Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion

We investigate a new algorithm for computing regularized solutions of the two-dimensional magnetotelluric inverse problem. The algorithm employs a nonlinear conjugate gradients (NLCG) scheme to minimize an objective function that penalizes data residuals and second spatial derivatives of resistivit...

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Main Authors: Rodi, William L., Mackie, Randall L.
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2012
Subjects:
Online Access:http://hdl.handle.net/1721.1/75725
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author Rodi, William L.
Mackie, Randall L.
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Rodi, William L.
Mackie, Randall L.
author_sort Rodi, William L.
collection MIT
description We investigate a new algorithm for computing regularized solutions of the two-dimensional magnetotelluric inverse problem. The algorithm employs a nonlinear conjugate gradients (NLCG) scheme to minimize an objective function that penalizes data residuals and second spatial derivatives of resistivity. We compare this algorithm theoretically and numerically to two previous algorithms for constructing such 'minimum-structure' models: the Gauss-Newton method, which solves a sequence of linearized inverse problems and has been the standard approach to nonlinear inversion in geophysics, and an algorithm due to Mackie and Madden, which solves a sequence of linearized inverse problems incompletely using a (linear) conjugate gradients technique. Numerical experiments involving synthetic and field data indicate that the two algorithms based on conjugate gradients (NLCG and Mackie-Madden) are more efficient than the GaussNewton algorithm in terms of both computer memory requirements and CPU time needed to find accurate solutions to problems of realistic size. This owes largely to the fact that the conjugate gradients-based algorithms avoid two computationally intensive tasks that are performed at each step of a Gauss-Newton iteration: calculation of the full Jacobian matrix of the forward modeling operator, and complete solution of a linear system on the model space. The numerical tests also show that the Mackie-Madden algorithm reduces the objective function more quickly than our new NLCG algorithm in the early stages of minimization, but NLCG is more effective in the later computations. To help understand these results, we describe the Mackie-Madden and new NLCG algorithms in detail and couch each as a special case of a more general conjugate gradients scheme for nonlinear inversion.
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spelling mit-1721.1/757252019-04-12T20:32:38Z Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion Rodi, William L. Mackie, Randall L. Massachusetts Institute of Technology. Earth Resources Laboratory Rodi, William L. Magnetotellurics Inversion We investigate a new algorithm for computing regularized solutions of the two-dimensional magnetotelluric inverse problem. The algorithm employs a nonlinear conjugate gradients (NLCG) scheme to minimize an objective function that penalizes data residuals and second spatial derivatives of resistivity. We compare this algorithm theoretically and numerically to two previous algorithms for constructing such 'minimum-structure' models: the Gauss-Newton method, which solves a sequence of linearized inverse problems and has been the standard approach to nonlinear inversion in geophysics, and an algorithm due to Mackie and Madden, which solves a sequence of linearized inverse problems incompletely using a (linear) conjugate gradients technique. Numerical experiments involving synthetic and field data indicate that the two algorithms based on conjugate gradients (NLCG and Mackie-Madden) are more efficient than the GaussNewton algorithm in terms of both computer memory requirements and CPU time needed to find accurate solutions to problems of realistic size. This owes largely to the fact that the conjugate gradients-based algorithms avoid two computationally intensive tasks that are performed at each step of a Gauss-Newton iteration: calculation of the full Jacobian matrix of the forward modeling operator, and complete solution of a linear system on the model space. The numerical tests also show that the Mackie-Madden algorithm reduces the objective function more quickly than our new NLCG algorithm in the early stages of minimization, but NLCG is more effective in the later computations. To help understand these results, we describe the Mackie-Madden and new NLCG algorithms in detail and couch each as a special case of a more general conjugate gradients scheme for nonlinear inversion. 2012-12-13T19:38:18Z 2012-12-13T19:38:18Z 2000 Technical Report http://hdl.handle.net/1721.1/75725 Earth Resources Laboratory Industry Consortia Annual Report;2000-14 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Magnetotellurics
Inversion
Rodi, William L.
Mackie, Randall L.
Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion
title Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion
title_full Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion
title_fullStr Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion
title_full_unstemmed Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion
title_short Nonlinear Conjugate Gradients Algorithm For 2-D Magnetotelluric Inversion
title_sort nonlinear conjugate gradients algorithm for 2 d magnetotelluric inversion
topic Magnetotellurics
Inversion
url http://hdl.handle.net/1721.1/75725
work_keys_str_mv AT rodiwilliaml nonlinearconjugategradientsalgorithmfor2dmagnetotelluricinversion
AT mackierandalll nonlinearconjugategradientsalgorithmfor2dmagnetotelluricinversion