1968
DOI: 10.1070/pu1968v011n03abeh003831
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Use of Nuclear Physics in Related Fields of Science and National Economy

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“…The existence of this pseudo-equilibrium region was at the basis of the method of synthesizing diamond starting from carbon saturated solutions of molten iron, silver, or silicates. In 1938, Rossini and Jessup [58] of the U.S. Bureau of Standards used accurate thermodynamic data to estimate that at 0 K the lowest pressure at which diamond would be stable against graphite is around 1.3 GPa, and around 2 GPa at 500 K. In 1939, the Russian scientist Leipunskii [59] published a review of the problem of diamond synthesis. On the basis of thermodynamic data, he suggested that the melting curve of graphite might be at about 4000 K, with possibly some increase with pressure.…”
Section: The History Of Carbon Phase Diagrammentioning
confidence: 99%
“…The existence of this pseudo-equilibrium region was at the basis of the method of synthesizing diamond starting from carbon saturated solutions of molten iron, silver, or silicates. In 1938, Rossini and Jessup [58] of the U.S. Bureau of Standards used accurate thermodynamic data to estimate that at 0 K the lowest pressure at which diamond would be stable against graphite is around 1.3 GPa, and around 2 GPa at 500 K. In 1939, the Russian scientist Leipunskii [59] published a review of the problem of diamond synthesis. On the basis of thermodynamic data, he suggested that the melting curve of graphite might be at about 4000 K, with possibly some increase with pressure.…”
Section: The History Of Carbon Phase Diagrammentioning
confidence: 99%