertainty of the reconstructions in terms of resolution and variance.
We then show that the method is practical for large scale field experiments
by showing its application to a large (20,000 traveltime data) cross-well seismic
survey at MIT's Michigan Basin research facility. Specifically, we solve the
nonlinear traveltime tomography problem using the regularization method of Tikhonov.
We pose the tomography problem as a joint minimization of data misfit, with
regard to a prior variance in the traveltimes, and model roughness. The latter
is quantified as the L2 norm of the model convolved with a differencing operator.
The use of a differencing operator is important in several ways. We know from
empirical measurements of well logs that physical parameters of the subsurface
are spatially correlated. We also understand that some form of regularization
is needed to stabilize the inverse problem of nonlinear traveltime tomography.
In addition, we wish to constrain that part of the tomography problem where
the traveltime data does not provide information, namely the high spatial wavenumbers.
By regularizing the tomography problem in such a manner, we obtain a stable,
unique solution of the nonlinear tomography problem for transmission surveys,
including the cases of completely surrounding ray coverage, VSP surveying in
laterally homogeneous media, and cross-borehole experiments with accompanying
slowness logs. We demonstrate stability by showing that the discrete solutions
approach continuum solutions at fine discretization. We also show that the same
solution can be obtained from different starting models. This implies that physically
meaningful reconstructions can be made in the absence of good prior information.
Computationally, we solve the nonlinear inversion by way of the Conjugate Gradient
method, employing fast and efficient traveltime/ray modeling to refine the propagation
paths in keeping with model changes. We show that this method may be straightforwardly
implemented on a parallel computer to solve large tomography problems almost
interactively. The implementation involves decomposing source positions among
the parallel processors and performing survey-wide traveltime modeling at the
same cost as serially computing traveltimes from a single source. ``Eikonal''
modeling is used to propagate first-arrival traveltimes from the source to all
receivers simultaneously. On medium-grained (100-1000 processor) parallel computers,
we can apply the method readily to typical field surveys. The same inversion
algorithm may also be applied to the linearized inversion problem with improved
performance. As the nonlinear inversion converges toward a solution, the algorithm
behaves more and more like linearized inversion. While optimality of the reconstruction may be cast in terms of how well the
data are fit, suitability of the solution is better judged by way of uncertainty
analysis. We perform uncertainty analysis to quantify the resolution and variance
at various positions in the model. We appeal to Backus and Gilbert's notions
of the spread-vs.-variance trade-off, but within a Bayesian framework whereby
both variance and resolution are inferred from the posterior covariance associated
with our reconstruction. For computational efficiency we calculate posterior
covariance by linearizing about the reconstructed model obtained from the nonlinear
inversion. We compute the posterior covariance using a Monte Carlo algorithm
in which many realizations of perturbed data and model roughnesses are inverted.
Finally we demonstrate, for field data examples as well as numerical problems,
that the method gives resolution and variance information that behaves correctly
with regard to the ray coverage and the character of the associated reconstruction.
We apply nonlinear traveltime to two data sets: a multiple offset VSP survey
shot near Larderello, Italy, and a cross-well survey conducted by MIT in the
Michigan Basin. In the first case, we show that the uncertainty analysis may
be applied to determine the validity of information obtained in a tomogram.
In the case of the Michigan survey, we demonstrate the robustness of the inversion
in reconstructing subsurface structure from slowness log and first arrival traveltime
data in the absence of a good prior model. We apply the uncertainty analysis
to characterize the resolution and variance of these results as well. Return to Theses Return to ERL Home Updated: May, 1999
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