The wettability of graphite by a melt of zinc at 8.0 GPa in the temperature
range 1900-3100 K has been investigated experimentally, and the temperatur
e dependence of the wetting angle of graphite by the zinc melt determined.
A polycrystalline diamond layer has been revealed at the interface in the z
inc-graphite system in the diamond stability region. Metallographic and X-r
ay studies of zinc-carbon alloys obtained under high pressure have been car
ried out. The existence of the carbide ZnC2 was found, which participates i
n two three-phase, non-variant equilibria in the system. It is determined t
hat octahedral diamond crystals form in high-carbon alloys of zinc at the p
ressure of 8.0 GPa between 2100 and 2500 K. (C) 2000 Elsevier Science S.A.
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