论文标题
Si:ii的自组织离子束图案中的纳米级动力学。 Kr $^+$轰炸
Nanoscale dynamics during self-organized ion beam patterning of Si: II. Kr$^+$ Bombardment
论文作者
论文摘要
尽管进行了广泛的研究,但对大型离子轰击对自组织的模式的基本了解仍然不完整且有争议。了解元素半导体的纳米图案,尤其是硅,既是更广泛的领域,以及内在的科学和技术兴趣本身的基础。这是对1 kev ar $^+$(第I部分)和kr $^+$轰炸过程中对动力学和自组织纳米级波动开发的动力学和波动动态进行两部分调查的第二个组成部分。在这里,发现与先前针对Ar $^+$构图所示的KR $^+$诱导的图案的离子增强粘性流放松基本上相等。对于KR $^+$,在早期动力学中,表面曲率依赖性粗糙率的大小大于AR $^+$,这与对初始表面不稳定性的侵蚀性和质量再分配贡献的期望一致。与AR $^+$情况一样,后期的波动动力学在长度尺度上显示了相关时间的峰值,与表面上的主要结构特征 - 波纹 - 涟漪。类比是与液体中de Gennes的现象进行的,但也指出了显着差异。最后,这表明可以分析表面进化过程中的斑点运动,以确定表面侵蚀速率和涟漪速度的空间不均匀性。这允许实时测量波纹运动的方向和速度,这是在FIB/SEM系统的专业环境之外测量这些基本参数的独特功能。
Despite extensive study, fundamental understanding of self-organized patterning by broad-beam ion bombardment is still incomplete and controversial. Understanding the nanopatterning of elemental semiconductors, particularly silicon, is both foundational for the broader field and of intrinsic scientific and technological interest itself. This is the second component of a two-part investigation of the kinetics and fluctuation dynamics of self-organized nanoscale ripple development on silicon during 1 keV Ar$^+$ (Part I) and Kr$^+$ bombardment. Here, it's found that the ion-enhanced viscous flow relaxation is essentially equal for Kr$^+$-induced patterning as previously found for Ar$^+$ patterning. The magnitude of the surface curvature dependent roughening rate in the early stage kinetics is larger for Kr$^+$ than for Ar$^+$, qualitatively consistent with expectations for erosive and mass redistributive contributions to the initial surface instability. As with the Ar$^+$ case, fluctuation dynamics in the late stage show a peak in correlation time at the length scale corresponding to the dominant structural feature on the surface -- the ripples. Analogy is made to the phenomenon of de Gennes narrowing in liquids, but significant differences are also pointed out. Finally, it's shown that speckle motion during the surface evolution can be analyzed to determine spatial inhomogeneities in erosion rate and ripple velocity on the surface. This allows the direction and speed of ripple motion to be measured in real time, a unique capability for measuring these fundamental parameters outside the specialized environment of FIB/SEM systems.