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Liquidus-solidus phase relations in the system CaO-CrO-Cr sub 2 O sub 3 -SiO sub 2

Journal Article · · Journal of the American Ceramic Society; (United States)
 [1];  [2]
  1. Council for Mineral Technology, Randburg, 2125 (ZA)
  2. College of Earth and Mineral Sciences, Pennsylvania State Univ., University Park, PA (US)

This paper reports on phase relations in the system CaO-chromium oxide-SiO{sub 2} were determined in equilibrium with metallic chromium and at various oxygen pressures in the range of {approximately}10{sup {minus}10} to 10{sup {minus}13} atm. Two ternary phases occur on the liquidus surface in equilibrium with metallic chromium, viz, the garnet Ca{sub 3}Cr{sub 2}Si{sub 3}O{sub 12} (uvarovite), and CaCrSi{sub 4}O{sub 10} of the gillespite-type structure and in which essentially all the chromium is present in the divalent state (Cr{sup 2+}). Furthermore, a previously reported binary calcium chromite phase X of approximate composition (Ca{sup 0.4}Cr{sub 0.6})Cr{sub 2}O{sub 4} is stable also on the liquidus surface of the present system. The lowest liquidus and solidus temperatures in the system under these conditions (contact with metallic chromium) are significantly lower (by 100{degree} to 200{degree}C, depending on Cao/SiO{sub 2} ratios of the melts) than those for the same system in air. Furthermore, there is considerable solid solution of chromium oxide in lime (CaO) and the various crystalline calcium silicates (pseudowollastonite, CaSiO{sub 3}; Rankinite, Ca{sub 3}Si{sub 2}O{sub 7}; dicalcium silicate, Ca{sub 2}SiO{sub 4}; tricalcium silicate, Ca{sub 3}SiO{sub 5}), presumably by partial substitution of Cr{sup 2+} for Ca{sup 2+} toward hypothetical chromium analogs of each CaO-containing phase, particularly in lime and Ca{sub 2}SiO{sub 4}.

OSTI ID:
7279877
Journal Information:
Journal of the American Ceramic Society; (United States), Journal Name: Journal of the American Ceramic Society; (United States) Vol. 75:6; ISSN JACTA; ISSN 0002-7820
Country of Publication:
United States
Language:
English