Application of the Reiner-Rivlin model to the slow flow of ice gravel past a cylinder

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DOIResolve DOI: http://doi.org/10.1016/0307-904X(94)90337-9
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TypeArticle
Journal titleApplied Mathematical Modelling
Volume18
Issue5
Pages288293; # of pages: 6
Subjectparameter evaluation; Reiner-Rivlin model; fragmented ice; slow motion
AbstractOn a sufficiently large scale, fragmented ice can be considered homogenous and isotropic, making model studies of its gross mechanical properties possible. The purpose of this paper is to examine the Reiner-Rivlin model by evaluating the effects of three parameters: Reynolds number, cross-viscosity, and size of the ice patch. Two-dimensional interaction with a circular cylinder is treated in detail. It has been found that, roughly speaking, the pressure distribution over a cyclindrical surface is inversely proportional to Reynolds number, and directly proportional to the coefficient C, which depends on the size of the ice patch. The total force is also proportional to the angle at separation.
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AffiliationNRC Institute for Ocean Technology; National Research Council Canada
Peer reviewedYes
IdentifierIR-1994-11
NRC number5616
NPARC number8896294
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Record identifier16a6e216-415e-47fd-83b7-15f5b4ab4eae
Record created2009-04-22
Record modified2016-05-09
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