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Melt structural self-organization and viscosity within the transient layer during a single crystal growth in microgravity

机译:微重力下单晶生长过程中过渡层内的结构自组织和粘度融化

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A brief review is given of the results obtained and published in 2003-2007 by IChPM and IPPE during their joint study and modeling of Ge:Ga, Ge:Sb, GaSb:Te, InP:S single crystal growth from stoichiometric and non-stoichiometric melts on board the Photon satellite series. The use of microgravity is shown to be justified and holding promise for research into the structural self-organization processes (cluster forming) taking place within the transient layer of the melt during the solidification. The mathematical model of convective heat and mass transfer taking into account the dual-phase character of matter in the boundary layers near the interface has been created and used as an independent tool for the study of such processes. Prospects are discussed for this new area of space material science.
机译:简要回顾了IChPM和IPPE在联合研究和建模Ge:Ga,Ge:Sb,GaSb:Te,InP:S从化学计量和非化学计量的单晶生长过程中获得并发表的结果(2003-2007年)在光子卫星系列上融化。已证明使用微重力是合理的,并有望用于研究在凝固过程中在熔体的瞬态层内发生的结构自组织过程(团簇形成)。考虑到界面附近边界层中物质的双相特性,建立了对流传热和传质的数学模型,并将其用作研究此类过程的独立工具。讨论了空间材料科学这一新领域的前景。

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