Show simple item record

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


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal