Journal
COMPUTATIONAL GEOSCIENCES
Volume 17, Issue 6, Pages 913-927Publisher
SPRINGER
DOI: 10.1007/s10596-013-9364-0
Keywords
Stochastic inverse modeling; Numerical linear algebra; Hierarchical matrices; Large-scale problems; Subsurface imaging; Tomography; Geostatistical estimation
Funding
- US Department of Energy, National Energy Technology Laboratory (DOE, NETL) [DE-FE0009260]
- National Science Foundation -Division of Mathematical Sciences [1228275]
- U.S. Army Research Laboratory [W911NF-07-2-0027]
- Division Of Mathematical Sciences
- Direct For Mathematical & Physical Scien [1228275] Funding Source: National Science Foundation
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Stochastic inverse modeling deals with the estimation of functions from sparse data, which is a problem with a nonunique solution, with the objective to evaluate best estimates, measures of uncertainty, and sets of solutions that are consistent with the data. As finer resolutions become desirable, the computational requirements increase dramatically when using conventional solvers. A method is developed in this paper to solve large-scale stochastic linear inverse problems, based on the hierarchical matrix (or a< (2) matrix) approach. The proposed approach can also exploit the sparsity of the underlying measurement operator, which relates observations to unknowns. Conventional direct algorithms for solving large-scale linear inverse problems, using stochastic linear inversion techniques, typically scale as oe'(a)(n (2) m+nm (2)), where n is the number of measurements and m is the number of unknowns. We typically have n a parts per thousand(a) m. In contrast, the algorithm presented here scales as oe'(a)(n (2) m), i.e., it scales linearly with the larger problem dimension m. The algorithm also allows quantification of uncertainty in the solution at a computational cost that also grows only linearly in the number of unknowns. The speedup gained is significant since the number of unknowns m is often large. The effectiveness of the algorithm is demonstrated by solving a realistic crosswell tomography problem by formulating it as a stochastic linear inverse problem. In the case of the crosswell tomography problem, the sparsity of the measurement operator allows us to further reduce the cost of our proposed algorithm from oe'(a)(n (2) m) to . The computational speedup gained by using the new algorithm makes it easier, among other things, to optimize the location of sources and receivers, by minimizing the mean square error of the estimation. Without this fast algorithm, this optimization would be computationally impractical using conventional methods.
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