Department of Physics, Sook-Myung Women's University, Seoul 04310, Republic of Korea.
Nanotechnology. 2018 Sep 21;29(38):385601. doi: 10.1088/1361-6528/aad019. Epub 2018 Jun 29.
Graphene can acquire salient properties by the intercalated nano structures, and to functionalize the graphene as designed, understanding the growth kinetics of the nano structures is a prerequisite. In that regards, Kr atoms are selectively intercalated just below the surface graphene of C(0001) by the incidence of low energy Kr ions. The growth kinetics of the encapsulated Kr nano structures is investigated by both scanning tunneling microscopy and molecular dynamics simulations. The intercalation proceeds via defect sites, such as surface vacancies. At room temperature, the thermal diffusion of intercalated Kr is almost frustrated by the strain field of the encapsulating graphene layers, and the growth of Kr nano structures proceeds via the transient mobility of both the intercalating Kr atoms and previously intercalated Kr atoms that are mobilized by collision with the incident Kr ions. At the elevated temperatures where thermal diffusion becomes effective, some Kr nano structures disappear, releasing pressurized Kr atoms, while others coalesce to form blisters via the delamination of the adjacent graphene. Some of the larger blisters explode to leave craters of varying depths at the surface. In contrast to growth on the substrate, the growth of each encapsulated nano structure depends significantly on extrinsic variables, such as surface vacancies and local topography around the nano structure, that affect the Kr diffusion and limit the maximal Kr pressure.
石墨烯可以通过插入的纳米结构获得显著的性质,并对石墨烯进行设计功能化,了解纳米结构的生长动力学是先决条件。在这方面,通过低能 Kr 离子的入射,选择将 Kr 原子仅插入到 C(0001)表面石墨烯的下方。通过扫描隧道显微镜和分子动力学模拟研究了封装 Kr 纳米结构的生长动力学。插层通过缺陷部位进行,例如表面空位。在室温下,插层 Kr 的热扩散几乎被封装石墨烯层的应变场所阻碍,并且 Kr 纳米结构的生长是通过插入 Kr 原子的瞬态迁移以及与入射 Kr 离子碰撞而迁移的先前插入的 Kr 原子来进行的。在热扩散有效的较高温度下,一些 Kr 纳米结构消失,释放出受压的 Kr 原子,而另一些则通过相邻石墨烯的分层形成气泡而聚结。一些较大的气泡会爆炸,在表面留下不同深度的火山口。与在衬底上的生长相比,每个封装纳米结构的生长都显著取决于外部变量,例如表面空位和纳米结构周围的局部地形,这些变量影响 Kr 扩散并限制最大 Kr 压力。