The variation of the concentration of C-14 in graphite subjected to vi
bratory milling in the presence of heavy (or light) water is investiga
ted using methods of radiocarbon beta-spectral analysis. It is discove
red that the C+D2O system exhibits a statistically significant increas
e in the beta counting rate in comparison to the C+H2O system milled u
nder similar conditions. A quantitative model of the transmutation of
the C-13 isotope into the C-14 isotope involving an interaction of mul
tiphonon excitations with deuterons in the graphite crystal lattice in
the presence of background thermal neutrons is proposed. (C) 1997 Ame
rican Institute of Physics.