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Mass fractal characteristics of wet sonogels as determined by small-angle x-ray scattering and differential scanning calorimetry

dc.contributor.authorVollet, D. R. [UNESP]
dc.contributor.authorDonatti, D. A. [UNESP]
dc.contributor.authorIbañez Ruiz, A. [UNESP]
dc.contributor.authorGatto, F. R. [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.date.accessioned2022-04-28T20:08:17Z
dc.date.available2022-04-28T20:08:17Z
dc.date.issued2006-08-03
dc.description.abstractLow density silica sonogels were prepared from acid sonohydrolysis of tetraethoxysilane. Wet gels were studied by small-angle x-ray scattering (SAXS) and differential scanning calorimetry (DSC). The DSC tests were carried out under a heating rate of 2°C min from -120°C up to 30°C. Aerogels were obtained by CO2 supercritical extraction and characterized by nitrogen adsorption and SAXS. The DSC thermogram displays two distinct endothermic peaks. The first, a broad peak extending from about -80°C up to practically 0°C, was associated to the melting of ice nanocrystals with a crystal size distribution with pore diameter ranging from 1 or 2 nm up to about 60 nm, as estimated from Thomson's equation. The second, a sharp peak with onset temperature close to 0°C, was attributed to the melting of macroscopic crystals. The DSC incremental nanopore volume distribution is in reasonable agreement with the incremental pore volume distribution of the aerogel as determined from nitrogen adsorption. No macroporosity was detected by nitrogen adsorption, probably because the adsorption method applies stress on the sample during measurement, leading to a underestimation of pore volume, or because often positive curvature of the solid surface is in aerogels, making the nitrogen condensation more difficult. According to the SAXS results, the solid network of the wet gels behaves as a mass fractal structure with mass fractal dimension D=2.20±0.01 in a characteristic length scale below ξ=7.9±0.1 nm. The mass fractal characteristics of the wet gels have also been probed from DSC data by means of an earlier applied modeling for generation of a mass fractal from the incremental pore volume distribution curves. The results are shown to be in interesting agreement with the results from SAXS. © 2006 The American Physical Society.en
dc.description.affiliationDepartamento de Física Unesp-Univerisdade Estadual Paulista IGCE, P.O. Box 178, CEP 13500-970 Rio Claro, SP
dc.description.affiliationUnespDepartamento de Física Unesp-Univerisdade Estadual Paulista IGCE, P.O. Box 178, CEP 13500-970 Rio Claro, SP
dc.identifierhttp://dx.doi.org/10.1103/PhysRevB.74.024208
dc.identifier.citationPhysical Review B - Condensed Matter and Materials Physics, v. 74, n. 2, 2006.
dc.identifier.doi10.1103/PhysRevB.74.024208
dc.identifier.issn1098-0121
dc.identifier.issn1550-235X
dc.identifier.scopus2-s2.0-33746554839
dc.identifier.urihttp://hdl.handle.net/11449/224782
dc.language.isoeng
dc.relation.ispartofPhysical Review B - Condensed Matter and Materials Physics
dc.sourceScopus
dc.titleMass fractal characteristics of wet sonogels as determined by small-angle x-ray scattering and differential scanning calorimetryen
dc.typeArtigo
dspace.entity.typePublication
unesp.campusUniversidade Estadual Paulista (UNESP), Instituto de Geociências e Ciências Exatas, Rio Claropt
unesp.departmentFísica - IGCEpt

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