基于热重分析的菱镁矿分解动力学解析
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国家自然科学基金(41002015);广东省自然科学基金(S2011010003599);佛山市院市合作项目(20111071010019)


Decomposition kinetics of magnesite deduced from thermogravimetric analysis
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    摘要:

    本文利用热重(TG)分析方法,探讨了菱镁矿的热分解过程。根据热微商(DTG)曲线峰顶温度,结合Kissinger及Ozawa-Doyle方法拟合计算得到菱镁矿热分解的活化能和指前因子(lgA)分别为211.55 kJ/mol和11.07 s-1。依次采用单曲线拟合、多元非线性拟合及Malek方法判定得出菱镁矿热分解过程属于三维相界反应模型(R3),其动力学方程为:dα/dT=(1011.07/β)·e-211.55×103/(8.314×T)·3(1-α2/3

    Abstract:

    Decomposition kinetics of magnesite was investigated by using thermogravimetric (TG) analysis. The activation energy (E) and pre-exponential factor (lgA) were calculated from Kissinger and Ozawa-Doyle equations, and the peak value of derivative thermogravimetry (DTG) data was used as the maximum temperature. The calculated E and lgA were 211.55 kJ/mol and 11.07 s-1, respectively. The reaction mechanism was further discussed by using single-TG curve, multivariate no-linear regressions and Malek method, respectively. The obtained results indicate that the reaction was a three-dimensional phase boundary reaction (R3). The kinetic equation was as follows: dα/dT=(1011.07/βe-211.55×103/(8.314×T)·3(1-α)2/3.

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张强,何宏平,陶奇,2014,基于热重分析的菱镁矿分解动力学解析[J].岩石矿物学杂志,33(2):391~396. ZHANG Qiang, HE Hong-ping, TAO Qi,2014,Decomposition kinetics of magnesite deduced from thermogravimetric analysis[J]. Acta Petrologica et Mineralogica,33(2):391~396.

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  • 收稿日期:2013-09-05
  • 最后修改日期:2013-12-06
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  • 在线发布日期: 2014-03-28
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