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    Citas

    Título
    Review and new data on the surface properties of palygorskite: A comparative study
    Autor(es)
    Suárez Barrios, María MercedesUSAL authority ORCID
    García Rivas, Javier
    Morales Sánchez Migallón, JuanUSAL authority ORCID
    Lorenzo, Adrián
    García-Vicente, Andrea
    García Romero, Emilia
    Palabras clave
    Palygorskite
    Specific surface area
    Microporosity
    external area
    microstructure
    Clasificación UNESCO
    2506 Geología
    Fecha de publicación
    2022
    Editor
    Elsevier
    Citación
    Mercedes 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)
    Resumen
    [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.
    URI
    https://hdl.handle.net/10366/169184
    ISSN
    0169-1317
    DOI
    10.1016/j.clay.2021.106311
    Versión del editor
    https://doi.org/10.1016/j.clay.2021.106311
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