Abstract
Oxygen permeation flux through La0.7Ca0.3CrO3 was determined by an electrochemical method. Yttria-stabilized zirconia (YSZ) was used as an oxygen pump/sensor to apply an oxygen potential gradient over the sample, and the steady state current was recorded. The oxygen vacancy diffusion coefficient, Dv, was determined to be 1 × 10-5 cm2 s-1 assuming a random defect model. The tracer exchange experiment was performed at 1273 K in 18O enriched O2 (0.2 bar), and the sample was analyzed by a depth profiling and imaging technique using a secondary ion mass spectrometer (SIMS). The existence of fast diffusion paths along grain boundaries was confirmed. The bulk tracer diffusion coefficient, D*, was calculated to be 2 × 10-12 cm2 s-1 in air, which was about 6 times higher than that expected from the electrochemical measurement.
Original language | English |
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Pages (from-to) | 201-207 |
Number of pages | 7 |
Journal | Solid State Ionics |
Volume | 79 |
Issue number | C |
DOIs | |
Publication status | Published - 1995 Jul |
Externally published | Yes |
Keywords
- Grain boundary diffusion
- Lanthanum cromite
- Oxygen permeation
- SIMS
- Tracer diffusion
ASJC Scopus subject areas
- Chemistry(all)
- Materials Science(all)
- Condensed Matter Physics