Adsorption of Formaldehyde from Aqueous Solutions Using Metakaolin-Based Geopolymer Sorbents
- Authors: Novikova L.A.1, Bogdanov D.S.1, Belchinskaya L.I.1, Kolousek D.2, Doushova B.2, Lhotka M.2, Petukhova G.A.3
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Affiliations:
- Voronezh State University of Forestry and Technologies named after G.F. Morozov
- Prague University of Chemistry and Technology
- Frumkin Institute of Physical Chemistry and Electrochemistry, Russian Academy of Sciences
- Issue: Vol 55, No 5 (2019)
- Pages: 864-871
- Section: Physicochemical Processes at the Interfaces
- URL: https://journals.rcsi.science/2070-2051/article/view/205462
- DOI: https://doi.org/10.1134/S2070205119050198
- ID: 205462
Cite item
Abstract
Geopolymer samples prepared through alkali activation of metakaolin under varying conditions of synthesis (100°C (14 h); 130°C (3 h); clinoptilolite filler) are employed as formaldehyde sorbents from aqueous solutions. The structure and physicochemical properties of geopolymer sorbents are studied using XRD, XRF, SEM, N2 adsorption–desorption, and chemical methods. Zeolite A is the main component among the structural components in the synthesized specimens (zeolite А, hydroxysodalite, and quartz). Addition of the clinoptilolite filler in the synthesis of geopolymers has resulted in a slight increase in their specific surface and pore volume. Geopolymer sorbent specimens display strong adsorption ability in relation to sorbate molecules in aqueous solutions of formaldehyde (0.064–0.366 M). The cation-exchange capacity of the geopolymers, which is 2–3 times as large as that of the natural clinoptilolite specimen, is the probable reason of their strong adsorption capacity to formaldehyde. The nature of the exchanged cation (Na+, \({\text{NH}}_{4}^{ + },\) Cu2+) determines the magnitude and the predominant mechanism of sorption uptake of formaldehyde (physical adsorption, chemisorption, and complexation). Higher adsorption values of formaldehyde are obtained in the case of \({\text{NH}}_{4}^{ + }\)- and Cu2+-forms of geopolymer sorbents compared to the Na+-form.
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About the authors
L. A. Novikova
Voronezh State University of Forestry and Technologies named after G.F. Morozov
Author for correspondence.
Email: chem@vglta.vrn.ru
Russian Federation, Voronezh, 394087
D. S. Bogdanov
Voronezh State University of Forestry and Technologies named after G.F. Morozov
Email: chem@vglta.vrn.ru
Russian Federation, Voronezh, 394087
L. I. Belchinskaya
Voronezh State University of Forestry and Technologies named after G.F. Morozov
Email: chem@vglta.vrn.ru
Russian Federation, Voronezh, 394087
D. Kolousek
Prague University of Chemistry and Technology
Email: chem@vglta.vrn.ru
Czech Republic, Prague
B. Doushova
Prague University of Chemistry and Technology
Email: chem@vglta.vrn.ru
Czech Republic, Prague
M. Lhotka
Prague University of Chemistry and Technology
Email: chem@vglta.vrn.ru
Czech Republic, Prague
G. A. Petukhova
Frumkin Institute of Physical Chemistry and Electrochemistry, Russian Academy of Sciences
Email: chem@vglta.vrn.ru
Russian Federation, Moscow, 119071
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