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Study of kinetic characteristics of limestone decomposition under different atmospheres and heating conditions

机译:不同大气和加热条件下石灰石分解动力学特性研究

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Decomposition tests on limestone were carried out under isothermal and non-isothermal experimental conditions in 21%O-2/79%N-2 and 21%O-2/79%CO2 atmospheres. The decomposition properties and kinetics of limestone in different atmospheres and under different heating conditions were explored. The results show that different atmospheres and heating conditions can both affect the decomposition properties and kinetics of limestone. Under non-isothermal conditions, the activation energy of limestone decomposition shows an initially increasing and then decreasing trend with the increase of conversion in both atmospheres. Under isothermal conditions, the activation energy of limestone decomposition increases slightly and then decrease with the increase in conversion in 21%O-2/79%N-2 atmosphere, while the activation energy decreases monotonically with the increase IN conversion in 21%O-2/79%CO2 atmosphere. Heating conditions exert no obvious effect on the decomposition mechanism. In both atmospheres, limestone decomposition process is governed by random nucleation and nucleus growth. Limestone decomposition follows the three-dimensional model (n = A 3/4) more likely in 21%O-2/79%N-2 atmosphere, while it follows the two-dimensional model (n = 1/2) more likely in 21%O-2/79%CO2 atmosphere.
机译:石灰石的分解试验在21%O-2/79%N-2和21%O-2/79%CO 2大气压中进行等温和非等温实验条件下进行。探讨了不同大气中的石灰石和不同加热条件下石灰石的分解特性和动力学。结果表明,不同的大气和加热条件都可以影响石灰石的分解特性和动力学。在非等温条件下,石灰石分解的激活能量显示出最初增加,然后随着两种大气中转化的增加而降低趋势。在等温条件下,石灰石分解的活化能略微增加,然后随着21%O-2/79%N-2气氛中的转化率的增加而降低,而活化能量随着21%的转化率的增加而单调地降低2/79%的二氧化碳气氛。加热条件对分解机制没有显而易见的影响。在两个大气中,石灰石分解过程受随机成核和细胞核生长的控制。石灰石分解遵循三维模型(n = a 3/4)更可能在21%O-2/79%N-2气氛中,而在其遵循的二维模型(n = 1/2)更容易21%O-2/79%的CO2气氛。

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