2012
DOI: 10.1007/s00269-012-0510-3
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Influence of graphite crystallinity on the microtexture of nano-polycrystalline diamond obtained by direct conversion

Abstract: Nano-polycrystalline diamond (NPD) is a super-hard pure polycrystalline aggregate of nano-diamonds and has a characteristic microtexture composed of a mixture of granular and lamellar crystals. We investigated the origin of the unique microtexture and the influence of the crystallinity of initial graphite sources on the resulting microtexture of NPDs. Polycrystalline graphite rods used for NPD synthesis were found to consist of coke-derived relatively large crystals and pitch-derived nanocrystalline particles.… Show more

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Cited by 32 publications
(26 citation statements)
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References 19 publications
(22 reference statements)
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“…Such microtexture and coaxial relations indicate that the phase transition from graphite to cubic diamond via hexagonal diamond intermediate occurred essentially by martensite-like mechanism at the studied PT conditions. This is because if the phase transition occur by nucleation and growth mechanism, both the original layered texture of graphite starting material and lattice relations among the three phases would not be preserved, like the case of nanopolycrystalline diamond which consists mostly of randomly oriented granular crystals [7][8][9]11]. The martensite-like transformation of graphite to hexagonal diamond and cubic diamond is thought to occur by the sliding and/or buckling of graphite planes (e.g., [15,16]) and predominantly takes place when well-crystalline graphite is used as a starting material [8,9].…”
Section: Resultsmentioning
confidence: 99%
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“…Such microtexture and coaxial relations indicate that the phase transition from graphite to cubic diamond via hexagonal diamond intermediate occurred essentially by martensite-like mechanism at the studied PT conditions. This is because if the phase transition occur by nucleation and growth mechanism, both the original layered texture of graphite starting material and lattice relations among the three phases would not be preserved, like the case of nanopolycrystalline diamond which consists mostly of randomly oriented granular crystals [7][8][9]11]. The martensite-like transformation of graphite to hexagonal diamond and cubic diamond is thought to occur by the sliding and/or buckling of graphite planes (e.g., [15,16]) and predominantly takes place when well-crystalline graphite is used as a starting material [8,9].…”
Section: Resultsmentioning
confidence: 99%
“…This is because if the phase transition occur by nucleation and growth mechanism, both the original layered texture of graphite starting material and lattice relations among the three phases would not be preserved, like the case of nanopolycrystalline diamond which consists mostly of randomly oriented granular crystals [7][8][9]11]. The martensite-like transformation of graphite to hexagonal diamond and cubic diamond is thought to occur by the sliding and/or buckling of graphite planes (e.g., [15,16]) and predominantly takes place when well-crystalline graphite is used as a starting material [8,9]. The sample synthesized at 15 GPa and 2300 ∘ C consists mostly of cubic diamond and of a small amount of hexagonal diamond, which are also in the coaxial relation stated above, suggesting that the conversion of graphite to diamonds fully completes above 1800 ∘ C at this pressure.…”
Section: Resultsmentioning
confidence: 99%
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“…The starting material is pure consolidated graphite (>99.99), which is made of a mixture of minute (a few micrometers) graphite crystals (flakes derived from "cokes") and poorly crystallized fine graphite powders (derived from "pitches") as described in Ohfuji et al (2012).…”
Section: Methodsmentioning
confidence: 99%