Anelastic behaviour of leucite KAlSi2O6
Anelastic behaviour of leucite KAlSi2O6
复制标题
白榴石 KAlSi2O6 的滞弹性行为
DOI:
10.1016/j.msea.2006.02.233
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发表时间:
2006
期刊:
影响因子:
6.4
通讯作者:
S. Redfern
中科院分区:
文献类型:
--
作者:
J. Walsh;R. Harrison;S. Redfern
An examination of the anelastic response of leucite, KAlSi2O6, to frequency modulated stress is presented. Leucite is a naturally occurring open framework aluminosilicate closely related to analcime (a zeolite compound) and is found in the earth's crust. It shows two phase transitions at [Formula: see text] 665°C and [Formula: see text] 645°C, from cubic Ia3d through I41/acd to I41/a. Consequently the low temperature I41/a phase contains both lamellar and merohedral twins; the intermediate I41/acd phase contains lamellar twins only. Leucites typically show a high density of twin walls. Recent studies have shown that lamellar microstructures can give rise to anelastic softening via twin wall motion [R.J. Harrison, S.A.T. Redfern, J. Appl. Phys. 95 (2004) 1706–1717; R.J. Harrison, S.A.T. Redfern, E.K.H. Salje, Phys. Rev. B 69 (2004) 144101-1–144101-10; R.J. Harrison, S.A.T. Redfern, J. Street, Am. Mineral. 88 (2003) 574–582]. This could be a mechanism for seismic attenuation in crustal and mantle rocks. We propose that this process also occurs in leucite on the basis of results of dynamical mechanical analysis. A frequency modulated stress (0.4–16Hz) was applied in three point bend geometry to single crystals of leucite containing twins. The dynamic modulus and tanδ functions have been measured, though these are partially obscured by the presence of the higher temperature phase transition. The apparent activation energies for twin wall motion (600kJmol−1or more) are unusually high, suggesting possible dependence on silicon diffusion within the aluminosilicate framework. Softening of the modulus in the high-temperature cubic phase, on cooling towards the Ia3d to I41/acd transition, is consistent with coupling to optic modes which show strong dispersion with three phonon branches softening equally in all directions.