Bergeon Nathalie, Reinhart Guillaume, Mota Fatima L, Mangelinck-Noël Nathalie, Nguyen-Thi Henri
CNRS, IM2NP, Aix Marseille Univ, Université de Toulon, Avenue Escadrille Normandie Niemen, 13397, Marseille Cedex 20, France.
Eur Phys J E Soft Matter. 2021 Jul 20;44(7):98. doi: 10.1140/epje/s10189-021-00102-0.
Under terrestrial conditions, solidification processes are influenced to a large degree by the gravity effects such as natural convection or buoyancy force, which can dramatically modify the final characteristics of the grown solid. In the last decades, the coupling of in situ observation of growth from the melt, that enables the study of microstructure formation dynamics, and microgravity experimentation, that allows to approach diffusive conditions, has been implemented for both transparent and metallic materials. The results of these investigations enable to test the validity of advanced solidification theories, to validate or develop numerical models and sometimes to reveal unexpected phenomena. The aim of this paper is to present a selection of conclusive experiments obtained with this combined approach in our group to highlight the gravity effects by a comparative study of experiments carried out on earth and in microgravity conditions.
在地球条件下,凝固过程在很大程度上受到重力效应的影响,如自然对流或浮力,这会极大地改变生长固体的最终特性。在过去几十年中,对于透明材料和金属材料,已实现了熔体生长的原位观察(这使得研究微观结构形成动力学成为可能)与微重力实验(这能实现接近扩散条件)的结合。这些研究结果能够检验先进凝固理论的有效性,验证或开发数值模型,有时还能揭示意外现象。本文的目的是展示我们团队通过这种组合方法获得的一系列确凿实验,通过对在地球和微重力条件下进行的实验进行对比研究来突出重力效应。