Time-space domain staggered-grid finite difference method for porous media

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Abstract

Finite difference methods have been widely used in seismic modeling; however, they generally suffer from numerical dispersion problems. Based on the dispersion relation for porous media, we develop the time-space domain and the weighted average time-space domain high-order staggered-grid finite difference (SFD) method to suppress the numerical dispersion. Compared with the conventional SFD method, the proposed method has better accuracy with dispersion analysis and numerical modeling under the same discretization.

Original languageEnglish
Title of host publicationSociety of Exploration Geophysicists International Exposition and 83rd Annual Meeting, SEG 2013
Subtitle of host publicationExpanding Geophysical Frontiers
PublisherSociety of Exploration Geophysicists
Pages3510-3514
Number of pages5
ISBN (Print)9781629931883
DOIs
StatePublished - 2013
EventSociety of Exploration Geophysicists International Exposition and 83rd Annual Meeting: Expanding Geophysical Frontiers, SEG 2013 - Houston, United States
Duration: 22 Sep 201327 Sep 2013

Publication series

NameSociety of Exploration Geophysicists International Exposition and 83rd Annual Meeting, SEG 2013: Expanding Geophysical Frontiers

Conference

ConferenceSociety of Exploration Geophysicists International Exposition and 83rd Annual Meeting: Expanding Geophysical Frontiers, SEG 2013
Country/TerritoryUnited States
CityHouston
Period22/09/1327/09/13

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