Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5795
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dc.contributor.authorMcGaw, Richard W.-
dc.date.accessioned2016-03-21T21:08:32Z-
dc.date.available2016-03-21T21:08:32Z-
dc.date.issued1967-12-
dc.identifier.urihttp://hdl.handle.net/11681/5795-
dc.descriptionResearch Report-
dc.descriptionAbstract: The systematic packing of uniform spheres is generalized by describing the primitive rhombohedral cell which characterizes the arrangement between layers. Volume and porosity are found in the equations to depend upon only two angular parameters, the angle between rows in a layer beta, and alpha the altitude angle between members of adjacent layers. An azimuth angle determines the position of the plane in which alpha is measured but does not enter into the porosity calculation. Four critical stacking arrangements are described, the porosity of which may be written as functions of the single parameter beta. The stable packings studied by Graton and Fraser (1935) are special cases of the critical positions. Typically unstable packings lie between these positions. Tables and graphs are presented which give the porosity of the primitive cell, as a function of alpha and beta, over the entire range from open to close packing for every possible layer configuration.-
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/1013245-
dc.relation.ispartofseriesResearch report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 201.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectSystematic packing-
dc.subjectSpheres-
dc.subjectPorosity-
dc.subjectCrystal structure-
dc.subjectSnow compaction-
dc.titleSystematic packing from the standpoint of the primitive cell-
dc.typeReporten_US
Appears in Collections:Research Report

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