DIFFUSION OF O-18 IN MASSIVE CR2O3 AND IN CR2O3 SCALES AT 900-DEGREES-C AND ITS RELATION TO THE OXIDATION-KINETICS OF CHROMIA FORMING ALLOYS

Citation
Sc. Tsai et al., DIFFUSION OF O-18 IN MASSIVE CR2O3 AND IN CR2O3 SCALES AT 900-DEGREES-C AND ITS RELATION TO THE OXIDATION-KINETICS OF CHROMIA FORMING ALLOYS, Oxidation of metals, 43(5-6), 1995, pp. 581-596
Citations number
18
Categorie Soggetti
Metallurgy & Metallurigical Engineering
Journal title
ISSN journal
0030770X
Volume
43
Issue
5-6
Year of publication
1995
Pages
581 - 596
Database
ISI
SICI code
0030-770X(1995)43:5-6<581:DOOIMC>2.0.ZU;2-8
Abstract
The lattice and grain-boundary diffusion coefficients of O-18 at P-O2= 0.1 atm and at 900 degrees C were determined in massive Cr2O3 and in C r2O3 scales which were grown on a Ni-30Cr alloy. The diffusion profile s were established by SIMS and analyzed considering two domains in the case of polycrystalline Cr2O3 (massive or scales), the first one rela tive to apparent diffusion and the second to grain-boundary diffusion. A ridge model is proposed for Cr2O3 scales to modify the f value, fra ction of sites associated with the grain boundary. With such a model, f is equal to 0.0006 and 0.0005 for the scales formed during 15 hr and 165 hr; respectively. The oxygen-lattice diffusion coefficients deter mined in Cr2O3 scales are in very good agreement with those in massive Cr2O3 . With some assumptions, our diffusion data lead to a calculate d parabolic oxidation constant equal to the experimental one. Scale gr owth occurs by countercurrent diffusion of oxygen and chromium, mainly by grain-boundary diffusion.