石墨烯
材料科学
扫描隧道显微镜
化学计量学
原子力显微镜
梯田(农业)
形态学(生物学)
单层
分析化学(期刊)
纳米技术
地质学
物理化学
化学
古生物学
考古
色谱法
历史
作者
M. L. Bolen,S. E. Harrison,Laura Biedermann,Michael A. Capano
出处
期刊:Physical Review B
[American Physical Society]
日期:2009-09-25
卷期号:80 (11)
被引量:126
标识
DOI:10.1103/physrevb.80.115433
摘要
Graphene is created through thermal decomposition of the Si face of $4H\text{-SiC}$ in high-vacuum. Growth temperature and time are varied independently to gain a better understanding of how surface features and morphology affect graphene formation. Growth mechanisms of graphene are studied by ex situ atomic force microscopy (AFM) and scanning tunneling microscopy (STM). On the route toward a continuous graphene film, various growth features, such as macroscale step bunching, terrace pits, and fingers, are found and analyzed. Topographic and phase AFM analysis demonstrates how surface morphology changes with experimental conditions. Step-bunched terraces and terrace pits show a strong preference for eroding along the ${11\overline{2}0}$ planes. Data from AFM are corroborated with STM to determine the surface structure of the growth features. It is shown that elevated finger structures are SiC while the depressed interdigitated areas between the fingers are comprised of at least a monolayer of graphene. Graphene formation at the bottom of terrace pits shows a dependence on pit depth. These features lend support for a stoichiometric view of graphene formation based on the number of decomposing SiC bilayers.
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