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Periclase-Chromite Refractory Decomposition by a Coal – Gas Medium During Copper Sulfide Raw Material Processing

Authors
  • Klyushnikov, A. M.1
  • Selivanov, E. N.1
  • Pikulin, K. V.1
  • Belyaev, V. V.2
  • Lebed’, A. B.2
  • Udoeva, L. Yu.1
  • 1 Russian Academy of Sciences, Institute of Metallurgy, Ural Branch, Ekaterinburg, Russia , Ekaterinburg (Russia)
  • 2 Ural Mining and Metallurgical Complex (UMMC) Technical University, Verkhnyaya Pyshma, Sverdlovsk Oblast, Russia , Verkhnyaya Pyshma (Russia)
Type
Published Article
Journal
Refractories and Industrial Ceramics
Publisher
Springer US
Publication Date
Mar 01, 2019
Volume
59
Issue
6
Pages
642–647
Identifiers
DOI: 10.1007/s11148-019-00288-z
Source
Springer Nature
Keywords
License
Yellow

Abstract

The composition and structure of periclase-chromite refractories contacting the coal–gas atmosphere of copper-sulfide-ore smelting furnaces were studied. Combined effects of high-temperature suspensions of enriched copper concentrate and SO2 altered the chemical composition of the refractory surface and inner layers. The impurity contents (wt%) reached Fe 54.0, Cu 7.2, Zn 6.4, and S 1.8. Saturation of the surface layer with iron and nonferrous-metal oxides decreased its porosity and promoted the formation of low-melting compounds and eutectics. The periclase-chromite refractories were decomposed by exfoliation of layers with filled pores during alternating heat—cool cycles because of the different linear thermal expansion coefficients of the phases. The surface layer of spent refractories should be mechanically removed for recycling. The remaining part is suitable for producing refractory powders for various purposes.

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