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Microstructure features of polycrystalline diamond synthesized directly from graphite under static high pressure

机译:静态高压下直接由石墨合成的多晶金刚石的微观结构特征

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摘要

Recently, ultra-hard polycrystalline diamond was synthesized from graphite by direct conversion under static high pressure. This paper describes the microstructure features of thus formed polycrystalline diamond. Transmission electron microscopy and electron diffraction have revealed that the polycrystalline diamond has a mixed texture of a homogeneous fine structure and a lamellar structure. The former structure consists of fine-grained diamond particles of several tens of nanometers across, which are randomly oriented. The latter structure has bending diamond layers, which may reflect deformed shapes of locally layered graphite of starting material. The experimental results suggest that diamond particles in the homogeneous fine structure are transformed from graphite in the diffusion process, while diamond layers in the lamellar structure are formed in the martensitic process from graphite via the hexagonal diamond phase. It is also noted that significant grain growth occurred at a high temperature of ∼2700°C, and the lamellar structure was segmentalized to form new grain boundaries.
机译:最近,通过在静态高压下直接转化由石墨合成超硬多晶金刚石。本文描述了这样形成的多晶金刚石的微观结构特征。透射电子显微镜和电子衍射表明,多晶金刚石具有均匀的精细结构和层状结构的混合织构。前一种结构由数十纳米宽的细晶粒金刚石颗粒组成,它们是随机取向的。后一种结构具有弯曲的金刚石层,其可以反映起始材料的局部层状石墨的变形形状。实验结果表明,均质精细结构的金刚石颗粒在扩散过程中从石墨转变而来,而层状结构的金刚石层在石墨的马氏体过程中通过六方金刚石相形成。还应注意的是,在约2700°C的高温下会出现明显的晶粒长大,并且层状结构被分割成新的晶界。

著录项

  • 来源
    《Journal of Materials Science》 |2004年第2期|445-450|共6页
  • 作者单位

    Advanced Materials RD Laboratories Sumitomo Electric Industries;

    Geodynamics Research Center Ehime University;

    Geodynamics Research Center Ehime University;

    Geodynamics Research Center Ehime University;

    Geodynamics Research Center Ehime University;

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  • 正文语种 eng
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