Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5997
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dc.contributorUniversity of Michigan. Engineering Research Institute.-
dc.contributor.authorWilson, James T.-
dc.date.accessioned2016-03-21T21:14:39Z-
dc.date.available2016-03-21T21:14:39Z-
dc.date.issued1955-09-
dc.identifier.urihttp://hdl.handle.net/11681/5997-
dc.descriptionTechnical report-
dc.descriptionAbstract: The elementary theory of coupling or resonance between a moving load and the flexural waves generated by it in a floating ice sheet is developed and verified by experiments. The theory indicates that for shallow water the critical velocity is approximately 20 percent greater than the velocity of long water waves. Experiments were carried out, using one and two vehicles as moving loads on ice sheets one to two feet thick. At the critical speed (for a single vehicle) the maximum observed motion approximately 2.5 times the static deflection. For two vehicles, running in tandem a half wave length apart, a considerable cancellation was observed. Attempts to solve the problem of a semi-infinite plate on an elastic foundation with a free edge under concentrated load (the ice-breaker problem) are reported. No satisfactory solution was obtained.-
dc.publisherU.S. Army Snow, Ice, and Permafrost Research Establishment.-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1022180-
dc.relation.ispartofseriesSIPRE report ; 34.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectIce-
dc.subjectFloating ice-
dc.subjectWater waves-
dc.subjectWave propagation-
dc.subjectRigidity-
dc.subjectResonance-
dc.subjectLoads-
dc.subjectElastic plates-
dc.subjectElastic shells-
dc.subjectMoving loads-
dc.subjectElastic waves-
dc.titleCoupling between moving loads and flexural waves in floating ice sheets-
dc.typeDOCUMENT-
Appears in Collections:Technical Report

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