Abstract:process are recommended for service under the conditions of high mechanical loads and erosion (including the temperatures in the 1700-1750~ range).
CONCLUSIONSAt high temperatures, periclase-carbon systems exhfbit 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… Show more
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