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Phase transformations in the carbon system

  • Physical Chemistry
  • Published:
Bulletin of the Academy of Sciences of the USSR, Division of chemical science Aims and scope

Conclusions

  1. 1.

    It is suggested that the diamond-graphite transitions can proceed either directly or through intermediate metastable phases.

  2. 2.

    The conditions required for thin-layer graphite-to-diamond transition are determined by the depth and mutual orientation of the layers.

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Literature cited

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Author information

Authors and Affiliations

  1. Institute of Physical Chemistry, Academy of Sciences of the USSR, Moscow

    D. V. Fedoseev, V. P. Varnin, A. A. Kochergina, B. V. Deryagin, S. P. Vnukov & I. G. Teremetskaya

Authors
  1. D. V. Fedoseev
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  2. V. P. Varnin
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  3. A. A. Kochergina
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  4. B. V. Deryagin
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  5. S. P. Vnukov
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  6. I. G. Teremetskaya
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Additional information

Translated from Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, No. 10, pp. 2220–2225, October, 1978.

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Fedoseev, D.V., Varnin, V.P., Kochergina, A.A. et al. Phase transformations in the carbon system. Russ Chem Bull 27, 1961–1965 (1978). https://doi.org/10.1007/BF00946506

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  • DOI: https://doi.org/10.1007/BF00946506

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