活化熵作为高岭石脱羟基反应中可能的结构敏感参数

I. Horváth, G. Kranz, Yu.G. Fedorenko
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引用次数: 8

摘要

采用等温热重法研究了14种不同结构无序(结晶度)高岭石的脱羟基化动力学。二级动力学被发现在脱羟基过程中控制水的释放速率,无论结晶度和/或等温加热的温度如何,转化率高达60%。结晶度和活化能(E)之间没有简单的关系。对于一些极度无序的结构,E的值出人意料地高。为了解释这一点,考虑了气体产物的晶内压力的作用及其在分解反应中的扩散路径的特征。结晶度(指数HWB)与活化熵(ΔS≠)通过经验直线函数关系:HWB = (0.07064 ΔS≠)+ 17.65 (correl。多项式系数。r = 0.873),其中ΔS≠值随高岭石结晶度的降低而增大(指数HWB增大)。
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Entropy of activation as a possible structure-sensitive parameter in the dehydroxylation of kaolinite

The kinetics of the dehydroxylation on 14 kaolinites having varying structural disorder (crystallinity) was studied by use of an isothermal TG method. Second-order kinetics were found to control the rate of water release during the dehydroxylation with up to 60% of conversion regardless of the crystallinity and/or temperature of the isothermal heating.

There is no simple relationship between crystallinity and activation energy (E). Unexpectedly high values of E have been determined for some extremely disordered structures. To explain this, the role of intracrystalline pressure of the gaseous product as well as the character of its diffusion paths in the decomposition reaction have been considered.

The crystallinity (index HWB) and activation entropy (ΔS) are related by empirical straight-line function: HWB = (0.07064 ΔS) + 17.65 (correl. coeff. r = 0.873) in which ΔS values increase with decreasing of kaolinite crystallinity (index HWB increases).

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