6533b870fe1ef96bd12d03a4
RESEARCH PRODUCT
Modeling of anisotropic grain growth in minerals
Lynn EvansKurt StüwePaul D. BonsTerence BarrMark Jessellsubject
Grain growthBoundary layerCondensed matter physicsFinite strain theoryGrain boundaryCrystalliteGrowth rateAnisotropyGeologySurface energydescription
The role of surface energy anisotropy during grain growth is investigated using both physical experiments on octachloropropane and numerical experiments using the Elle microstructural modelling system. In particular the effects of anisotropy on growth rates, grain shapes and lattice preferred orientations are analysed. Anisotropic growth in thin polycrystalline sheets of octachloropropane is found to systematically remove certain c-axis orientations from the sample, without obviously modifying the grain shapes. By comparison with equivalent numerical experiments, we can explain these observations with a simple boundary layer model that treats each side of each grain boundary as an independent system. The observed growth exponent in the physical experiment of 0.35 is significantly below the theoretical level of 1, and although the numerical experiments have growth rates as low as 0.68, apparently some other factor which suppresses the growth rate in the octachloropropane was also active. The anisotropy of surface energies also leads to an increase in the grain size distribution, and when it occurs in rocks with a strong pre-existing crystallographic preferred orientation, may even lead to the development of a shape preferred orientation which is completely unrelated to the shape of the finite strain ellipsoid. * Corresponding author. E-mail address: bons@mail.uni-mainz.de Accepted for publication in the "Hans Ramberg" Volume, Bulletin of the American Geological Society Bons et al. Anisotropic grain growth... 17. Januar 2000 page 2
year | journal | country | edition | language |
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2001-01-01 |