红柱石(Al2SiO5)固相高温转化成32-莫来石(3al2o3.2 . SiO2)和二氧化硅(SiO2)的动力学及机理

H Schneider, A Majdič
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引用次数: 23

摘要

利用x射线技术研究了红柱石(<40 μm)的高温转变动力学。相变区间在1250 ~ 1500℃之间。结果表明:1 - α = exp (- kt + ct/(t + 1))是最佳拟合方程。动力学曲线与铝氧八面体链保存和铝、硅、氧原子扩散的拓扑转换模式有关。在1380℃以下,莫来石(+SiO2)的形成基本上局限于转变的初始快速阶段,因为成核和产物生长只发生在能量有利的晶格位置(如晶界)。在1380°C以上,莫来石和SiO2在整个低温相(红柱石)的整个体积内都可能成核和生长。
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Kinetics and mechanism of the solid-state high-temperature transformation of andalusite (Al2SiO5) into 32-mullite (3Al2O3.2SiO2) and silica (SiO2)

The kinetics of the high-temperature transformation of andalusite (<40 μm) were investigated by means of X-ray techniques. The transformation interval was determined to lie between about 1250 and 1500°C. The best fitting of the kinetic data was achieved with an exponential law of the type: 1 − α = exp (−kt + ct/(t + 1)). The kinetic curves are associated with a topotactic transformation mode with preservation of the aluminium-oxygen octahedral chains and diffusion of aluminium, silicon and oxygen atoms. Below 1380°C, mullite (+SiO2) formation is essentially restricted to an initial rapid period of the transformation, because nucleation and product growth occur only at energetically favored lattice sites (e.g. grain boundaries). Above 1380°C, mullite and SiO2 nucleation and growth may take place throughout the volume of the low-temperature phase (andalusite) over the whole range investigated.

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