Ra. Pushkareva et al., Infrared spectroscopic study of gamma-radiation-induced hydrogen isotope exchange in clay minerals, RADIOCHEMIS, 41(6), 1999, pp. 599-603
It was demonstrated by infrared spectroscopy that gamma-radiation catalyzes
hydrogen isotope exchange in crystal hydroxyls of kaolinite and montmorill
onite (bentonite). At a gamma-radiation dose of 1.2 x 10(7) Gy about 10-15%
of hydroxyls are involved in deuterium exchange. Radiolytic deuterium exch
ange is observed in all the major types of crystal hydroxyls of kaolinite e
ven in the initial stages of irradiation. Lowering dose by an order of magn
itude (to 10(6) Gy) decreases the degree of exchange by a factor of about 3
.