Thermodynamic calculations of graphite yield at the interaction of gas
eous components of the C-H-O system were performed. Their results prov
ed to be in satisfactory agreement with experimental data published on
the lower concentration boundary of the diamond deposition region, Th
e calculations indicate an influence of the substrate temperature, tot
al pressure, and concentrations of inert and active additives on this
boundary's location. These data confirm an inference that a diamond de
position mechanism might include spontaneous growth-etch cycles due to
fluctuations of the gas concentrations. (C) 1996 American Institute o
f Physics.