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Using a very recent multi-part equation of state mannequin for carbon 37 , we expect the temperatures of the states, which stay in the graphite part in the order of four,000 okay, 4,000-6,000 k for the diamond data and 6,000-7,000 okay for the measurements, which present the lonsdaleite construction. For 19 gpa, diffraction exhibits graphite, which is mainly compressed alongside the c axis, together with some chilly material from the rear aspect of the sample not reached by the shock.
Further compression then leads to states of upper entropy and thus temperature compared with shock compression of the upper density pyrolytic samples to the same stress 30 for porous polycrystalline graphite, we report nanosecond formation of diamond with a transition threshold at barely lower strain in contrast with the pyrolytic samples.
