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Growth and microstructure of iron nitride layers and pore formation in ε-Fe3N

  • C. Middendorf and W. Mader EMAIL logo
Published/Copyright: January 11, 2022

Abstract

Layers of ε-Fe3N and γ′-Fe4N on ferrite were produced by nitriding iron single crystals or rolled sheets of iron in flowing ammonia at 520 °C. The nitride layers were characterised using X-ray diffraction, light microscopy as well as scanning and transmission electron microscopy. The compound layer consists of ε-Fe3N at the surface and of γ′-Fe4N facing the ferrite. After 4 h of nitriding, pores develop in the near surface region of ε-Fe3N showing more or less open porosity. Growth of the entire compound layer as well as of the massive and the porous ε-Fe3N sublayer is diffusion-controlled and follows a parabolic growth rate. The γ′-Fe4N layer is formed as a transition phase within a narrow interval of nitrogen activity, and it shows little growth in thickness. The transformation of γ′-Fe4N to ε-Fe3N is topotactic, where the orientation of the closed-packed iron layers of the crystal structures is preserved. Determination of lattice plane spacings was possible by X-ray diffraction, and this was correlated to the nitrogen content of ε-Fe3N. While the porous layer exhibits an enhanced nitrogen content corresponding to the chemical composition Fe3N11, the massive e Fe3N layer corresponds to Fe3N1.0. The pore formation in ε-Fe3N11 is concluded to be the result of excess nitrogen atoms on non-structural sites, which have a high mobility. Therefore, recombination of excess nitrogen to molecular N2 at lattice defects is preferred in ε-Fe3N with high nitrogen content compared to stoichiometric ε-Fe3N1.0 with nitrogen on only structural sites.

Abstract

Ein Schichtsystem von Eisennitriden auf Ferrit wurde durch Nitrieren von Eiseneinkristallen und -blechen im Ammoniak-Strom bei 520 °C hergestellt und mittels Röntgenbeugung sowie lichtmikroskopisch und elektronenmikroskopisch charakterisiert. In der Verbindungsschicht, welche sich aus ε-Fe3N an der Oberfläche und γ′-Fe4N an den Ferrit grenzend zusammensetzt, entsteht nach ca. 4 h Nitrieren im oberflächennahen Bereich von ε-Fe3N ein Porensaum mit weitgehend offener Porosität. Das Wachstum der gesamten Verbindungsschicht sowie der dichten ε-Fe3N-Schicht und des Porensaums erfolgt diffusionskontrolliert nach einem parabolischen Zeitgesetz. Die γ′-Fe4N-Schicht entsteht als Übergangsphase in einem engen Intervall der Stickstoffaktivität und weist ein geringes Dickenwachstum auf. Die Umwandlung von γ′-Fe4N in ε-Fe3N erfolgt topo-taktisch unter Beibehaltung der Orientierung der dicht gepackten Eisenlagen beider Kristallstrukturen. Über die Bestimmung von Netzebenenabständen aus der Lage von Röntgenreflexen gelang der Nachweis eines erhöhten Stickstoffgehaltes im Porensaum von ε-Fe3N mit der Zusammensetzung Fe3N11 im Vergleich zur porenfreien ε-Fe3N-Schicht mit Fe3N1.0. Die Porenbildung in ε-Fe3N11 wird auf Überschuss-Stickstoffatome auf nicht-strukturellen Oktaederplätzen zurückgeführt, die eine erhöhte Beweglichkeit im Gitter besitzen und damit an Kristallfehlern mit höherer Wahrscheinlichkeit zu molekularem N2 rekom-binieren können, als dies in stöchiometrischem ε-Fe3N1.0 mit ausschließlich auf strukturellen Plätzen befindlichen Stickstoffatomen der Fall ist.


Prof. Dr. W. Mader Institut für Anorganische Chemie Römerstr. 164, D-53117 Bonn, Germany Tel.: +49 228 73 4203 Fax: +49 228 73 4205
Dedicated to Professor Dr. Dr. h. c. Manfred Rühle on the occasion of his 65th birthday

Funding statement: The authors would like to thank Dr. D. Brunner, Max-Planck-Institut für Metallforschung, Stuttgart, for supporting the iron single crystal. Financial support by the Deutsche Forschungsgemeinschaft and by the Fonds der Chemischen Industrie is gratefully acknowledged.

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Received: 2003-01-07
Published Online: 2022-01-11

© 2003 Carl Hanser Verlag, München

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