Thermal and structural stability of microporous natural clinoptilolite zeolite

Thermal treatment of zeolites prior to their use as adsorbents is needed to remove adsorbed water from zeolite pores, increasing porosity and surface area without inducing structural deterioration. Here, natural zeolite clinoptilolite (CLI) was thermally treated at 378–1073 K in air atmosphere. Poro...

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Published inMicroporous and mesoporous materials Vol. 341; p. 112101
Main Authors Kukobat, Radovan, Škrbić, Ranko, Massiani, Pascale, Baghdad, Karima, Launay, Franck, Sarno, Maria, Cirillo, Claudia, Senatore, Adolfo, Salčin, Esad, Atlagić, Suzana Gotovac
Format Journal Article
LanguageEnglish
Published Elsevier Inc 01.08.2022
Elsevier
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ISSN1387-1811
1873-3093
DOI10.1016/j.micromeso.2022.112101

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Summary:Thermal treatment of zeolites prior to their use as adsorbents is needed to remove adsorbed water from zeolite pores, increasing porosity and surface area without inducing structural deterioration. Here, natural zeolite clinoptilolite (CLI) was thermally treated at 378–1073 K in air atmosphere. Porosity and structural changes after treatments at particular temperatures were investigated with N2 adsorption at 77 K, Fourier transform infrared (FTIR) spectroscopy and X-ray diffraction (XRD). Brunauer, Emmett and Teller (BET) surface area reached 60 m2 g−1 and αS surface area reached 80 m2 g−1 after thermal treatment at 473 K due to the evolution of water as evidenced with FTIR spectroscopy. Monoclinic crystal structure of the CLI zeolite was preserved after thermal treatment at ∼873 K as indicated with XRD analysis. The CLI zeolite are structurally stable at ∼873 K, reaching the highest specific surface area at 473 K, thus being promising for future adsorbent applications. [Display omitted] •Composition and porosity against thermal treatment were investigated for the natural clinoptilolite zeolites.•The BET and αS specific surface areas reached the maximum of 60 and 80 m2 g−1 after thermal treatment at 473 K.•The surface area increased due to the evolution of water from the clinoptilolite pores.
ISSN:1387-1811
1873-3093
DOI:10.1016/j.micromeso.2022.112101