ELECTROMAGNETIC INDUCTION IN A GENERALIZED 3D ANISOTROPIC EARTH, PART 2: THE LIN PRECONDITIONER

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dc.contributor.author Weiss C.J.
dc.contributor.author Newman G.A.
dc.date.accessioned 2022-02-05T05:13:31Z
dc.date.available 2022-02-05T05:13:31Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=14076289
dc.identifier.citation Geophysics, 2003, 68, 3, 922-930
dc.identifier.issn 0016-8033
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/34978
dc.description.abstract A practical limitation in the use of generalized 3D forward modeling algorithms for inversion of electromagnetic data is the high computational cost of solving large, ill-conditioned systems of linear equations arising from the discretization of the governing Maxwell equations. To address this problem, a new class of preconditioners has recently been proposed which is based on a Helmholtz decomposition of the electric field in the low induction number (LIN) regime. This paper further develops that idea and introduces a LIN preconditioner which can be applied to problems characterized by a fully generalized anisotropic medium. Included are sample calculations demonstrating a reduction by two orders of magnitude in the number of "quasi-minimal residual" iterates and a speedup by a factor of approximately four in the solution time for one forward calculation. Also included are results previously unobtainable by standard Jacobi preconditioning for simulating multicomponent induction sonde response in a horizontal well within a crossbedded formation.
dc.title ELECTROMAGNETIC INDUCTION IN A GENERALIZED 3D ANISOTROPIC EARTH, PART 2: THE LIN PRECONDITIONER
dc.type Статья


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