The low-temperature behavior of a natural kalsilite (ideal formula KAlSiO4) with P31c symmetry has been investigated by in situ single-crystal diffraction. A series of intensity data collections and structural refinements have been performed at 298, 250, 200, 150, and 100 K on decreasing temperature, and 175, 225, and 275 K on increasing T. The variations of the unit-cell parameters of kalsilite as a function of T are continuous, and show no evidence of any phase transitions or thermo-elastic anomalies in this temperature range. An expansion is observed along [0001] with decreasing temperature. The axial and volume thermal expansion coefficients (αj = lj–1⋅∂lj/∂T, αV = V–1⋅∂V/∂T) between 298 and 100 K, calculated by weighted linear regression through the data points, are αa = αb = 1.30(6)·10–5, αc = –1.5(1)·10–5, αV = 1.1(2)·10–5 K–1. The main structural change on decreasing temperature is a cooperative anti-rotation of tetrahedra forming the six-membered rings lying parallel to (0001). This tetrahedral rotation is coupled with a change in the distances between the extra-framework cations and the framework O atoms. A small decrease in the tetrahedral tilts perpendicular to [0001] is responsible for the negative thermal expansion along [0001]; the implications of these mechanisms for thermal expansion in nephelines and kalsilites are discussed.

Low-temperature behaviour of natural kalsilite with P31c symmetry: an in-situ single-crystal X-ray diffraction study / G. D. Gatta, R. J. Angel, M. A. Carpenter. - In: AMERICAN MINERALOGIST. - ISSN 0003-004X. - 95:7(2010 Jul), pp. 1027-1034. [10.2138/am.2010.3478]

Low-temperature behaviour of natural kalsilite with P31c symmetry: an in-situ single-crystal X-ray diffraction study

G.D. Gatta
Primo
;
2010

Abstract

The low-temperature behavior of a natural kalsilite (ideal formula KAlSiO4) with P31c symmetry has been investigated by in situ single-crystal diffraction. A series of intensity data collections and structural refinements have been performed at 298, 250, 200, 150, and 100 K on decreasing temperature, and 175, 225, and 275 K on increasing T. The variations of the unit-cell parameters of kalsilite as a function of T are continuous, and show no evidence of any phase transitions or thermo-elastic anomalies in this temperature range. An expansion is observed along [0001] with decreasing temperature. The axial and volume thermal expansion coefficients (αj = lj–1⋅∂lj/∂T, αV = V–1⋅∂V/∂T) between 298 and 100 K, calculated by weighted linear regression through the data points, are αa = αb = 1.30(6)·10–5, αc = –1.5(1)·10–5, αV = 1.1(2)·10–5 K–1. The main structural change on decreasing temperature is a cooperative anti-rotation of tetrahedra forming the six-membered rings lying parallel to (0001). This tetrahedral rotation is coupled with a change in the distances between the extra-framework cations and the framework O atoms. A small decrease in the tetrahedral tilts perpendicular to [0001] is responsible for the negative thermal expansion along [0001]; the implications of these mechanisms for thermal expansion in nephelines and kalsilites are discussed.
Kalsilite, feldspathoids, low temperature, single-crystal X-ray diffraction, thermal expansion
Settore GEO/09 - Georisorse Miner.Appl.Mineral.-Petrogr.per l'amb.e i Beni Cul
Settore GEO/06 - Mineralogia
lug-2010
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/145003
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