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Oxygen surface exchange and diffusion in mayenite single crystal.
Anna S Tolkacheva1, Sergey N Shkerin, Natalia M Porotnikova
1The Institute of High-Temperature Electrochemistry of the Ural Branch of the Russian Academy of Sciences, 620137 Ekaterinburg, Russia. a.s.tolkacheva@urfu.ru.
Physical Chemistry Chemical Physics : PCCP
|November 5, 2019
Summary
This study reveals new insights into oxygen diffusion in mayenite (Ca12Al14O33±δ) using an in situ isotope equilibration method. The research clarifies surface heterogeneity and challenges previous understandings of oxygen diffusion mechanisms.
Area of Science:
- Materials Science
- Solid State Chemistry
- Crystallography
Background:
- Mayenite (Ca12Al14O33±δ) is a complex oxide with potential applications in various fields.
- Understanding oxygen surface exchange and diffusion is crucial for optimizing material performance.
- Previous studies have proposed models for oxygen diffusion in mayenite, but some aspects remain debated.
Purpose of the Study:
- To investigate oxygen surface exchange and diffusion in Ca12Al14O33±δ single crystals.
- To develop and apply a novel in situ method for analyzing oxygen transport mechanisms.
- To clarify the surface heterogeneity and diffusion behavior of mayenite, particularly in the 750 °C to 850 °C range.
Main Methods:
- Utilized a unique in situ method based on isotope equilibration in the gas phase.
- Analyzed oxygen surface exchange rates and diffusion coefficients.
- Employed single crystal samples of Ca12Al14O33±δ.
Main Results:
- The interphase exchange rate and oxygen diffusion coefficient align with existing data.
- The employed method successfully isolated contributions from various exchange types, enabling surface heterogeneity estimation.
- Results contradict previous literature, indicating the 750 °C to 850 °C range is not an intermediate region for two coexisting oxygen diffusion types.
Conclusions:
- The study provides the first quantitative estimation of mayenite surface heterogeneity.
- The findings challenge established models regarding oxygen diffusion mechanisms in mayenite within the studied temperature range.
- A new model is proposed, explaining temperature-dependent properties based on near-surface layer stability.

