M. Fattahi et al., RADIOLYSIS OF CLAY-WATER SYSTEMS - APPLICATION TO THE STORAGE OF RADIOACTIVE-WASTE, Journal de chimie physique et de physico-chimie biologique, 90(4), 1993, pp. 767-775
The long-term storage of radioactive waste buried in deep geological f
ormations raises numerous problems due to the radiolysis of the ground
. In order to evaluate the consequences of the radiolytic reactions wh
ich will take place in the ground, we are studying the effect of gamma
irradiation on the clay Fo-Ca 7 and on the clay water. Concerning irr
adiation of the solid phase, the lixiviation of Fe2+ in acidic water i
ncreases with the dose, probably as a consequence of structural modifi
cations.The non-irradiated clay water has reducing properties which ar
e diminished upon irradiation. Clay water contains several unidentifie
d efficient OH scavengers. As a consequence, the yield of hydrogen per
oxide is higher in clay water than in pure water. The mechanism of H2O
2 formation and decay has been studied in clay water and a kinetic sch
eme is proposed which allows the computation of the H2O2 amont for dos
es up to ca. 20,000 Gy. The efficient scavenging of OH free radicals i
s also consistent with a massive radiolytic formation of dihydrogen.