Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/9235
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dc.contributor.authorNevel, D. E.-
dc.contributor.authorHaynes, F. Donald-
dc.date.accessioned2016-06-20T13:40:51Z-
dc.date.available2016-06-20T13:40:51Z-
dc.date.issued1976-04-
dc.identifier.urihttp://hdl.handle.net/11681/9235-
dc.descriptionCRREL Report-
dc.descriptionAbstract: Griffith, and later Babel, have previously developed a tensile fracture criterion for a two-dimensional state of stress. This theory is extended to the compression-compression region. From this theory the angle of fracture is developed. The theory is extended conceptually to three dimensions. Triaxial test data by Haynes for snow-ice are shown in this three-dimensional fracture theory. The test data are slightly less than those predicted when the void in the snow-ice is spherical.-
dc.publisherCold Regions Research and Engineering Laboratory (U.S.)-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1011068-
dc.relation.ispartofseriesCRREL report ; 76-5.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectFracture (mechanics)-
dc.subjectIce tensile strength-
dc.subjectTriaxial stresses-
dc.subjectFracture mechanics-
dc.subjectIce-
dc.titleInterpretation of the tensile strength of ice under triaxial stress-
dc.typeReporten_US
Appears in Collections:CRREL Report

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