Abstract
Identification of heterogeneous hydraulic aquifer properties from limited dynamic flow measurements typically leads to underdetermined nonlinear inverse problems that can have many solutions, including solutions that are geologically implausible and fail to predict future performance of the system. The problem is usually regularized by incorporating implicit or explicit prior information to stabilize the solution techniques and to obtain plausible solutions. A meaningful regularization must be informed by the physics of the problem, distinct properties of the formation under investigation, and other available sources of information (e.g., outcrop, well logs, and seismic). This chapter proposes sparsity as an intrinsic property of spatially distributed aquifer hydraulic properties that can be used to regularize the solution of the related ill-posed inverse problem. Inspired by recent advances in sparse signal processing, formalized under the compressed sensing paradigm, proper sparsifying bases are introduced to describe aquifer hydraulic conductivity distribution. Such descriptions give rise to a sparse reconstruction formulation of the subsurface flow model calibration inverse problem, which can be efficiently solved following recent algorithmic developments in sparse signal processing. The compressed sensing paradigm specifies the conditions under which unique solutions to underdetermined linear system of equations exist and can be computed efficiently. Sparsity is a fundamental notion in compressed sensing, and is often present in many natural images. In particular, sparsity is prevalent in describing many spatially correlated aquifer properties. The practical implications of compressed sensing are as far reaching as the solution of underdetermined system of equations is in science and engineering. This chapter introduces the guidelines set forth by sparse reconstruction techniques and the compressed sensing paradigm and incorporates them to formulate and solve ill-posed groundwater model calibration inverse problems.
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Jafarpour, B. (2013). Sparsity-Promoting Solution of Subsurface Flow Model Calibration Inverse Problems. In: Mishra, P., Kuhlman, K. (eds) Advances in Hydrogeology. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-6479-2_4
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