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Framework 'interstitial' oxygen in La(10)(GeO(4))(5-)(GeO(5))O(2) apatite electrolyte
Stevin S Pramana1, Wim T Klooster, T J White
1Nanyang Technological University, School of Materials Science and Engineering, 50 Nanyang Avenue, 639798 Singapore.
Oxygen vacancies in apatite materials facilitate low-temperature oxygen conduction, crucial for solid-oxide fuel cells. New research reveals interstitial oxygen in La(10)(GeO(4))(6)O(3) apatites drives ion migration through structural changes.
Area of Science:
- Materials Science
- Solid-State Chemistry
- Electrochemistry
Background:
- Apatite materials exhibit oxygen conduction at low temperatures, making them promising solid electrolytes for solid-oxide fuel cells.
- The precise defect structures governing ion migration in these apatites, particularly inter-tunnel mobility, remain incompletely understood.
Purpose of the Study:
- To elucidate the defect structure responsible for oxygen ion migration in apatite electrolytes.
- To investigate the role of interstitial oxygen and its diffusion mechanism in La(10)(GeO(4))(6)O(3) apatite.
Main Methods:
- Neutron powder diffraction was employed to analyze the crystal structure of stoichiometric La(10)(GeO(4))(6)O(3).
- Structural analysis focused on identifying the location and concentration of oxygen defects and their impact on ion mobility.
Main Results:
- The stoichiometric compound is better described as La(10)(GeO(4))(5-)(GeO(5))O(2) apatite, indicating a significant concentration of interstitial oxygen within channel walls.
- Interstitial oxygen atoms are proposed to act as a reservoir for migrating ions, facilitating inter-tunnel oxygen diffusion.
Conclusions:
- The migration mechanism involves transient conversion of GeO(4) tetrahedra to GeO(5) trigonal bipyramids, driven by interstitial oxygen.
- This structural flexibility may be a general characteristic of oxide apatites, impacting their performance as solid electrolytes.
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