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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(WC13%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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