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 in | Microporous and mesoporous materials Vol. 341; p. 112101 |
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Main Authors | , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Inc
01.08.2022
Elsevier |
Subjects | |
Online Access | Get full text |
ISSN | 1387-1811 1873-3093 |
DOI | 10.1016/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.
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•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. |
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ISSN: | 1387-1811 1873-3093 |
DOI: | 10.1016/j.micromeso.2022.112101 |