タイトル(掲載誌)Surface Science = Surface Science
一般注記The origin of RHEED intensity oscillations or variations during growth is analysed by using RHEED intensity distributions calculated from wave functions inside and outside the crystal surface. When the growth proceeds in a layer by layer fashion and the observed intensity is near a diffraction peak, there are only two possible origins of the intensity variations. One is theinterference between waves diffracted by the top and the subsequent underlying layers, and the other is the disturbance of the RHEED electron waves by step edges. RHEED rocking curves are computed and the intensities of peaks in the curves are found to vary systematically when material is deposited on the surface. The mechanism of these variations is identified by computing RHEED intensity distributions. An approximate measure of the disturbance of the wave function by step edges is also introduced.
一次資料へのリンクURLhttps://yamanashi.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4706&item_no=1&attribute_id=22&file_no=1
連携機関・データベース国立情報学研究所 : 学術機関リポジトリデータベース(IRDB)(機関リポジトリ)