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首页> 外文期刊>Philosophical Magazine >On the high-temperature structural behaviour of talc (Mg3Si4O10(OH)2) to 1600°C: Effect of mechanical deformation and strain
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On the high-temperature structural behaviour of talc (Mg3Si4O10(OH)2) to 1600°C: Effect of mechanical deformation and strain

机译:关于滑石粉(Mg 3 Si 4 O 10 (OH) 2 )的高温结构行为1600°C:机械变形和应变的影响

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摘要

The high-temperature structural behaviour of talc, Mg3Si4O10(OH)2, deformed by compaction and shear was investigated for the first time by extending the temperature range to 1600°C. The deformation was induced with low mechanical load through a specifically built planetary ball milling working in a controlled thermodynamic environment (25°C and at a vacuum of 0.13 Pa). The mechanical energy transfer to the material was measured via the microstrain ϵ 21/2. In our experimental set-up, amorphisation was not deliberately reached since we wanted to investigate the details of the evolution of the talc structure as a function of the microstrain. At the very early stage of milling (up to 1 h), no strain was accumulated in the talc structure which, however, presented lamination, layer flattening and texturing. Further milling induced a progressive reduction of the stacking layer coherence and an increase of the microstrain, in both cases as a non linear function of the deformation time. The thermo-structural behaviour of talc was investigated by TG-DTA in a helium atmosphere at 10°C/min of heating rate. In the medium temperature range (400-1100°C), the mechanical milling affected the dehydroxylation reaction by a significant anticipation of about 200-300°C of the temperature range, which usually occurs between 750 and 1050°C and gave rise to a clear exothermic reaction at about 840°C, related to an increase of the recrystallisation kinetics of MgSiO3 (orthoenstatite). The mechanical deformation strongly influenced also the kinetics of the high-temperature endothermic reactions at about 1555°C, involving cristobalite and MgSiO3 polymorphs melting and transformation. All thermal reactions linearly correlate to the microstrain ϵ 21/2 accumulated in the talc structure.
机译:滑石粉Mg 3 Si 4 O 10 (OH) 2 的高温结构行为通过将温度范围扩展到1600°C,首次研究了压实和剪切。通过在受控的热力学环境(25°C和0.13 Pa的真空)下工作的专门制造的行星式球磨机,以较低的机械负载引起了变形。通过微应变ϵ 2 1/2 测量向材料的机械能传递。在我们的实验装置中,没有故意达到非晶化,因为我们想研究滑石结构随微应变变化的细节。在研磨的最早期阶段(长达1小时),滑石结构中没有积聚任何应变,但是却出现了层压,层变平和变形的现象。在这两种情况下,进一步的研磨都会引起堆积层相干性的逐渐降低和微应变的增加,这都是变形时间的非线性函数。滑石粉的热结构行为由TG-DTA在氦气气氛中以10℃/ min的升温速率研究。在中等温度范围(400-1100°C)中,机械铣削通过显着预期温度范围大约为200-300°C(通常在750至1050°C之间发生)来影响脱羟基反应。在大约840°C时发生明显的放热反应,这与MgSiO 3 (正钙长石)的重结晶动力学增加有关。机械变形还强烈影响大约1555°C的高温吸热反应的动力学,涉及方石英和MgSiO 3 多晶型物的熔化和转变。所有热反应与滑石结构中累积的微应变ϵ 2 1/2 线性相关。

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