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

DOI	Trouver le DOI : https://doi.org/10.1016/0307-904X(94)90337-9
Auteur	Rechercher : Shih, L. Y.
Format	Texte, Article
Sujet	parameter evaluation; Reiner-Rivlin model; fragmented ice; slow motion
Résumé	On 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.
Date de publication	1994
Dans	Applied Mathematical Modelling 18, nº 5 (1994) : 288–293.
Publications évaluées par des pairs	Oui
Identificateur	IR-1994-11
Numéro du CNRC	NRC-IOT-5616
Numéro NPARC	8896294
Exporter la notice	Exporter en format RIS
Signaler une correction	Signaler une correction (s'ouvre dans un nouvel onglet)
Identificateur de l’enregistrement	16a6e216-415e-47fd-83b7-15f5b4ab4eae
Enregistrement créé	2009-04-22
Enregistrement modifié	2020-04-27

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