Elastic wave propagation in an irregularly layered medium
The indirect boundary element method (IBEM) is used to simulate wave propagation in two-dimensional irregularly layered elastic media for internal line sources. The method is based on the integral representation for scattered elastic waves using single layer boundary sources. Fulfillment of the boun...
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Veröffentlicht in: | Soil dynamics and earthquake engineering (1984) 1999, Vol.18 (1), p.11-18 |
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container_title | Soil dynamics and earthquake engineering (1984) |
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creator | Vai, Rossana Castillo-Covarrubias, José Manuel Sánchez-Sesma, FranciscoJ Komatitsch, Dimitri Vilotte, Jean-Pierre |
description | The indirect boundary element method (IBEM) is used to simulate wave propagation in two-dimensional irregularly layered elastic media for internal line sources. The method is based on the integral representation for scattered elastic waves using single layer boundary sources. Fulfillment of the boundary conditions leads to a system of integral equations. Results are obtained in the frequency domain and seismograins are computed through Fourier synthesis. In order to test and validate the method we present various comparisons between our results and the time series obtained analytically for a buried line source in a half-space and by using the recently developed spectral element method (SEM). |
doi_str_mv | 10.1016/S0267-7261(98)00027-X |
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The method is based on the integral representation for scattered elastic waves using single layer boundary sources. Fulfillment of the boundary conditions leads to a system of integral equations. Results are obtained in the frequency domain and seismograins are computed through Fourier synthesis. 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The method is based on the integral representation for scattered elastic waves using single layer boundary sources. Fulfillment of the boundary conditions leads to a system of integral equations. Results are obtained in the frequency domain and seismograins are computed through Fourier synthesis. In order to test and validate the method we present various comparisons between our results and the time series obtained analytically for a buried line source in a half-space and by using the recently developed spectral element method (SEM).</description><subject>Applied geophysics</subject><subject>Computer Science</subject><subject>Diffracted–scattered wavefields</subject><subject>Distributed, Parallel, and Cluster Computing</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Engineering geology</subject><subject>Exact sciences and technology</subject><subject>Internal geophysics</subject><subject>Irregularly layered viscoelastic media</subject><subject>Synthetic seismograms</subject><issn>0267-7261</issn><issn>1879-341X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqFkE1rGzEQQEVJoU7an1DYQynNYduRtCtpTyGEfBQMPTQB38RYO0oU5F1HWjv430eOQ3rsZWYY3swwj7GvHH5y4OrXXxBK11oo_qMzpwAgdL34wGbc6K6WDV8csdk78okd5_wIwDU3asa6y4h5Cq56xi1V6zSu8R6nMA5VGCosMSW630RMcVdF3FGivlpRHzarz-yjx5jpy1s-YXdXl7cXN_X8z_Xvi_N57Rqlp1p6AuOlFL2UqofGoFDKLY0RxjXdspGeU-uXHXojQRPxUjdqyb1yjQbXyBN2etj7gNGuU1hh2tkRg705n9t9D0CpDlq95YX9fmDLI08bypNdhewoRhxo3GQrNPCWq7aA7QF0acw5kX_fzMHupdpXqXZvzHbGvkq1izL37e0AZofRJxxcyP-GlVBGioKdHTAqYraBks0u0OCKuERusv0Y_nPoBal6ik4</recordid><startdate>1999</startdate><enddate>1999</enddate><creator>Vai, Rossana</creator><creator>Castillo-Covarrubias, José Manuel</creator><creator>Sánchez-Sesma, FranciscoJ</creator><creator>Komatitsch, Dimitri</creator><creator>Vilotte, Jean-Pierre</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SM</scope><scope>8FD</scope><scope>FR3</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0003-2309-8269</orcidid></search><sort><creationdate>1999</creationdate><title>Elastic wave propagation in an irregularly layered medium</title><author>Vai, Rossana ; Castillo-Covarrubias, José Manuel ; Sánchez-Sesma, FranciscoJ ; Komatitsch, Dimitri ; Vilotte, Jean-Pierre</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c467t-3fe08f332d336d048a266cb8828c49b43f1e5fb9af8307ee1fb946b1f6c470c43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>Applied geophysics</topic><topic>Computer Science</topic><topic>Diffracted–scattered wavefields</topic><topic>Distributed, Parallel, and Cluster Computing</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Engineering geology</topic><topic>Exact sciences and technology</topic><topic>Internal geophysics</topic><topic>Irregularly layered viscoelastic media</topic><topic>Synthetic seismograms</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Vai, Rossana</creatorcontrib><creatorcontrib>Castillo-Covarrubias, José Manuel</creatorcontrib><creatorcontrib>Sánchez-Sesma, FranciscoJ</creatorcontrib><creatorcontrib>Komatitsch, Dimitri</creatorcontrib><creatorcontrib>Vilotte, Jean-Pierre</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Earthquake Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Soil dynamics and earthquake engineering (1984)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Vai, Rossana</au><au>Castillo-Covarrubias, José Manuel</au><au>Sánchez-Sesma, FranciscoJ</au><au>Komatitsch, Dimitri</au><au>Vilotte, Jean-Pierre</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Elastic wave propagation in an irregularly layered medium</atitle><jtitle>Soil dynamics and earthquake engineering (1984)</jtitle><date>1999</date><risdate>1999</risdate><volume>18</volume><issue>1</issue><spage>11</spage><epage>18</epage><pages>11-18</pages><issn>0267-7261</issn><eissn>1879-341X</eissn><coden>SDEEEJ</coden><abstract>The indirect boundary element method (IBEM) is used to simulate wave propagation in two-dimensional irregularly layered elastic media for internal line sources. 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subjects | Applied geophysics Computer Science Diffracted–scattered wavefields Distributed, Parallel, and Cluster Computing Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Engineering geology Exact sciences and technology Internal geophysics Irregularly layered viscoelastic media Synthetic seismograms |
title | Elastic wave propagation in an irregularly layered medium |
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