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PHOTOLUMINESCENCE AND STRUCTURE OF FULLERITE C_(60) INTERCALATED WITH HELIUM

机译:夹层富铝C_(60)的光致发光和结构

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摘要

Powder x-ray diffractometry was employed to study infusion of He into C_(60) fullerite. It has been shown that the intercalation at a pressure of 0.1 MPa is a two-stage process, the first stage being the saturation of the octahedral voids, virtually complete after 55 hr. Photoluminescence spectra have been measured at 5 K on C_(60) with virtually completely saturated octahedral voids. Helium in the lattice voids is shown to reduce that part of the luminescent emission which is due to 0-0 transitions around 1.69 eV from the so-called deep traps, or according to existing notions, covalently bound pairs of C_(60) molecules. The effect of intercalation with helium on dimer formation in fullerite C_(60) is ascribed to a combined action of the following factors: intercalation-related changes of the pentagon to hexagon configuration ratio, formation of a bonded state of He in the C_(60) lattice, and moderation by helium of the orientational phase transition near 260 K, the last factor resulting in a reduced number of dislocations (which also promotes dimer formation).
机译:利用粉末X射线衍射法研究了He向C_(60)富勒岩中的注入。已经表明,在0.1 MPa的压力下进行插层是一个两阶段的过程,第一阶段是八面体空隙的饱和,实际上在55小时后就完成了。已在C_(60)上于5 K下测量了几乎完全饱和的八面体空隙的光致发光光谱。晶格空隙中的氦气显示减少了发光发射的那部分,这归因于所谓的深陷阱中1.69 eV附近的0-0跃迁,或者根据现有观念,共价键合了C_(60)分子对。富碳C_(60)中氦与插层对二聚体形成的影响归因于以下因素的综合作用:五角形与六边形构型比的与插层有关的变化,C_(60)中He的键合状态的形成晶格)和260 K附近氦的定向相变的缓和作用,最后一个因素导致位错数量减少(这也促进了二聚体的形成)。

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