File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Conference Paper: Mechanics of water waves over a viscoelastic mud layer

TitleMechanics of water waves over a viscoelastic mud layer
Authors
KeywordsViscoelastic mud
Water surface waves
Wave boundary layer flow
Issue Date2006
PublisherISOPE.
Citation
Proceedings Of The International Offshore And Polar Engineering Conference, 2006, p. 702-708 How to Cite?
AbstractThis is a study on the interaction between water surface waves and a thin layer of viscoelastic mud on the bottom. On assuming that the mud layer is comparable in thickness with the wave boundary layer and is much smaller than the wavelength, a two-layer Stokes boundary layer model is adopted to determine the mud motions under the waves. Analytical expressions are derived for the near-bottom water and mud velocity fields, surface wave-damping rate, and interface wave amplitude and phase lag. It is examined in particular how these kinematic quantities may depend on the viscous and elastic properties of the mud. Copyright © 2006 by The International Society of Offshore and Polar Engineers.
Persistent Identifierhttp://hdl.handle.net/10722/100442
ISSN
References

 

DC FieldValueLanguage
dc.contributor.authorNg, COen_HK
dc.contributor.authorZhang, Xen_HK
dc.date.accessioned2010-09-25T19:10:11Z-
dc.date.available2010-09-25T19:10:11Z-
dc.date.issued2006en_HK
dc.identifier.citationProceedings Of The International Offshore And Polar Engineering Conference, 2006, p. 702-708en_HK
dc.identifier.issn1098-6189en_HK
dc.identifier.urihttp://hdl.handle.net/10722/100442-
dc.description.abstractThis is a study on the interaction between water surface waves and a thin layer of viscoelastic mud on the bottom. On assuming that the mud layer is comparable in thickness with the wave boundary layer and is much smaller than the wavelength, a two-layer Stokes boundary layer model is adopted to determine the mud motions under the waves. Analytical expressions are derived for the near-bottom water and mud velocity fields, surface wave-damping rate, and interface wave amplitude and phase lag. It is examined in particular how these kinematic quantities may depend on the viscous and elastic properties of the mud. Copyright © 2006 by The International Society of Offshore and Polar Engineers.en_HK
dc.languageengen_HK
dc.publisherISOPE.en_HK
dc.relation.ispartofProceedings of the International Offshore and Polar Engineering Conferenceen_HK
dc.subjectViscoelastic muden_HK
dc.subjectWater surface wavesen_HK
dc.subjectWave boundary layer flowen_HK
dc.titleMechanics of water waves over a viscoelastic mud layeren_HK
dc.typeConference_Paperen_HK
dc.identifier.emailNg, CO:cong@hku.hken_HK
dc.identifier.authorityNg, CO=rp00224en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.scopuseid_2-s2.0-36749017930en_HK
dc.identifier.hkuros116381en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-36749017930&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.spage702en_HK
dc.identifier.epage708en_HK
dc.publisher.placeUnited Statesen_HK
dc.identifier.scopusauthoridNg, CO=7401705594en_HK
dc.identifier.scopusauthoridZhang, X=13410231200en_HK

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats