Abstract
Anisotropic diffusion is described by a tensor of diffusivities, D αβ, which may be composition dependent leading to nonlinear anisotropic diffusion. In this work the practical problem of reconstructing such a tensor for Na-K interdiffusion in potassium-rich alkali feldspar in the composition range 0.85 ≤ X Or ≤ 1.00 is addressed. Gem quality sanidine with an initial composition of X Or = 0.85 was exchanged with KCl salt melt at 850°C and ≈1 bar. The diffusivity tensor D αβ(X Or) and its composition dependence was reconstructed from composition profiles produced by cation exchange in six different crystallographic directions using a generalization of the Boltzmann approach. Na-K interdiffusion in potassium-rich alkali feldspar is considerably anisotropic and composition dependent. The principal axes of the diffusivity tensor representing the directions of highest and lowest diffusivity lie in the a-c plane with highest diffusivity parallel to the [101] direction, lowest diffusivity perpendicular to the (101) plane, and the direction with intermediate diffusivity parallel to the crystallographic b-axis. All diffusivities D αβ(X Or) increase as X Or tends to unity. Our main result is given in the form of numerical values for all components of the D αβ(X Or) tensor for 0.85 ≤ X Or ≤ 1.
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 1284-1299 |
| Seitenumfang | 16 |
| Fachzeitschrift | American Journal of Science: an international earth science journal |
| Jahrgang | 314 |
| Ausgabenummer | 9 |
| DOIs | |
| Publikationsstatus | Veröffentlicht - Nov. 2014 |
ÖFOS 2012
- 105116 Mineralogie
- 105120 Petrologie
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