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通过电子束辐照和在高压电子显微镜中进行原位加热在高岭土中形成晶体硅。

Formation of crystalline silicon in kaolinite by electron beam irradiation and in situ heating in the HVEM.

作者信息

Lee Sujeong, Kim Young-Min, Kim Youn-Joong

出版信息

J Electron Microsc (Tokyo). 2007 Aug;56(4):153-5. doi: 10.1093/jmicro/dfm015. Epub 2007 Oct 19.

Abstract

Electron beam irradiation can change the bulk structure of a specimen permanently. The crystallizations of amorphous phases in the 900 degrees C-heated kaolinite by electron beam irradiation and natural kaolinite by in situ heating are observed in a 1250 keV HVEM in this study. Crystalline silicon was formed in both cases. The lack of the parent structure and the aluminum loss are obstacles to the formation of the spinel-type phase. Amorphous silica is segregated instead and silicon crystals are progressively formed through Si--O bond breakage and Si--Si bond formation. Irradiation damage and element loss are considered to contribute to the crystallization of silicon under ultra high vacuum.

摘要

电子束辐照可永久性改变样品的整体结构。本研究在1250 keV高压电子显微镜下观察了经电子束辐照的900℃加热高岭土中非晶相的结晶以及原位加热的天然高岭土中非晶相的结晶。在这两种情况下均形成了晶体硅。母体结构的缺失和铝的损失是形成尖晶石型相的障碍。相反,非晶态二氧化硅发生偏析,并且通过Si—O键的断裂和Si—Si键的形成逐渐形成硅晶体。在超高真空下,辐照损伤和元素损失被认为有助于硅的结晶。

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