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dc.contributor.authorKuzhir, Pavel
dc.contributor.authorMagnet, Cecilia
dc.contributor.authorRodríguez Arco, Laura 
dc.contributor.authorLópez López, Modesto Torcuato 
dc.contributor.authorFezai, H.
dc.contributor.authorMeunier, Alain
dc.contributor.authorZubarev, Andrey
dc.contributor.authorBossis, Georges
dc.date.accessioned2015-11-03T07:35:50Z
dc.date.available2015-11-03T07:35:50Z
dc.date.issued2014-09-11
dc.identifier.citationKuzhir, P.; et al. Magnetorheological effect in the magnetic field oriented along the vorticity. Journal of Rheology, 58: 1829 (2014). [http://hdl.handle.net/10481/38668]es_ES
dc.identifier.issn0148-6055
dc.identifier.issn1520-8516
dc.identifier.urihttp://hdl.handle.net/10481/38668
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 Kuzhir, P.; et al. Magnetorheological effect in the magnetic field oriented along the vorticity. Journal of Rheology, 58: 1829 (2014) and may be found at http://dx.doi.org/10.1122/1.4893586.es_ES
dc.description.abstractIn this work, we have studied the magnetorheological (MR) fluid rheology in the magnetic field parallel to the fluid vorticity. Experimentally, the MR fluid flow was realized in the Couette coaxial cylinder geometry with the magnetic field parallel to the symmetry axis. The rheological measurements were compared to those obtained in the cone-plate geometry with the magnetic field perpendicular to the lower rheometer plate. Experiments revealed a quasi-Bingham behavior in both geometries with the stress level being just a few dozens of percent smaller in the Couette cylindrical geometry at the same internal magnetic field. The unexpectedly high MR response in the magnetic field parallel to the fluid vorticity is explained by stochastic fluctuations of positions and orientations of the particle aggregates. These fluctuations are induced by magnetic interactions between them. Once misaligned from the vorticity direction, the aggregates generate a high stress independent of the shear rate, and thus assimilated to the suspension apparent (dynamic) yieldstress. Quantitatively, the fluctuations of the aggregate orientation are modeled as a rotary diffusion process with a diffusion constant proportional to the mean square interaction torque. The model gives a satisfactory agreement with the experimental field dependency of the apparent yield stress and confirms the nearly quadratic concentration dependency rY / U2:2, revealed in experiments. The practical interest of this study lies in the development of MR smart devices with the magnetic field nonperpendicular to the channel walls.es_ES
dc.description.sponsorshipThis work has been supported by Projects P09-FQM-4787 (Junta de Andalucıa, Spain), “Factories of the Future” (Grant No. 260073, DynExpert FP7) and PICS 161801 project: “Magnetic nanocomposites for mechanical and biological applications” with Ural Federal University, Russia. In addition, L.R.-A. acknowledges financial support by Secretarıa de Estado de Educacion, Formacion Profesional y Universidades (MECD, Spain) through its FPU and Estancias Breves programs.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.subjectMagnetorheological effectes_ES
dc.subjectMagnetorheological fluidses_ES
dc.subjectMagnetic fields es_ES
dc.subjectVortex dynamicses_ES
dc.subjectSuspensionses_ES
dc.subjectMagnetoresistancees_ES
dc.titleMagnetorheological effect in the magnetic field oriented along the vorticityes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.doi10.1122/1.4893586


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