Zhang Lin, Zhu Yu, Yin Wanzhong, Guo Bao, Rao Feng, Ku Jiangang
College of Zijin Mining, Fuzhou University, Fuzhou 350116, Fujian, PR China.
Fuzhou University-Zijin Mining Group Joint Research Center for Comprehensive Utilization of Mineral Resources, Fuzhou 350116, PR China.
ACS Omega. 2020 Apr 9;5(15):8605-8612. doi: 10.1021/acsomega.9b04497. eCollection 2020 Apr 21.
The coal-based reduction of fayalite was characterized using thermogravimetric (TG) and differential TG methods with reduction temperatures from 1123 to 1273 K. The results of fayalite isothermal reduction indicate that the reduction process is divided two stages. The corresponding apparent activation energy was gained using the isoconversional and model-fitting methods. At the first stage, the effect of temperature on the reduction degree was not clear, and the phase boundary chemical reaction was the controlling step, with an apparent activation energy value of 175.32-202.37 kJ·mol. At the second stage, when the temperature was more than 1123 K, the conversion degree and the reaction rate increased nonlinearly with increasing temperature, and two-dimensional diffusion, three-dimensional diffusion, one-dimensional diffusion, and phase boundary-controlled reaction were the controlling stages, with an apparent activation energy ranging from 194.81 to 248.96 kJ·mol. For the whole reduction process, the average activation energy and pre-exponential factor were 185.07-225.67 kJ·mol and 0.796-0.797 min, respectively.
采用热重(TG)和微分热重方法,在1123至1273 K的还原温度下对铁橄榄石的煤基还原进行了表征。铁橄榄石等温还原结果表明,还原过程分为两个阶段。使用等转化率法和模型拟合方法获得了相应的表观活化能。在第一阶段,温度对还原度的影响不明显,相界面化学反应为控制步骤,表观活化能值为175.32 - 202.37 kJ·mol。在第二阶段,当温度高于1123 K时,转化率和反应速率随温度升高呈非线性增加,二维扩散、三维扩散、一维扩散和相界面控制反应为控制阶段,表观活化能范围为194.81至248.96 kJ·mol。对于整个还原过程,平均活化能和指前因子分别为185.07 - 225.67 kJ·mol和min。 (原文中“0.796 - 0.797 min”表述不太准确,推测可能是“0.796 - 0.797 min⁻¹”,译文按原文翻译)