File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Wave propagation in layered media by time domain BEM

TitleWave propagation in layered media by time domain BEM
Authors
Cheung, YKTham, LGLei, ZX
Issue Date1993
Citation
Earthquake Engineering & Structural Dynamics, 1993, v. 22 n. 3, p. 225-244 How to Cite?
AbstractA time domain boundary element in a cylindrical co-ordinate system is developed for the analysis of wave propagation in a layered half-space. The field quantities (displacements and tractions) are expressed as products of Fourier series in the circumferential direction and as linear polynomials in the other spatial directions. An integral equation is written for each layer as an independent domain, and these equations are then assembled into a general equation by virtue of compatibility and equilibrium conditions between the interfaces. Examples of three-dimensional wave propagation in the layered half-spaces due to various forms of surface and inner-domain excitations are reported to demonstrate the accuracy and versatility of the method. -Authors
Persistent Identifierhttp://hdl.handle.net/10722/149998
ISI Accession Number ID
WOS:A1993KR96800004

 

DC FieldValueLanguage
dc.contributor.authorCheung, YKen_US
dc.contributor.authorTham, LGen_US
dc.contributor.authorLei, ZXen_US
dc.date.accessioned2012-06-26T06:01:01Z-
dc.date.available2012-06-26T06:01:01Z-
dc.date.issued1993en_US
dc.identifier.citationEarthquake Engineering & Structural Dynamics, 1993, v. 22 n. 3, p. 225-244en_US
dc.identifier.urihttp://hdl.handle.net/10722/149998-
dc.description.abstractA time domain boundary element in a cylindrical co-ordinate system is developed for the analysis of wave propagation in a layered half-space. The field quantities (displacements and tractions) are expressed as products of Fourier series in the circumferential direction and as linear polynomials in the other spatial directions. An integral equation is written for each layer as an independent domain, and these equations are then assembled into a general equation by virtue of compatibility and equilibrium conditions between the interfaces. Examples of three-dimensional wave propagation in the layered half-spaces due to various forms of surface and inner-domain excitations are reported to demonstrate the accuracy and versatility of the method. -Authorsen_US
dc.languageengen_US
dc.relation.ispartofEarthquake Engineering & Structural Dynamicsen_US
dc.titleWave propagation in layered media by time domain BEMen_US
dc.typeArticleen_US
dc.identifier.emailCheung, YK:hreccyk@hkucc.hku.hken_US
dc.identifier.emailTham, LG:hrectlg@hkucc.hku.hken_US
dc.identifier.authorityCheung, YK=rp00104en_US
dc.identifier.authorityTham, LG=rp00176en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0027341382en_US
dc.identifier.volume22en_US
dc.identifier.issue3en_US
dc.identifier.spage225en_US
dc.identifier.epage244en_US
dc.identifier.isiWOS:A1993KR96800004-
dc.identifier.scopusauthoridCheung, YK=7202111065en_US
dc.identifier.scopusauthoridTham, LG=7006213628en_US
dc.identifier.scopusauthoridLei, ZX=7202931795en_US

Export via OAI-PMH Interface in XML Formats

OR

Export to Other Non-XML Formats