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Disordered kalsilite KAlSiO4.
Aleksandar Kremenović1, Predrag Vulić1
1Laboratory of Crystallography, Faculty of Mining and Geology, University of Belgrade, Đušina 7, 11000 Belgrade, Serbia.
Disordered kalsilite (KAlSiO4) shows undefined tetrahedral directionality within its building units. This structural disorder leads to unique X-ray diffraction extinction conditions, differing from ordered kalsilite.
Area of Science:
- Mineralogy
- Crystallography
- Materials Science
Background:
- Kalsilite (KAlSiO4) is a potassium aluminium orthosilicate mineral.
- Understanding the structural disorder in kalsilite is crucial for its characterization.
- Previous studies have focused on ordered kalsilite structures.
Purpose of the Study:
- To investigate the X-ray powder diffraction pattern of disordered kalsilite.
- To define the structural characteristics of disordered kalsilite, specifically the (Al,Si)O4 tetrahedra.
- To elucidate the impact of disorder on crystallographic extinction conditions.
Main Methods:
- X-ray powder diffraction analysis was employed.
- The study focused on analyzing the diffraction patterns corresponding to the disordered state of kalsilite.
- Crystallographic principles were used to interpret the observed patterns and structural features.
Main Results:
- The directionality of (Al,Si)O4 tetrahedra within six-membered tetrahedral ring (S6R) units could not be definitively determined.
- An undefined sequence of up (U) and down (D) tetrahedral directionalities is required to describe the S6R units.
- Disordered kalsilite exhibits distinct extinction conditions compared to ordered kalsilite (space group P63).
- Systematic absences of h0l and hhl reflections with l = 2n + 1 were observed in disordered kalsilite.
Conclusions:
- The disordered state of kalsilite is characterized by ambiguous tetrahedral orientation within S6R units.
- The observed extinction conditions provide a fingerprint for identifying disordered kalsilite.
- This research contributes to a deeper understanding of structural disorder in silicate minerals.
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