Diffusion path during internal displacement reactions in multi-component oxides: Reaction between Fe and (Co,Mg)TiO3 solid solution at 1273K
| Autor: | Brian R. Sundlof, K. T. Jacob, S. N. S. Reddy |
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| Rok vydání: | 2011 |
| Předmět: |
Precipitation (chemistry)
Chemistry Diffusion Metallurgy Alloy Analytical chemistry Oxide Materials Engineering (formerly Metallurgy) General Chemistry engineering.material Condensed Matter Physics Metal chemistry.chemical_compound visual_art engineering visual_art.visual_art_medium General Materials Science Ilmenite Stoichiometry Solid solution |
| Zdroj: | Solid State Ionics. 182:1-7 |
| ISSN: | 0167-2738 |
| Popis: | The reaction between Fe foil and a disc of ilmenite solid solution (Co-0.48 Ni-0.52) TiO3 was studied at 1273 K. At the metal/oxide interface, the displacement reaction, Fe + (Co,Mg)TiO3 = Co + (Fe,Mg)TiO3 occurs, resulting in an ilmenite solid solution containing three divalent cations. Ferrous ions diffuse into the oxide solid solution and cause the precipitation of Co-Fe alloy as discrete particles inside the oxide matrix. The morphology of the product layer was characterized by SEM. Only two phases, alloy and ilmenite, were detected in the reaction zone. This suggests that the local flux condition imposed by ilmenite stoichiometry (Co + Fe + Mg):Ti = 1:1] was satisfied during the reactive diffusion: (J(Co) + J(Fe) + J(Mg)) = J(Ti). The composition of the alloy and the oxide was determined using EPMA as a function of distance in the direction of diffusion. Although Mg does not participate in the displacement reaction, its composition in the ilmenite phase was found to be position dependent inside the reaction zone. The up-hill diffusion of inert Mg is caused by the development of chemical potential gradients as a result of displacement reaction. The evolution of composition gradients inside the reaction zone and the diffusion path in a ternary composition diagram of the system CoTiO3-FeTiO3-MgTiO3 are discussed. (C) 2010 Elsevier B.V. All rights reserved. |
| Databáze: | OpenAIRE |
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