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Kinetics of the chrysotile and brucite dehydroxylation reaction: a combined non-isothermal/isothermal thermogravimetric analysis and high-temperature X-ray powder diffraction study

机译:温石棉与水镁石脱羟基反应的动力学:非等温/等温热重分析与高温X射线粉末衍射研究的结合

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摘要

The dehydroxylation reactions of chrysotile Mg₃Si₂O₅(OH)₄ and brucite Mg(OH)₂ were studied under inert nitrogen atmosphere using isothermal and non-isothermal approaches. The brucite decomposition was additionally studied under CO₂ in order to check the influence of a competing dehydroxylation/carbonation/decarbonisation reaction on the reaction kinetics. Isothermal experiments were conducted using in situ high-temperature X-ray powder diffraction, whereas non-isothermal experiments were performed by thermogravimetric analyses. All data were treated by model-free, isoconversional approaches (‘time to a given fraction’ and Friedman method) to avoid the influence of kinetic misinterpretation caused by model-fitting techniques. All examined reactions are characterised by a dynamic, non-constant reaction-progress-resolved (‘’-resolved) course of the apparent activation energy and indicate, therefore, multi-step reaction scenarios in case of the three studied reactions. The dehydroxylation kinetics of chrysotile can be subdivided into three different stages characterised by a steadily increasing ( ≤ 15 %, 240–300 kJ/mol), before coming down and forming a plateau (15 % ≤  ≤ 60 %, 300–260 kJ/mol). The reaction ends with an increasing ( ≥ 60 %, 260–290 kJ/mol). The dehydroxylation of brucite under nitrogen shows a less dynamic, but generally decreasing trend in versus (160–110 kJ/mol). In contrast to that, the decomposition of brucite under CO₂ delivers a dynamic course with a much higher apparent characterised by an initial stage of around 290 kJ/mol. Afterwards, the apparent comes down to around 250 kJ/mol at  ~ 65 % before rising up to around 400 kJ/mol. The delivered kinetic data have been investigated by the () master plot and generalised time master plot methods in order to discriminate the reaction mechanism. Resulting data verify the multi-step reaction scenarios (reactions governed by more than one rate-determining step) already visible in versus plots
机译:用等温和非等温方法研究了在惰性氮气气氛下温石棉Mg 3 Si 2 O 3(OH)3和水镁石Mg(OH)2的脱羟基反应。为了检查竞争的脱羟基/碳酸化/脱碳反应对反应动力学的影响,还另外对水镁石在CO 2下的分解进行了研究。使用原位高温X射线粉末衍射进行等温实验,而通过热重分析进行非等温实验。所有数据均采用无模型的等转换方法(“给定分数的时间”和Friedman方法)进行处理,以避免因模型拟合技术引起的动力学错误解释的影响。所有检查的反应的特征是表观活化能的动态,非恒定反应进行分辨(“-”分辨)过程,因此,在研究三个反应的情况下,它们指示了多步反应方案。温石棉的脱羟基动力学可分为三个不同的阶段,其特征是在下降并形成平稳之前(15%≤60%,300-260 kJ /%)稳定增加(≤15%,240-300 kJ / mol)。摩尔)。反应以增加(≥60%,260–290 kJ / mol)结束。氮条件下水镁石的脱羟基反应动力学较弱,但与(160-110kJ / mol)相比,总体上呈下降趋势。与此相反,水镁石在CO 2下的分解提供了一个动态过程,其动态过程具有明显更高的特征,其初始阶段约为290 kJ / mol。之后,表观在〜65%时下降到约250 kJ / mol,然后上升到约400 kJ / mol。传递的动力学数据已通过()主图和广义时间主图方法进行了研究,以区分反应机理。所得数据验证了在对比图中已经可见的多步反应场景(反应由多个速率确定步骤决定)

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