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Growth of massive cementite layers; thermodynamic parameters and kinetics

Massive, pure cementite layers were grown on ferrite substrates by nitrocarburising in a dedicated NH(3)/H(2)/CO/N(2) containing gas atmosphere at temperatures in the range of 783–843 K. From the parabolic layer-growth constants, an “apparent” activation energy for cementite-layer growth of 109 ± 12...

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Detalles Bibliográficos
Autores principales: Nikolussi, Marc, Leineweber, Andreas, Mittemeijer, Eric Jan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer US 2009
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8319907/
https://www.ncbi.nlm.nih.gov/pubmed/34341611
http://dx.doi.org/10.1007/s10853-008-3160-6
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author Nikolussi, Marc
Leineweber, Andreas
Mittemeijer, Eric Jan
author_facet Nikolussi, Marc
Leineweber, Andreas
Mittemeijer, Eric Jan
author_sort Nikolussi, Marc
collection PubMed
description Massive, pure cementite layers were grown on ferrite substrates by nitrocarburising in a dedicated NH(3)/H(2)/CO/N(2) containing gas atmosphere at temperatures in the range of 783–843 K. From the parabolic layer-growth constants, an “apparent” activation energy for cementite-layer growth of 109 ± 12 kJ/mol was obtained. This “apparent” activation energy can be subdivided into a positive contribution due to the activation energy for (tracer) diffusion of carbon in cementite and a negative contribution due to the temperature dependence of the difference of the carbon activity in cementite at the surface and at the interface cementite/ferrite.
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spelling pubmed-83199072021-07-29 Growth of massive cementite layers; thermodynamic parameters and kinetics Nikolussi, Marc Leineweber, Andreas Mittemeijer, Eric Jan J Mater Sci Article Massive, pure cementite layers were grown on ferrite substrates by nitrocarburising in a dedicated NH(3)/H(2)/CO/N(2) containing gas atmosphere at temperatures in the range of 783–843 K. From the parabolic layer-growth constants, an “apparent” activation energy for cementite-layer growth of 109 ± 12 kJ/mol was obtained. This “apparent” activation energy can be subdivided into a positive contribution due to the activation energy for (tracer) diffusion of carbon in cementite and a negative contribution due to the temperature dependence of the difference of the carbon activity in cementite at the surface and at the interface cementite/ferrite. Springer US 2009-02-01 2009 /pmc/articles/PMC8319907/ /pubmed/34341611 http://dx.doi.org/10.1007/s10853-008-3160-6 Text en © The Author(s) 2008 https://creativecommons.org/licenses/by-nc/2.0/Open AccessThis is an open access article distributed under the terms of the Creative Commons Attribution Noncommercial License (https://creativecommons.org/licenses/by-nc/2.0 (https://creativecommons.org/licenses/by-nc/2.0/) ), which permits any noncommercial use, distribution, and reproduction in any medium, provided the original author(s) and source are credited.
spellingShingle Article
Nikolussi, Marc
Leineweber, Andreas
Mittemeijer, Eric Jan
Growth of massive cementite layers; thermodynamic parameters and kinetics
title Growth of massive cementite layers; thermodynamic parameters and kinetics
title_full Growth of massive cementite layers; thermodynamic parameters and kinetics
title_fullStr Growth of massive cementite layers; thermodynamic parameters and kinetics
title_full_unstemmed Growth of massive cementite layers; thermodynamic parameters and kinetics
title_short Growth of massive cementite layers; thermodynamic parameters and kinetics
title_sort growth of massive cementite layers; thermodynamic parameters and kinetics
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8319907/
https://www.ncbi.nlm.nih.gov/pubmed/34341611
http://dx.doi.org/10.1007/s10853-008-3160-6
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