Graphene formation mechanisms on 4H-SiC(0001)

被引:111
|
作者
Bolen, Michael L. [1 ,2 ]
Harrison, Sara E. [1 ,2 ]
Biedermann, Laura B. [2 ,3 ]
Capano, Michael A. [1 ,2 ]
机构
[1] Purdue Univ, Sch Elect Engn, W Lafayette, IN 47907 USA
[2] Purdue Univ, Birck Nanotechnol Ctr, W Lafayette, IN 47907 USA
[3] Purdue Univ, Dept Phys, W Lafayette, IN 47907 USA
来源
PHYSICAL REVIEW B | 2009年 / 80卷 / 11期
关键词
ELECTRONIC-PROPERTIES; EPITAXIAL GRAPHENE; SILICON-CARBIDE; GRAPHITE; 6H-SIC(0001); LAYERS; FILMS;
D O I
10.1103/PhysRevB.80.115433
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Graphene is created through thermal decomposition of the Si face of 4H-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 (2) over bar0} 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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页数:9
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