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Review and new data on the surface properties of palygorskite: A comparative study

dc.contributor.authorSúarez Barrios, Mercedes
dc.contributor.authorGarcía Rivas, Javier
dc.contributor.authorMorales, Juan
dc.contributor.authorLorenzo, Adrián
dc.contributor.authorGarcía Vicente, Andrea
dc.contributor.authorGarcía Romero, Emilia
dc.date.accessioned2023-06-16T14:18:09Z
dc.date.available2023-06-16T14:18:09Z
dc.date.issued2021-10-17
dc.description.abstractPalygorskite 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.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Ciencia e Innovación (MICINN)
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/69307
dc.identifier.doi10.1016/j.clay.2021.106311
dc.identifier.issn0169-1317
dc.identifier.officialurlhttps://doi.org/10.1016/j.clay.2021.106311
dc.identifier.urihttps://hdl.handle.net/20.500.14352/4590
dc.issue.number106311
dc.journal.titleApplied clay science
dc.language.isoeng
dc.publisherElsevier
dc.relation.projectIDPID-2019-106504RB
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.cdu549.62
dc.subject.keywordPalygorskite
dc.subject.keywordSpecific surface area
dc.subject.keywordMicroporosityExternal area
dc.subject.keywordMicrostructure
dc.subject.ucmMineralogía (Geología)
dc.subject.unesco2506.11 Mineralogía
dc.titleReview and new data on the surface properties of palygorskite: A comparative study
dc.typejournal article
dc.volume.number216
dspace.entity.typePublication
relation.isAuthorOfPublicatione039abf0-032e-428b-a0d2-513967a1c0ff
relation.isAuthorOfPublicationb7658e83-41da-46f0-aca8-94370da806bd
relation.isAuthorOfPublication.latestForDiscoverye039abf0-032e-428b-a0d2-513967a1c0ff

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