The equilibrium curve between graphite and diamond is calculated up to 1200°K by making use of some new experimental data. The justification for extrapolating the values to higher temperatures is given. The equilibrium pressures below 1200° are shown in a table, while above 1200°K the curve can be represented by the equation P ats = 7000 + 27 T (°K), which should be accurate to within about 5%.
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Berman et al. (1955) studied this question.
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