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Comparative Mössbauer study of the aging of Fe-C and Fe-N martensites

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Abstract

The clustering-ordering synergy which forms Fe6C precipitates by aging Fe-C martensite is compared to the long-range ordering which forms Fe16N2 by aging Fe-N martensite.

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Author notes

  1. O. N. C. Uwakweh

    Present address: Department of Materials Science and Engineering, University of Cincinnati, 498 Rhodes Hall, 45221-0012, Cincinnati, OH, USA

Authors and Affiliations

  1. Laboratoire de Chimie Physique pour l'Environnement, Groupe de Spectrométrie Mössbauer, UMR 9992 CNRS, Université H. Poincaré, Nancy 1

    J. -M. R. Génin, I. Fall & O. N. C. Uwakweh

  2. Département Sciences des Matériaux, ESSTIN, 405 rue de Vandœuvre, F-54600, Villers-Nancy, France

    J. -M. R. Génin, I. Fall & O. N. C. Uwakweh

Authors
  1. J. -M. R. Génin
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  2. I. Fall
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  3. O. N. C. Uwakweh
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Génin, J.M.R., Fall, I. & Uwakweh, O.N.C. Comparative Mössbauer study of the aging of Fe-C and Fe-N martensites. Hyperfine Interact 92, 981–986 (1994). https://doi.org/10.1007/BF02065722

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  • DOI: https://doi.org/10.1007/BF02065722

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