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dc.contributor.authorJakobsen, Morten
dc.contributor.authorHuang, Xingguo
dc.contributor.authorWu, Ru-Shan
dc.date.accessioned2020-04-27T12:18:45Z
dc.date.available2020-04-27T12:18:45Z
dc.date.issued2020
dc.PublishedJakobsen M, Huang X, Wu R. Homotopy analysis of the Lippmann-Schwinger equation for seismic wavefield modeling in strongly scattering media. Geophysical Journal International. 2020eng
dc.identifier.issn0956-540Xen_US
dc.identifier.issn1365-246Xen_US
dc.identifier.urihttps://hdl.handle.net/1956/22014
dc.description.abstractWe present an application of the homotopy analysis method for solving the integral equations of the Lippmann-Schwinger type, which occurs frequently in acoustic and seismic scattering theory. In this method, a series solution is created which is guaranteed to converge independent of the scattering potential. This series solution differs from the conventional Born series because it contains two auxiliary parameters ε and h and an operator H that can be selected freely in order to control the convergence properties of the scattering series. The ε-parameter which controls the degree of dissipation in the reference medium (that makes the wavefield updates localized in space) is known from the so-called convergent Born series theory; but its use in conjunction with the homotopy analysis method represents a novel feature of this work. By using H = I (where I is the identity operator) and varying the convergence control parameters h and ε, we obtain a family of scattering series which reduces to the conventional Born series when h = −1 and ε = 0. By using H = γ where γ is a particular preconditioner and varying the convergence control parameters h and ε, we obtain another family of scattering series which reduces to the so-called convergent Born series when h = −1 and ε ≥ εc where εc is a critical dissipation parameter depending on the largest value of the scattering potential. This means that we have developed a kind of unified scattering series theory that includes the conventional and convergent Born series as special cases. By performing a series of 12 numerical experiments with a strongly scattering medium, we illustrate the effects of varying the (ε, h, H)-parameters on the convergence properties of the new homotopy scattering series. By using (ε, h, H) = (0.5, −0.8, I) we obtain a new scattering series that converges significantly faster than the convergent Born series. The use of a non-zero dissipation parameter ε seems to improve on the convergence properties of any scattering series, but one can now relax on the requirement ε ≥ εc from the convergent Born series theory, provided that a suitable value of the convergence control parameter h and operator H is used.en_US
dc.language.isoengeng
dc.publisherOxford University Pressen_US
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.titleHomotopy analysis of the Lippmann-Schwinger equation for seismic wavefield modeling in strongly scattering mediaen_US
dc.typePeer reviewed
dc.typeJournal article
dc.date.updated2020-02-12T08:43:53Z
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright the Author(s) 2020. Published by Oxford University Press on behalf of The Royal Astronomical Society.en_US
dc.identifier.doihttps://doi.org/10.1093/gji/ggaa159
dc.identifier.cristin1777097
dc.source.journalGeophysical Journal International
dc.source.pagenumber743–753
dc.identifier.citationGeophysical Journal International. 2020, 222 (2), 743-753.
dc.source.volume222
dc.source.issue2


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