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Mg(OH)_2 dehydroxylation: A kinetic study by controlled rate thermal analysis (CRTA)

机译:Mg(OH)_2脱羟基:通过控制速率热分析(CRTA)进行的动力学研究

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The present work is the first kinetic study of Mg(OH)_2 dehydroxylation carried out by controlled rate thermal analysis technique. Its aim is first to highlight the importance of controlling the residual water vapor pressure above the sample as well as the rate of the thermal decomposition during the thermal dehydroxylation of brucite Mg(OH)_2 and second to investigate its kinetics of dehydroxylation. For this reason, the dehydroxylation of the titled compound was followed by both: the constant rate thermal analysis technique at P_(H_2O) = 10~(-3) hPa and the conventional thermal analysis techniques (TG and DSC) in air. It has been shown that the structure of the final product depends strongly on the nature of the thermal treatment. However, in air atmosphere brucite decomposes in the temperature range 610-772 K, to obtain a high defect MgO as an intermediate phase which retains the brucite structure. This defect structure collapses progressively to the cubic MgO in the temperature range 772-810 K, whereas decomposition carried out at P_(H_2O) = 10~(-3) hPa by CRTA technique, gives a high defect MgO phase which retains the brucite structure even after the end of the dehydroxylation. In first approximation, it can be supposed that this step is controlled by a process of nucleation and growth of nuclei in three dimensions (A3). This conclusion is confirmed by the comparison of two iso-kinetic CRTA curves for dehydroxylation of Mg(OH)_2 carried out under the same water vapor pressure (P_(H_2O) = 10~ (-3) hPa) which allows to use the Arrhenius law and so to calculate an apparent activation energy equal to 188 + - 10 kJ mol~(-1) in almost the total dehydroxylation interval.
机译:目前的工作是通过控制速率热分析技术进行的Mg(OH)_2脱羟基反应的第一个动力学研究。其目的是首先强调控制水样上方残留水蒸气压力以及水镁石Mg(OH)_2热脱羟基过程中热分解速率的重要性,其次是研究其脱羟基动力学。因此,要进行标题化合物的脱羟基反应:在P_(H_2O)= 10〜(-3)hPa时采用恒速热分析技术和在空气中进行常规热分析技术(TG和DSC)。已经表明,最终产品的结构在很大程度上取决于热处理的性质。然而,在空气气氛中,水镁石在610-772K的温度范围内分解,以获得高缺陷MgO作为保留水镁石结构的中间相。该缺陷结构在772-810 K的温度范围内逐渐塌陷为立方MgO,而通过CRTA技术在P_(H_2O)= 10〜(-3)hPa下进行分解,得到了高缺陷MgO相,并保留了水镁石结构。甚至在脱羟基结束之后。在第一近似中,可以假设此步骤是由三个维度的成核和核生长过程控制的(A3)。通过比较在相同水蒸气压力(P_(H_2O)= 10〜(-3)hPa)下进行的Mg(OH)_2脱羟基的两条等速CRTA曲线可以证实这一结论,这允许使用Arrhenius依此类推,计算出几乎在整个脱羟基间隔内的表观活化能等于188 +-10 kJ mol〜(-1)。

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