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

期刊

APPLIED CLAY SCIENCE
卷 216, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.clay.2021.106311

关键词

Palygorskite; Specific surface area; Microporosity; External area; Microstructure

资金

  1. [PID-2019-106504RB]
  2. [MCIN/AEI/10.130 39/501100011033]

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Palygorskite is a mineral widely used in various industrial sectors, including nanocomposites and bionanocomposites. The study highlights the significant variability in surface properties of Palygorskite, which cannot be solely explained by impurities or analysis conditions. Experimental data reveals the relationship between microporosity and crystal chemistry of Palygorskite.
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 (SSA(mu p)), micropore volume (V-mu p), external surface area (SSA(Ex)), and mean equivalent pore diameter. Both the bibliographic data and new data show that SSA varies from a few tens of m(2)g(-1) to almost 300 m(2)g(-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.

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