正二十面体金刚石的形成及其计算机模拟

Formation of an icosahedral diamond crystal and its computer simulation

  • 摘要: 采用热丝化学气相沉积(HFCVD)法,以甲烷和氢气为反应气体,在YG13(WC13%Co)硬质合金基体上制备了金刚石膜。膜中存在大量五重对称结构的正二十面体金刚石晶粒(IDC)。当尺寸较小时晶粒为较完整的正二十面体形状,尺寸达微米级后晶粒为带有“沟槽”或“凹坑”的变种正二十面体形状。研究了IDC的形成机制,并进行了计算机模拟。结果表明:对于四面体立方结构来说,IDC的111孪晶面与正常111孪晶面相比存在2.87o的差异,孪晶面两侧原子几何位置失配,使其成为畸变孪晶面,这种畸变孪晶面导致IDC晶粒存在“凹坑”和“沟槽”;IDC的晶核是正十二面体烷(C20H20)。

     

    Abstract: Icosahedral diamond crystals (IDCs) were found in chemical vapour deposited diamond by a field emission scanning electron microscope, using. YG13 (cemented tungsten carbide containing 13% of Co) as a substrate. It is found that the nanometer sized IDCs are in the shape of a nearly perfect icosahedron and the micrometer sized IDCs are in the shape of a icosahedron with dimples or grooves. A simulation on atomistic scale is performed by assuming a nucleation-growth model in order to elaborate the mechanism of IDC formation. Results show that the nucleus of IDCs is dodecahedrane, C20H20. For the tetrahedral cubic packing, the dihedral angle of 111 facets of IDCs is 2.87o larger than that of the normal 111 twin plane. The geometric position of the bilateral atoms on the 111 twin plane of IDCs is mismatched, resulting in a distorted twin plane (DTP) in IDCs. The high energy of DTP induces the dimples or grooves that occurred in IDCs.

     

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