Mostrar el registro sencillo del ítem

dc.contributor.authorJiménez Olivares, María Luisa 
dc.contributor.authorDelgado Mora, Ángel Vicente 
dc.contributor.authorKaatze, U.
dc.date.accessioned2013-11-13T12:51:21Z
dc.date.available2013-11-13T12:51:21Z
dc.date.issued2008
dc.identifier.citationJiménez, M.L.; Delgado, A.V.; Kaatze, U. Surface characterization of clay particles via dielectric spectroscopy. Annales Universitatis Mariae Curie-Sklodowska. Sectio AA. Chemia, 63(7): 73-86 (2008). [http://hdl.handle.net/10481/29105]es_ES
dc.identifier.issn2083-358X
dc.identifier.issn0137-6853
dc.identifier.otherdoi: 10.2478/v10063-008-0030-7
dc.identifier.urihttp://hdl.handle.net/10481/29105
dc.descriptionDedicated to Professor Emil Chibowski on the occasion of his 65th birthday.es_ES
dc.description.abstractThis work deals with the high frequency dielectric relaxation of clay (sodium montmorillonite, or NaMt) suspensions. By high frequency it is meant that the permittivity will be determined in the region where the Maxwell-Wagner-O’Konski relaxation takes place, roughly, the MHz frequency range. The applicability of dielectric determinations for the characterization of the electrical properties of these complex systems is demonstrated. In fact, standard electrophoresis measurements only allow to detect that the charge of the particles becomes slightly more negative upon increasing pH. Much more information is obtained from the high frequency electric permittivity for different concentrations of solids and pHs. From the characteristic frequencies of the relaxation it is possible to detect separate processes for parallel and perpendicular orientations of the clay platelets, modelled as oblate spheroids with a high aspect ratio. In addition, using a suitable model the surface conductivity of the clay particles can be estimated. Our data indicate that this quantity is minimum around pH 7, which is admitted as representative of the isoelectric point of the edges of the clay platelets. Data are also obtained on the amplitude (value of the relative permittivity at low frequency minus that at high frequency) of the relaxation, and it is found that it depends linearly on the volume fraction of solids, and that it is minimum at pH 5. These results are considered to be a manifestation of the fact that particle interactions do not affect the electric conduction inside the electric double layer, while the special behaviour at pH 5 is related to the existence of aggregates at pH 5, which increase the effective size of the particles and provoke a reduction of their effective conductivity.es_ES
dc.description.sponsorshipFinancial support for this work by MEC (Spain) (Projects FIS2005-06860-C02-01, 02) and Junta de Andalucia (Spain) (Project FQM410) is gratefully acknowledged.es_ES
dc.language.isoenges_ES
dc.publisherWydawnictwo Uniwersytetu Marii Curie-Sklodowskiej w Lubliniees_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.subjectClay es_ES
dc.subjectParticles es_ES
dc.subjectDielectrices_ES
dc.subjectSpectroscopyes_ES
dc.subjectSodium montmorillonitees_ES
dc.subjectElectrophoresis es_ES
dc.subjectMaxwell-Wagner-O'Konski (MWO)es_ES
dc.titleSurface characterization of clay particles via dielectric spectroscopyes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


Ficheros en el ítem

[PDF]

Este ítem aparece en la(s) siguiente(s) colección(ones)

Mostrar el registro sencillo del ítem

Creative Commons Attribution-NonCommercial-NoDerivs 3.0 License
Excepto si se señala otra cosa, la licencia del ítem se describe como Creative Commons Attribution-NonCommercial-NoDerivs 3.0 License