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Stability of diamond-like carbon in hydrothermal conditions

机译:类金刚石碳在水热条件下的稳定性

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The effect of water at high temperature and pressure (hydrothermal conditions) in a tetrahedral amorphous carbon (ta-C) type of diamond-like carbon has been investigated. At temperatures over 200 deg C, the action of water leads to the sp~3 to sp~2 conversion in diamond-like carbon rich in sp~3 bonds and the almost complete transformation into sp~2 bonded amorphous carbon (a-C) at temperatures below 600 deg C. After treatment at 600 deg C, open porous structures of interconnected multiwall cells were observed. The formation of curved graphitic shells is explained by the partial etching/dissolution of the carbon film and precipitation from the reactive hydrothermal fluid. The high ratio of sp~3 carbon nuclei present does not seem to promote the precipitation of additional sp~3-bonded carbon from the supercritical fluid, rather the growth of crystalline multiwall graphitic layers with sp~2-bonding, as demonstrated with micro and macro-Raman measurements.
机译:研究了水在高温高压(水热条件)下对四面体无定形碳(ta-C)型类金刚石碳的影响。在超过200摄氏度的温度下,水的作用导致富含sp〜3键的类金刚石碳中的sp〜3到sp〜2转化,并在该温度下几乎完全转化为sp〜2键的无定形碳(aC)低于600℃。在600℃下处理后,观察到互连的多壁电池的开孔结构。弯曲的石墨壳的形成可以通过碳膜的部分蚀刻/溶解和反应性热液中的沉淀来解释。存在的高比例的sp〜3碳核似乎并未促进超临界流体中额外的sp〜3键合碳的沉淀,而是通过sp〜2键合形成的结晶多壁石墨层的生长,这在微观和微观上都得到了证明。宏观拉曼测量。

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