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黄铁矿在CO2气氛下非等温氧化转化及动力学分析

Non-Isothermal Oxidation Transformation and Kinetics of Pyrite in CO2

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【作者】 黄芳况怡婷张立麒米铁辛善志刘晓烨

【Author】 Huang Fang;Kuang Yiting;Zhang Liqi;Mi Tie;Xin Shanzhi;Liu Xiaoye;Hubei Key Laboratory of Industrial Fume and Dust Pollution Control,School of Environment and Health,Jianghan University;State Key Laboratory of Coal Combustion,School of Energy and Power Engineering,Huazhong University of Science and Technology;

【通讯作者】 米铁;

【机构】 江汉大学环境与健康学院工业烟尘污染控制湖北省重点实验室华中科技大学能源与动力工程学院煤燃烧国家重点实验室

【摘要】 针对煤中常见含铁矿物黄铁矿在富氧燃烧典型气氛下转化特性,通过同步热分析结合烟气分析研究了黄铁矿在CO2气氛下的转化行为.结果发现,黄铁矿在CO2气氛下主要经历5个失重阶段且均为吸热过程,首先是黄铁矿颗粒表面硫脱除的起始热解段(相界面反应,n=1/2),活化能低于其在N2气氛下近30 k J/mol,为220.27 k J/mol,随后裂解成磁黄铁矿(三维扩散,n=1/2)活化能与其在N2(177.27 k J/mol)下接近为178.1 k J/mol;温度高于690℃,随着升温磁黄铁矿缓慢失硫,CO2逐渐参与磁黄铁矿转化且释放SO2和CO;820~1 150℃经历双峰失重峰阶段,820~1 020℃,氧化气体产物SO2大量生成且在约1 000℃达到体积浓度峰值;最后1 020~1 150℃,坩埚中残留物大量与CO2持续氧化反应失重形成SO2和CO,坩埚中形成复杂物相体系,铁硫化物和铁氧化物共存(或共融).CO2参与黄铁矿产物转化失重阶段活化能分别为180.94 k J/mol、229.69 k J/mol和243.46 k J/mol,动力学机制均为成核与生长(n=1).

【Abstract】 To investigate the transformation behavior of pyrite under typical oxy-fuel combustion atmosphere,the transformation behavior of pyrite in CO2 atmosphere was studied by simultaneous thermal analysis and flue gas analysis.The results showed that the pyrolysis of pyrite can be mainly divided into five weight loss stages in CO2atmosphere,all of which were endothermic processes.The activation energy of the initial pyrolysis stage (phase interface reaction,n=1/2) of sulfur removal on the surface of pyrite particles was 220.27 k J/mol in CO2 atmosphere,which was about 30 k J/mol lower than that in N2 atmosphere.Then,the pyrite was mainly decomposed into pyrrhotite (three-dimensional diffusion,n=1/2),and the activation energy was 178.1 k J/mol (177.27 k J/mol in N2).When the temperature was raised above 690℃,the solid products continued to lose sulfur slowly,and CO2 gradually participated in the conversion of solid products to release SO2 and CO.At 820—1 150℃,the sample experienced bimodal weight loss peak stage.At 820—1 020℃,the oxidizing gas SO2 was generated in large quantities and reached the maximum volume concentration at about 1 000℃.At the temperature between 1 020—1 150℃,a large amount of residue in the crucible continuously reacted with CO2 to generate SO2 and CO,and a complex phase system was formed in the crucible,in which iron sulfides and iron oxides co-existed (or formed eutectic mixtures).The activation energies of the mass loss stages of pyrite decomposition products reacting with CO2 are 180.94 k J/mol,229.69 k J/mol and 243.46 k J/mol,respectively,and the kinetic mechanisms are nucleation and growth (n=1).

【关键词】 黄铁矿非等温CO2氧化转化动力学
【Key words】 pyritenon-isothermalCO2oxidation transformationkinetics analysis
【基金】 国家自然科学基金资助项目(51706085);湖北省教育厅高校中青年创新团队资助项目(T201420);江汉大学“四新”专项基金资助项目(2022SXZX05)
  • 【文献出处】 燃烧科学与技术 ,Journal of Combustion Science and Technology , 编辑部邮箱 ,2024年01期
  • 【分类号】TQ534
  • 【下载频次】64
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