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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4816

Authors: Iezzi, G.*
Title: The thermal behavior of richterite
Title of journal: American Mineralogist
Series/Report no.: /93(2008)
Publisher: Mineralogical Society of America
Issue Date: Oct-2008
Keywords: amphibole
Debye model
Abstract: The thermal behavior of synthetic richterite ANaB(NaCa)CMg5TSi8O22(OH)2, crystallized at 800 °C and 0.35 GPa under hydrothermal conditions, was studied by serial powder diffraction experiments using synchrotron radiation between 123 and 873 K. The a, b, and β cell parameters show a non-linear behavior, whereas the c parameter shows a linear trend; values of the saturation temperature θs are 410(3), 215(2), and 300(2) K for a, b, and asinβ, respectively. The axial expansion pattern below room temperature is αb > αc > αa, whereas above room T it is αb > αa > αc, the difference being related to the different saturation temperatures of the individual cell parameters. The thermal expansion was modeled following the Debye approximation for the density-of-state of phonons; the refined parameters are V0 = 908.20 (0.04) Å3, k = 1 (4), Q0 =32 (2) MJ, and the Debye temperature θD = 586(31) K. The non-linear behavior at low T is well described without systematic differences between the data and the model. The volume thermal expansion coefficient αV changes significantly with temperature, also at temperatures higher than room temperature. It is suggested that this may occur also in other amphiboles and pyroxenes, requiring critical re-examination of the available data. A comparison of the strain tensor for the thermal expansion between amphiboles and pyroxenes shows that in amphiboles the major deformation occurs onto the (010) plane, whereas in pyroxenes it occurs along the b axis. Moreover, the major deformation on (010) in Ca-bearing pyroxenes occurs along the bond of the M2 cation with the furthermost O3 atoms, whereas in compositionally related Ca-amphiboles (i.e., tremolite) it occurs in a direction rotated by 10–20° to a*, i.e., in a direction not corresponding to that of the M4-O5 bonds. It is proposed that the M4 polyhedron contributes less to the thermal deformation of amphibole than the M2 polyhedron contributes to the thermal deformation of pyroxene.
Appears in Collections:04.01.04. Mineral physics and properties of rocks
Papers Published / Papers in press

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