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亚单层沉积过程中岛状形核与生长的捕获区面积分布。

Capture zone area distributions for nucleation and growth of islands during submonolayer deposition.

机构信息

Department of Physics and Astronomy, Iowa State University, Ames, Iowa 50011, USA.

Department of Physics, Renmin University of China, Beijing 100872, People's Republic of China.

出版信息

J Chem Phys. 2016 Dec 7;145(21):211911. doi: 10.1063/1.4961264.

Abstract

A fundamental evolution equation is developed to describe the distribution of areas of capture zones (CZs) associated with islands formed by homogeneous nucleation and growth during submonolayer deposition on perfect flat surfaces. This equation involves various quantities which characterize subtle spatial aspects of the nucleation process. These quantities in turn depend on the complex stochastic geometry of the CZ tessellation of the surface, and their detailed form determines the CZ area distribution (CZD) including its asymptotic features. For small CZ areas, behavior of the CZD reflects the critical island size, i. For large CZ areas, it may reflect the probability for nucleation near such large CZs. Predictions are compared with kinetic Monte Carlo simulation data for models with two-dimensional compact islands with i = 1 (irreversible island formation by diffusing adatom pairs) and i = 0 (adatoms spontaneously convert to stable nuclei, e.g., by exchange with the substrate).

摘要

发展了一个基本的演化方程来描述在完美平坦表面上亚单层沉积过程中均匀成核和生长所形成的捕获区(CZ)的面积分布。该方程涉及各种数量,这些数量表征了成核过程的细微空间方面。这些数量反过来又取决于 CZ 表面细分的复杂随机几何形状,它们的详细形式决定了 CZ 面积分布(CZD),包括其渐近特征。对于小的 CZ 区域,CZD 的行为反映了临界岛的大小,即。对于大的 CZ 区域,它可能反映了在这种大 CZ 附近成核的概率。预测结果与具有二维紧密岛屿的 i = 1(通过扩散 adatoms 对的不可逆岛屿形成)和 i = 0(adatoms 自发转化为稳定核,例如通过与衬底交换)的模型的动力学蒙特卡罗模拟数据进行了比较。

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