Abstract
Powdered pressed compacts of different cationic forms of a natural chabazite were tested by dilatometry. The dilatometric curves of the various cationic forms displayed markedly different features, interpretable in terms of shrinkage by dehydration, thermal expansion, cation migration and thermal breakdown of the zeolitic structure.
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References
D. W. Breck, Zeolite Molecular Sieves: Structure, Chemistry and Use, Wiley, New York 1974, p. 771.
A. Dyer, An Introduction to Zeolite Molecular Sieves, J. Wiley & Sons, Chichester 1988, p. 149.
G. Artioli, Natural Zeolites '93, D. W. Ming and F. A. Mumpton Eds., Int. Comm. Nat. Zeol., Brockport, New York 1995, p. 199.
E. Passaglia, Natural Zeolites. Occurrence, Properties and Uses, L. B. Sand and F. A. Mumpton Eds., Pergamon Press, Elmsford 1978, p. 45.
RILEM 25 P. E. M., Recommended tests to measure the deterioration of stones and to assess the effectiveness of treatment methods, 13, n∘ 75, 1980, p. 177.
J. W. Smith, Acta Crystallografica, 15 (1962) 833.
J. W. Smith, F. Rinaldi and L. S. Glasser, Acta Cristallografica, 16 (1963) 45.
J. W. Smith, C. R. Knowles and F. Rinaldi, Acta Cristallografica, 17 (1964) 374.
J. W. Smith, J. Chem. Soc., (1964) 3759.
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Colantuono, A., Dal Vecchio, S., Mascolo, G. et al. Dilatometric behaviour of chabazite. Journal of Thermal Analysis 47, 281–289 (1996). https://doi.org/10.1007/BF01982707
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DOI: https://doi.org/10.1007/BF01982707