Abstract
AbstractThe crystal structure of pollucite (ANA) (Cs,Na)AlSi2O6is characterized by single-crystal X-ray diffractometry. The space groupC2/c,monoclinic, is found to be the most probable space group for this mineral based on the systematic absences of reflections. Cesium ions or water molecules are disordered at the center of a channel and are slightly apart from the special position. This is the origin of symmetry breaking and the space group becomes lower fromIa-3d(analcime) toC2/c. Sodium ions or vacancies are located at the contact point of the channel. No ordering of aluminum is observed in the pollucite structure.
Subject
Inorganic Chemistry,Condensed Matter Physics,General Materials Science
Cited by
20 articles.
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