Abstract
Zeolite of the calcium-containing gmelinite type was synthesized based on the halloysite, dolomite, and obsidian minerals. The cation-exchange, dehydrating, and rehydrating properties of zeolite were studied and the oxygen exchange was calculated.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
http://wiki.web.ru/wiki
Baerlocher, C., McCusker, L.B., and Olson, D.H., Atlas of Zeolite Framework Types, New York: Elsevier, 2007, 6th ed.
Ganbarov, D.M. and Amirov, S.T., Strukturnaya khimiya tseolitov (Structural Chemistry of Zeolites), Baku: Elm, 2001.
Mamedov, Kh.S. and Gasimov, G.O., The oxygen volume and water content in zeolites, Azerb. Khim. Zh., 1973, no. 4, pp. 118–121.
Agapyatova, O.A., Vanina, E.A., Astapova, E.S., and Bogun, S.V., Study of chain silicates and layered aluminum silicates by IR spectroscopy, in Materialy III Regional’noi nauchnoi konferentsii “Fizika fundamental’nye i prikladnye issledovaniya, obrazovanie” (Proc. III Regional Sci. Conf. “Physics: Fundamental Problems, Applied Research, and Education”), Blagoveshchensk, 2002, pp. 115–116.
Author information
Authors and Affiliations
Corresponding author
Additional information
Original Russian Text © G.A. Mamedova, 2016, published in Fizika i Khimiya Stekla.
Rights and permissions
About this article
Cite this article
Mamedova, G.A. Synthesis of zeolite with a gmelinite structure in the dolomite-halloysite-obsidian system. Glass Phys Chem 42, 518–521 (2016). https://doi.org/10.1134/S1087659616050102
Received:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S1087659616050102