Orientation of Disk-like Particles in a Microcomposite Processing

K. Yasuda, N. Ohara, N. Mori, K. Chiba
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引用次数: 7

Abstract

The objective of this study is to well understand the migration and orientation of thin micro-particles in a suspension flow by means of both experiments and numerical simulations. In this framework, the evolution of the orientation of thin micro-particles such as talc and mica, which were modeled by a disk-like particle, in a flow through a slit channel was analyzed to obtain the knowledge of the processing operations of thin micro-particle reinforced composites.The thin disk-like particles were subjected by a planar extensional flow in a reservoir, then by a simple shear flow through a slit channel in the experimental apparatus used. The evolution of the orientation of thin disk-like particles was, therefore, studied in both a planar extensional and simple shear flows by numerical calculation of the Jeffery equation: thin disk-like particles aligned in a parallel orientation to upper- and lower-walls of the slit channel in a planar extensional flow through the reservoir, then entered into the inlet of the slit channel. On the other hand, in a simple shear flow through the slit channel, the disk-like particles kept this parallel orientation except the occurrence of a flip-over phenomenon. The period of the flip-over became longer with a decrease in the aspect ratio of the disk-like particles.Furthermore, the measurements of the orientation of the talc particles in a suspension flow through the slit channel clearly showed that almost the same period of the flip-over was found although the particle size was different. These experimental results arise from complex geometries and no accurate data of the thickness of the talc particles.
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微复合材料加工中圆盘状颗粒的取向
本研究的目的是通过实验和数值模拟来更好地了解悬浮流中细颗粒的迁移和取向。在此框架下,以圆盘状颗粒为模型,分析了滑石和云母等细颗粒在狭缝通道中的取向演变,从而获得细颗粒增强复合材料的加工操作知识。薄片状颗粒在储层中经受平面拉伸流动,然后在实验装置中经受通过狭缝通道的简单剪切流动。因此,通过对Jeffery方程的数值计算,研究了平面伸展流动和简单剪切流动中薄盘状颗粒的取向演化:在平面伸展流动中,薄盘状颗粒沿狭缝通道上下壁面平行排列,然后进入狭缝通道入口。另一方面,在通过狭缝通道的简单剪切流动中,除了发生翻转现象外,盘状颗粒保持这种平行方向。随着盘状颗粒长径比的减小,翻转周期变长。此外,对滑石颗粒在悬浮流中通过狭缝通道的方向的测量清楚地表明,尽管颗粒大小不同,但发现几乎相同的翻转周期。这些实验结果源于复杂的几何形状和没有精确的滑石颗粒厚度数据。
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