z-logo
Premium
Elastic Properties of Mullite Single Crystals up to 1400°C
Author(s) -
Schreuer Jürgen,
Hildmann Bernd,
Schneider Hartmut
Publication year - 2006
Publication title -
journal of the american ceramic society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.9
H-Index - 196
eISSN - 1551-2916
pISSN - 0002-7820
DOI - 10.1111/j.1551-2916.2006.00921.x
Subject(s) - resonant ultrasound spectroscopy , thermal expansion , atmospheric temperature range , thermoelastic damping , materials science , orthorhombic crystal system , softening , mullite , volume (thermodynamics) , analytical chemistry (journal) , mineralogy , thermodynamics , composite material , thermal , chemistry , crystallography , crystal structure , physics , elastic modulus , ceramic , chromatography
Elastic constants and their temperature derivatives of orthorhombic 2/1‐mullite single crystals were determined using resonant ultrasound spectroscopy between ambient temperature and 1400°C in air. The values at room temperature given in GPa were c 11 =279.5(4), c 22 =234.9(2), c 33 =360.6(3), c 44 =109.49(7), c 55 =74.94(4), c 66 =79.89(4), c 12 =103.1(2), c 13 =96.1(3), and c 23 =135.6(1). The high temperature ultrasound data sets were corrected for thermal expansion effects using the coefficients, which were measured in the range −170° to 1400°C by means of dilatometry. Up to about 1000°C, the temperature evolution of the elastic stiffnesses was linear and the corresponding thermoelastic constants T ij =d log c ij /d T given in 10 −6 °C −1 were T 11 =−100(2), T 22 =−126(2), T 33 =−78.2(6), T 44 =−75.3(7), T 55 =−81.3(9), T 66 =−113(1), T 12 =−153(3), T 13 =−94(4), and T 23 =−47(2). While the temperature derivatives of the longitudinal stiffnesses and the transverse interaction coefficients remained linear, the shear resistances c 44 , c 55 , and c 66 displayed an increased softening above about 1000°C, which was accompanied by a rapidly increasing ultrasound dissipation. In the same temperature region, small, but clearly recognizable discontinuities in the longitudinal and in the volume thermal expansion coefficients occurred. Taking into account the behavior of the heat capacity, the observed anomalies may indicate a glass‐like transition of mullite above about 1000°C. An unexpected peak in the ultrasound dissipation at about 70°C was most likely caused by anelastic point defect relaxations.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here