The dehydration behavior of yugawaralite has been studied by single crystal x-ray diffraction on three samples dehydrated under vacuum at 20, 150 and 200°C, resp. Yugawaralite held in vacuum at room temp. (r.T) - even for relatively long times - does not show noticeable structural changes with respect to untreated samples. The Ca atom remains coordinated to four framework oxygen atoms and to four water oxygens; two of these water mols. are disordered with two alternative oxygen positions. Yugawaralite heated at 150°C is characterized by a water loss as high as 54%, with all the residual water mols. in two fully occupied sites. The Ca atoms are 6-coordinated by four framework oxygens and the two residual water mols. The framework undergoes only minor modifications. The crystal heated at 200°C shows a further 50% loss of the residual water present at 150°C and a collapsing of the channel system: a sudden decrease of unit cell vol. occurs (about 13%), the cell parameter a is doubled, the space group changes from Pc to Pn, and the structure is strongly squashed. Owing to the doubling of parameter a, there are two sym. independent Ca sites; both are 6-coordinated, but now with five framework oxygens and one water mol.

Structural modifications induced by dehydration in yugawaralite / A., Alberti; S., Quartieri; Vezzalini, Maria Giovanna. - STAMPA. - 84:(1994), pp. 637-644. (Intervento presentato al convegno 10th International Zeolite Conference tenutosi a GARMISCH PARTENKIR, GERMANY nel JUL 17-22, 1994).

Structural modifications induced by dehydration in yugawaralite

VEZZALINI, Maria Giovanna
1994

Abstract

The dehydration behavior of yugawaralite has been studied by single crystal x-ray diffraction on three samples dehydrated under vacuum at 20, 150 and 200°C, resp. Yugawaralite held in vacuum at room temp. (r.T) - even for relatively long times - does not show noticeable structural changes with respect to untreated samples. The Ca atom remains coordinated to four framework oxygen atoms and to four water oxygens; two of these water mols. are disordered with two alternative oxygen positions. Yugawaralite heated at 150°C is characterized by a water loss as high as 54%, with all the residual water mols. in two fully occupied sites. The Ca atoms are 6-coordinated by four framework oxygens and the two residual water mols. The framework undergoes only minor modifications. The crystal heated at 200°C shows a further 50% loss of the residual water present at 150°C and a collapsing of the channel system: a sudden decrease of unit cell vol. occurs (about 13%), the cell parameter a is doubled, the space group changes from Pc to Pn, and the structure is strongly squashed. Owing to the doubling of parameter a, there are two sym. independent Ca sites; both are 6-coordinated, but now with five framework oxygens and one water mol.
1994
ZEOLITES AND RELATED MICROPOROUS MATERIALS: STATE OF THE ART 1994
ELSEVIER SCIENCE PUBL B V
PAESI BASSI
Structural modifications induced by dehydration in yugawaralite / A., Alberti; S., Quartieri; Vezzalini, Maria Giovanna. - STAMPA. - 84:(1994), pp. 637-644. (Intervento presentato al convegno 10th International Zeolite Conference tenutosi a GARMISCH PARTENKIR, GERMANY nel JUL 17-22, 1994).
A., Alberti; S., Quartieri; Vezzalini, Maria Giovanna
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11380/737492
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