Hostname: page-component-77c89778f8-gq7q9 Total loading time: 0 Render date: 2024-07-19T01:55:55.862Z Has data issue: false hasContentIssue false

Roggianite: revised chemical formula and zeolitic properties

Published online by Cambridge University Press:  05 July 2018

E. Passaglia
Affiliation:
Istituto di Mineralogia, Universita' di Ferrara, Corso Ercole I d'Este 32, 44100 Ferrara, Italy
Giovanna Vezzalini
Affiliation:
Istituto di Mineralogia e Petrologia, Universita' di Modena, via S. Eufemia 19, 41100 Modena, Italy

Abstract

The holotype roggianite from Alpe Rosso (Novara, Italy) has been chemically re-analysed using modern analytical procedures (microprobe, atomic absorption spectrophotometer, TG analyses) and tested for its zeolitic behaviour. When compared with that given in the original description, the new chemical composition shows an appreciable amount of Be and a different Si/Al ratio. On the basis of its structural data, the chemical formula here proposed for roggianite is: (Ca14.24Sr0.01Na0.37K0.56)Σ15.18[(Be5.29Al14.92Si27.79)Σ48O89.96(OH)14](OH)2·33.68H2O

An accurate powder pattern, index taking into account the structural factors, is also given. Since the mineral showed an almost complete rehydration after heating to 750°C and an appreciable ion exchange capacity, it must be considered as belonging to the zeolitic group of minerals, and, in this frame, it represents the first and up to now the only zeolite with Be as fundamental constituent and, like partheite, with OH groups in the framework.

Type
Mineralogy
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1988

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Albee, A.L. and Ray, L. (1970) Correction factors for electron-probe microanalysis of silicates, oxides, carbonates, phosphates and sulphates. Anal. Chem. 42, 1408-14.CrossRefGoogle Scholar
Alberti, A. (1976) The use of structure factors in the refinement of unit-cell parameters from powder diffraction data. J. Appl. Crystallogr. 9, 373-4.CrossRefGoogle Scholar
Donnay, G. and Allmann, R. (1970) How to recognize O2-, OH- , and H20 in crystal structures determined by X-rays. Am. Mineral. 55, 1003-15.Google Scholar
Engel, N. and Yvon, K. (1984) The crystal structure of partheite. Z. Kristallogr. 169, 165-75.Google Scholar
Galli, E. (1980) The crystal structure of roggianite, a zeolite-like silicate. Proc. 5th Int. Conf. Zeolites (Rees L.V.C., ed.) Heyden, London, 205-13.Google Scholar
Gard, J.A. (1969) An electron microscope and diffraction study of roggianite. Clay Mineral. 8, 112-3.CrossRefGoogle Scholar
Gottardi, G. and Galli, E. (1985) Natural zeolites. Springer- Verlag. Berlin-Heidelberg.CrossRefGoogle Scholar
Jones, J.B. (1968) Al-O and Si-O tetrahedral distances in aluminosilicate framework structures. Acta Crystallogr. B24, 355-8.CrossRefGoogle Scholar
Passaglia, E. (1969) Roggianite a new silicate mineral. Clay Mineral. 8, 107-11.CrossRefGoogle Scholar
Vezzalini, G. and Mattioli, V. (1979) Secondo ritrovammento della roggianite. Period. Mineral. 48, 15-20.Google Scholar
Ziebold, T.O. and Ogilvie, R.E. (1964) An empirical method for electron microanalysis. Anal. Chem. 36, 322-7.CrossRefGoogle Scholar