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dc.contributor.authorSuárez Barrios, María Mercedes 
dc.contributor.authorGarcía Rivas, Javier
dc.contributor.authorMorales Sánchez Migallón, Juan 
dc.contributor.authorLorenzo, Adrián
dc.contributor.authorGarcía-Vicente, Andrea
dc.contributor.authorGarcía Romero, Emilia
dc.date.accessioned2026-01-22T11:49:52Z
dc.date.available2026-01-22T11:49:52Z
dc.date.issued2022
dc.identifier.citationMercedes Suárez, Javier García-Rivas, Juan Morales, Adrián Lorenzo, Andrea García-Vicente, Emilia García-Romero, Review and new data on the surface properties of palygorskite: A comparative study, Applied Clay Science, Volume 216, 2022, 106311, ISSN 0169-1317, https://doi.org/10.1016/j.clay.2021.106311. (https://www.sciencedirect.com/science/article/pii/S0169131721003355)es_ES
dc.identifier.issn0169-1317
dc.identifier.urihttp://hdl.handle.net/10366/169184
dc.description.abstract[EN]Palygorskite is a mineral used in a wide number of industrial sectors. Currently, there are hundreds of studies in which palygorskite is a part of different nanocomposites and bionanocomposites. The surface properties are essential for these applications, and in this work, an in-depth revision of these properties is done, showing that the high variability found cannot be explained only by the number of impurities or by differences in the analysis conditions. To further deepen the knowledge of the surface properties of palygorskite and palygorskitic clays, a comparative study of a wide group of high purity samples is also performed, and new data on these surface properties are provided with the determination of the specific surface area (SSA), micropore surface area (SSAμp), micropore volume (Vμp), external surface area (SSAEx), and mean equivalent pore diameter. Both the bibliographic data and new data show that SSA varies from a few tens of m2g−1 to almost 300 m2g−1, and the microporosity and external surface proportions also vary greatly. The experimental data obtained show that 1) ordinary soft vacuum conditions produce structural folding, which limits the accessibility to the inner part of the structural tunnels; 2) microporosity is related to the intra- and inter-fibre microporosity, depending first on the fibre size, because the shorter the fibre, the higher the partial accessibility to the entrance of the channels; 3) the crystal chemistry of the samples also influences the SSA because the Mg-rich terms, which have higher content of sepiolite polysome proportions in their structure as well as wider and more accessible intracrystalline channels than palygorskite polysomes.es_ES
dc.format.mimetypeapplication/pdf
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.subjectPalygorskitees_ES
dc.subjectSpecific surface areaes_ES
dc.subjectMicroporosityes_ES
dc.subjectexternal areaes_ES
dc.subjectmicrostructurees_ES
dc.titleReview and new data on the surface properties of palygorskite: A comparative studyes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publishversionhttps://doi.org/10.1016/j.clay.2021.106311es_ES
dc.subject.unesco2506 Geologíaes_ES
dc.identifier.doi10.1016/j.clay.2021.106311
dc.relation.projectIDGrant PID-2019-106504RB funded by MCIN/AEI/ 10.13039/501100011033es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.journal.titleApplied Clay Sciencees_ES
dc.volume.number216es_ES
dc.page.initial106311es_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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