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dc.contributor.authorZubarev, Andrey
dc.contributor.authorIskakova, Larisa
dc.contributor.authorLópez-López, Modesto T.
dc.contributor.authorKuzhir, Pavel
dc.contributor.authorBossis, Georges
dc.date.accessioned2015-11-03T10:02:01Z
dc.date.available2015-11-03T10:02:01Z
dc.date.issued2014-09-10
dc.identifier.citationZubarev, A.; et al. On the theory of magnetoviscous effect in magnetorheological suspensions. Journal of Rheology, 58: 1673 (2014). [http://hdl.handle.net/10481/38671]es_ES
dc.identifier.issn0148-6055
dc.identifier.urihttp://hdl.handle.net/10481/38671
dc.descriptionCopyright 2014 American Institute of Physics. This article may be downloaded for personal use only. Any other use requires prior permission of the author and the American Institute of Physics.es_ES
dc.descriptionThe following article appeared in Zubarev, A.; et al. On the theory of magnetoviscous effect in magnetorheological suspensions. Journal of Rheology, 58: 1673 (2014) and may be found at http://dx.doi.org/10.1122/1.4889902es_ES
dc.description.abstractA theoretical model of magnetoviscous effect in a suspension of nonBrownian linearly magnetizable particles is suggested. A simple shear flow in the presence of an external magnetic field aligned with the velocity gradient is considered. Under the action of the applied field, the particles are supposed to form dense highly elongated droplike aggregates. Two different scenarios of the aggregates’ destruction under shearing forces are considered, namely, a “bulk” destruction of aggregates into pieces and an “erosive” destruction connected to the rupture of individual particles from the aggregate surface. Both models are based on a balance of forces acting either on the whole aggregate or on individual particles. The two approaches lead to qualitatively different Mason number (Ma) behaviors of the magnetic suspensions: The suspension viscosity scales as either Ma^-2/3 for the bulk destruction of aggregates or Ma^-4/5 for the erosive destruction. In any case, we do not recover Bingham behavior (Ma^-1) often predicted by chain models of the magneto- or electrorheology. Our theoretical results are discussed in view of comparison with existing theories and experimental results in the wide range of Mason numbers.es_ES
dc.description.sponsorshipThis work has been done under support of Russian Fund of Fundamental Investigations, Grant Nos. 12-01-00132, 13-02-91052, 13-01-96047, and 14-08-00283; by the Act 211 Government of the Russian Federation No. 02.A03.21.0006. The University of Granada (Acción Integrada con Rusia; Plan Propio 2011), as well as project CNRS PICS No. 6102 are also acknowledged for their financial support.es_ES
dc.language.isoenges_ES
dc.publisherSociety of Rheologyes_ES
dc.rightsCreative Commons Attribution-NonCommercial-NoDerivs 3.0 Licensees_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es_ES
dc.subjectMagnetoviscous effectes_ES
dc.subjectMagnetorheological fluides_ES
dc.subjectSuspensionses_ES
dc.subjectHydrodynamics es_ES
dc.subjectSurface tensiones_ES
dc.subjectViscosity es_ES
dc.subjectMagnetic fields es_ES
dc.titleOn the theory of magnetoviscous effect in magnetorheological suspensionses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.doi10.1122/1.4889902


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