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Structure evolution in periclase-carbon refractories at elevated temperatures

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Conclusions

At high temperatures, periclase-carbon systems exhibit a significant change in their phase composition and spatial distribution of the oxide and the carbonaceous components. The structure evolution of the periclase-carbon refractories occurs due to sintering of the mineralogical filler under the conditions involving a change in the volumetric proportions of the oxide and the carbonaceous phases because of the oxidation-reduction reactions.

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Authors and Affiliations

  1. Lensovet Leningrad Technological Institute, USSR

    S. A. Suvorov, D. E. Denisov, V. G. Borisov, E. Ya. Shapiro, L. M. Myznikova & S. V. Kazakov

  2. All-Union Institute of Refractories, USSR

    S. A. Suvorov, D. E. Denisov, V. G. Borisov, E. Ya. Shapiro, L. M. Myznikova & S. V. Kazakov

Authors
  1. S. A. Suvorov
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  2. D. E. Denisov
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  3. V. G. Borisov
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  4. E. Ya. Shapiro
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  5. L. M. Myznikova
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  6. S. V. Kazakov
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Additional information

Translated from Ogneupory, No. 1, pp. 10–13, January, 1988.

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Suvorov, S.A., Denisov, D.E., Borisov, V.G. et al. Structure evolution in periclase-carbon refractories at elevated temperatures. Refractories 29, 12–16 (1988). https://doi.org/10.1007/BF01386597

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  • DOI: https://doi.org/10.1007/BF01386597

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