中国物理B ›› 2010, Vol. 19 ›› Issue (10): 106102-106102.doi: 10.1088/1674-1056/19/10/106102
Jeyanthinath Mayandi1, 王学森1, 薛其坤2, 徐茂杰3, 贾金锋3, 窦晓鸣4
Xu Mao-Jie(徐茂杰)a), Jeyanthinath Mayandib), Wang Xue-Sen(王学森)b), Jia Jin-Feng(贾金锋)a),Xue Qi-Kun(薛其坤)c), and Dou Xiao-Ming(窦晓鸣)a)d)†
摘要: Pit formation and surface morphological evolution in Si(001) homoepitaxy are investigated by using scanning tunneling microscopy. Anti-phase boundary is found to give rise to initial generation of pits bound by bunched DB steps. The terraces break up and are reduced to a critical nucleus size with pit formation. Due to anisotropic kinetics, a downhill bias diffusion current, which is larger along the dimer rows through the centre area of the terrace than through the area close to the edge, leads to the prevalence of pits bound by {101} facets. Subsequent annealing results in a shape transition from {101}-faceted pits to multi-faceted pits.
中图分类号: (Structure of clean surfaces (and surface reconstruction))