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Multicomponent diffusion in ionic crystals: theoretical model and application to combined tracer- and interdiffusion
E Petrishcheva1, L Tiede1, D Heuser1
1Department of Lithospheric Research, University of Vienna, 1090 Vienna, Austria.
A new model explains multicomponent diffusion in ionic crystals, considering both vacancy-mediated and direct exchange mechanisms. This model accurately describes sodium and potassium diffusion in alkali feldspar, revealing faster sodium diffusion.
Area of Science:
- Materials Science
- Geochemistry
- Solid-State Physics
Background:
- Multicomponent diffusion in ionic crystals is complex, involving various mechanisms.
- Understanding these mechanisms is crucial for materials science and geochemistry.
Purpose of the Study:
- To develop a comprehensive model for multicomponent diffusion in ionic crystals.
- To apply this model to Na and K diffusion in alkali feldspar.
Main Methods:
- Developed a model incorporating vacancy-mediated diffusion and binary ionic exchange.
- Applied the model to alkali feldspar crystals using K doped KCl diffusion couples.
- Annealed samples between 800-950 °C and analyzed concentration profiles using Time of Flight Secondary Ion Mass Spectrometry (ToF-SIMS).
Main Results:
- The Na self-diffusion coefficient was found to be at least 500 times higher than the K self-diffusion coefficient.
- Diffusion mediated by binary K- K exchange was necessary for accurate model fits.
- The kinetic coefficient for K-K exchange was well-constrained.
Conclusions:
- The proposed model successfully describes multicomponent diffusion in ionic crystals.
- The findings highlight the significant difference in diffusion rates between Na and K in alkali feldspar.
- Binary exchange mechanisms play a critical role in the diffusion of multiple ionic species.
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