摘要
The oxidation kinetics of Panzhihua ilmenite was studied in a fluidized bed in the temperature range of 1053-1153 K. Within this temperature interval, the reaction can be expressed: From the experimental results, it was clarified that the intrinsic chemical reaction is the rate-controlling step.
The oxidation kinetics of Panzhihua ilmenite was studied in a fluidized bed in the temperature range of 1053-1153 K. Within this temperature interval, the reaction can be expressed: From the experimental results, it was clarified that the intrinsic chemical reaction is the rate-controlling step.
