Carbonization of α-Fe upon mechanical alloying

Methods of thermomagnetic analysis (TMA) and Mössbauer spectrometry ( 57 Fe) have been used to study the processes of the carburizing of α-Fe under the conditions of mechanical milling in a medium of liquid hydrocarbons. It has been established that, under the chosen conditions of the mechanical syn...

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Published in:Physics of metals and metallography Vol. 115; no. 1; pp. 53 - 68
Main Authors: Barinov, V. A., Tsurin, V. A., Kazantsev, V. A., Surikov, V. T.
Format: Journal Article
Language:English
Published: Boston Springer US 2014
Springer
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Summary:Methods of thermomagnetic analysis (TMA) and Mössbauer spectrometry ( 57 Fe) have been used to study the processes of the carburizing of α-Fe under the conditions of mechanical milling in a medium of liquid hydrocarbons. It has been established that, under the chosen conditions of the mechanical synthesis of carbides, the process of carbonization at T < 375 K occurs through the decomposition of the deformation-induced martensite, i.e., the supersaturated bct solid solution α″-Fe(C) with the formation of transitional hcp ε and ε′ phases that precede the formation of cementite. The milling of the metallic iron in the toluene medium substantially enhances the catalytic capability of disperse powders of α-Fe in the process of conversion of cyclic structures of hydrocarbons into other chemical forms. The increase in the dispersity of the iron powder to a nanocrystalline state leads to an increase in the chemical activity of carbon and an increase in the rate of diffusion sufficient for the formation in the Fe-C mixture of both primary cementite (θ′) with an anomalously low Curie temperature T C (θ′)(first stage) and secondary cementite (θ″) at the second stage of mechanosynthesis. The parameters of hyperfine interactions have been calculated for a number of synthesized carbides. It has been shown that the change in the carbon concentration in iron carbides is determined by the following inequality: c C (θ′) > c C (ε) > c C (ε′). The boundary of the temperature stability of cementite has been established. The effect of the decomposition of the θ phase (Fe 3 C) upon thermal cycling θ ⇔ γ in the temperature range of 300 < T < 1075 K has been revealed. Based on the results obtained, a scheme of the sequence of phase transformations that occur in the Fe-C system under the conditions of low-temperature mechanosynthesis has been derived.
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ISSN:0031-918X
1555-6190
DOI:10.1134/S0031918X14010025