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金属矿山 ›› 2026, Vol. 55 ›› Issue (7): 177-.

• 矿物工程 • 上一篇    下一篇

菱镁矿悬浮煅烧热分解过程的反应动力学研究

李鹏俊1,2 李艳军1,2 袁 帅1,2 白丽梅3 王余莲4 姚 金1,2   

  1. 1.东北大学矿物加工科学与技术全国重点实验室,辽宁 沈阳 110819;2.东北大学资源与土木工程学院,辽宁 沈阳 110819; 3.华北理工大学矿业工程学院,河北 唐山 063210;4.沈阳理工大学材料科学与工程学院,辽宁 沈阳 110159
  • 出版日期:2026-07-15 发布日期:2026-08-24
  • 通讯作者: 李艳军(1972—),男,教授,博士,博士研究生导师。
  • 作者简介:李鹏俊(2000—),女,硕士研究生。
  • 基金资助:
    兴辽英才计划青年拔尖人才项目(编号:XYC2203167);辽宁省优秀青年自然科学基金项目(编号:2023JH3/10200010)。

Study on the Reaction Kinetics of the Thermal Decomposition Process of Magnesite Suspension Calcination

LI Pengjun1,2 LI Yanjun1,2 YUAN Shuai1,2 BAI Limei3 WANG Yulian4 YAO Jin1,2   

  1. 1.State Key Laboratory of Mineral Processing,Northeastern University,Shenyang 110819,China; 2.School of Resources and Civil Engineering,Northeastern University,Shenyang 110819,China; 3.School of Mining Engineering,North China University of Science and Technology,Tangshan 063210; 4.College of Materials Science and Engineering,Shenyang University of Science and Technology,Shenyang 110159,China
  • Online:2026-07-15 Published:2026-08-24

摘要: 为探究细粒菱镁矿在悬浮态下的热分解反应机理,并为悬浮煅烧工艺优化提供理论依据,本研究采用 气相组成在线分析系统对细粒菱镁矿热分解过程中的反应动力学进行了深入研究。结果表明,随着温度升高,菱镁 矿颗粒反应速率的峰值逐渐升高,并且达到峰值的时间明显缩短。不同粒度的菱镁矿反应分数和反应速率有着相似 的变化趋势。积分法分析表明,-325目含量占60%的菱镁矿颗粒在低温下的热分解反应动力学符合G(α) =1-(1-α)1/3模型,其表观活化能为87.04 kJ/mol;在高温条件下反应动力学模型为G(α) =[1-(1-α)1/3]2,其表观活化 能为72.08 kJ/mol;粒度为-325目含量90%的菱镁矿颗粒在低温和高温条件下的热分解反应动力学均符合G(α) = 1-(1-α)1/3模型,反应活化能分别为107.58 kJ/mol和76.79 kJ/mol。不同条件下菱镁矿热分解反应动力学模型存 在差异,本质是界面化学反应速率与产物CO2 扩散速率竞争的结果,受温度和粒度共同调控;随着粒度的增大,菱镁 矿热分解反应控制机理由界面化学反应控制向颗粒内扩散控制转变。

关键词: 菱镁矿 , 等温动力学 , 悬浮煅烧 , 粒度

Abstract: To investigate the thermal decomposition reaction mechanism of fine magnesite in a suspended state and to provide a theoretical basis for optimizing the suspension calcination process,this study employed an online gas composition a nalysis system to conduct an indepth investigation into the reaction kinetics during the thermal decomposition of fine magnesite. The results indicate that with increasing temperature,the peak reaction rate of magnesite particles gradually rises,and the time required to reach the peak is significantly shortened.The reaction fraction and reaction rate of magnesite with different particle sizes exhibit similar trends.Integral kinetic analysis reveals that for magnesite particles with 60% passing 325 mesh,the ther mal decomposition kinetics at low temperatures follow the model G(α) =1-(1-α)1/3,with an apparent activation energy of 87.04 kJ/mol;At high temperatures,the kinetic model conforms to G(α)=[1-(1-α)1/3]2,with an apparent activation en ergy of 72.08 kJ/mol.For magnesite particles with 90% passing 325 mesh,the thermal decomposition kinetics at both low and high temperatures fit the model G(α) =1-(1-α)1/3,with activation energies of 107.58 kJ/mol and 76.79 kJ/mol,respec tively.The variation in kinetic models under different conditions is essentially attributable to the competition between the inter facial chemical reaction rate and the CO2 product diffusion rate,which is jointly governed by temperature and particle size.As the particle size increases,the rate-controlling mechanism of magnesite thermal decomposition shifts from interfacial chemical reaction control to intraparticle diffusion control.

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