Abstract
Information relating to the Ye-N-C ternary component system is essentially to be found in [1-3]. Repeated use of these data and their interpretation in research into carbonitriding processes has given them a classical status. However, for the analysis of phase equilibria in the Fe-N-C system, and in particular in the carbonitrided layer, the literature data are frequently inadequate. For this reason therefore, sometimes it is necessary to use the binary Fe-N system, which however, is by no means always justified, particularly for studying the carbonitride layer formation kinetics, the phase transitions taking place therein, and the structures and substructures.
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