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Kinetics of Carbothermal Reduction of Quartz Under Vacuum
Author(s) -
KHALAFALLA S. E.,
HAAS L. A.
Publication year - 1972
Publication title -
journal of the american ceramic society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.9
H-Index - 196
eISSN - 1551-2916
pISSN - 0002-7820
DOI - 10.1111/j.1151-2916.1972.tb11324.x
Subject(s) - carbothermic reaction , nucleation , activation energy , quartz , kinetics , oxide , chemistry , phase (matter) , alkali metal , analytical chemistry (journal) , partial pressure , graphite , mineralogy , rate equation , inorganic chemistry , materials science , metallurgy , oxygen , chromatography , physics , organic chemistry , quantum mechanics
The kinetics of reduction of 0.2 mol of –70?mesh quartz particles by 0.2 mol of graphite were determined in a batch reactor between 0.25 and 10 −0 torr. The effects of temperature, CO partial pressure, SiO 2 phase transformation, and alkali and alkaline‐earth oxide additives on the rate of reaction were studied. Increasing CO overpressure retarded carbothermal reduction. At 1400−C, addition of 5 wt% alkali oxide inhibited the reaction, whereas the same amount of alkaline‐earth oxide decreased the induction time; CaO was the best promoter. The initial reaction rate obeyed the cubic power law of nucleation growth at weight losses <15%, with an apparent activation energy of 77 kcal/mol. At higher weight losses, the Austin‐Rickett equation with an exponent near 2 was more applicable. The results are consistent with a model based on a transitory phase intermediate.

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