The kinetic mechanism and influential factors of the thermal decomposition process of magnesium-smelting dolomite from Wansheng area of Chongqing
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    Abstract:

    Thermal decomposition reactions of dolomite samples from Wansheng area of Chongqing were investigated by the simultaneous TG/DTG experiments to reveal the thermal decomposition mechanism and influential factors. The results show that the thermal decomposition process of dolomite samples follows the three-dimensional diffusion (three dimensional particle shape, Jander equation) model, and the value of the activation energy for the thermal composition is 357.4 kJ/mol. The kinetic model of the thermal decomposition process has been established based on the research results. The contrast experiments of the influential factors show that the value of the activation energy for the thermal composition would be increased significantly with the decrease of sample particle size and the increase of sample weight; nevertheless, the change of the SiO2 content of dolomite and the flow rate of protective gas has little impact on the activation energy of thermal decomposition of the dolomite samples.

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刘欢,龙思远,周玉乐,杨怀德,游国强,2013,重庆万盛炼镁用白云岩分解动力学及影响因素的研究[J].岩石矿物学杂志,32(6):1001~1005. LIU Huan, LONG Si-yuan, ZHOU Yu-le, YANG Huai-de, YOU Guo-qiang,2013,The kinetic mechanism and influential factors of the thermal decomposition process of magnesium-smelting dolomite from Wansheng area of Chongqing[J]. Acta Petrologica et Mineralogica,32(6):1001~1005.

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History
  • Received:June 15,2013
  • Revised:September 13,2013
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  • Online: November 19,2013
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