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dc.contributor.authorGalindo-Gonzalez, Cecilia
dc.contributor.authorLópez López, Modesto Torcuato 
dc.contributor.authorGarcía López-Durán, Juan De Dios 
dc.date.accessioned2021-03-26T11:57:48Z
dc.date.available2021-03-26T11:57:48Z
dc.date.issued2012
dc.identifier.citationJournal of Applied Physics 112 (4), 043917, 2012es_ES
dc.identifier.urihttp://hdl.handle.net/10481/67731
dc.description.abstractMontmorillonite clay particles coated with magnetite nanoparticles suspended in aqueous media behave as magnetorheological fluids with enhanced stability as compared to conventional ones. In this work, the study of the magnetorheological behavior of these suspensions of magnetite-clay composite particles has been carried out. For this purpose, both steady and dynamic rheological measurements were carried out in the absence and in the presence of external magnetic fields. In the first kind of experiments, the rheograms of the suspensions (shear stress versus shear rate plot) are analyzed as a function of the strength of the magnetic field applied. In the second one, oscillatory stresses are applied to the system, and the storage modulus is studied as a function of the external magnetic field. In the absence of magnetic field, the suspensions develop a weak yield stress due to the aggregation of the magnetite covered clay particles. In the presence of magnetic field, the yield stress is strongly dependent on the magnetic field strength inside the samples, demonstrating that the suspensions experience a magnetorheological effect, moderate when the magnetic field strength is weak and stronger for values of magnetic field higher than 150–200 kA/m. Actually, the most intriguing result is the change of the trend in the dependence of the yield stress with the field. This dependence is approximately linear with the field for strength values smaller than 150–200 kA/m. On the other hand, for higher values, the yield stress increases with magnetic field following a power law with exponent 4.5.The results are interpreted by means of a model that relates the structure of the particles in the suspensions to the magnetic field applied and using the interaction energy between particles calculated by the extended DLVO theory to include magnetic interaction.es_ES
dc.description.sponsorshipFinancial support by Ministerio de Ciencia e Innovación (Spain) under project No FIS2009-07321, and Junta de Andalucía (Spain) under Project Nos. P08-FQM-3993 and P09-FQM-4787 is gratefully acknowledgedes_ES
dc.language.isoenges_ES
dc.titleMagnetorheological behavior of magnetite covered clay particles in aqueous suspensionses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.doi10.1063/1.4748878
dc.type.hasVersioninfo:eu-repo/semantics/acceptedVersiones_ES


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