TY - JOUR
AU - Arinicheva, Yulia
AU - Gausse, Clemence
AU - Neumeier, Stefan
AU - Brandt, Felix
AU - Rozov, Konstantin
AU - Szenknect, Stéphanie
AU - Dacheux, Nicolas
AU - Bosbach, Dirk
AU - Deissmann, Guido
TI - Influence of temperature on the dissolution kinetics of synthetic LaPO4-monazite in acidic media between 50 and 130 °C
JO - Journal of nuclear materials
VL - 509
SN - 0022-3115
CY - Amsterdam [u.a.]
PB - Elsevier Science
M1 - FZJ-2018-04024
SP - 488-495
PY - 2018
AB - Single-phase monazite-type ceramics are discussed as waste forms for the safe disposal of surplus plutonium or separated minor actinides. To gain a deeper insight into the mechanism governing the dissolution of monazite-type compounds, the dissolution kinetics of synthetic LaPO4-monazite was systematically studied by dynamic dissolution experiments carried out in the temperature range from 50 to 130 °C in acidic media (0.01 M HNO3). The dissolution rates at far from equilibrium conditions increased from 3.2 × 10−5 g m−2 d−1 at 50 °C to 2.5 × 10−4 g m−2 d−1 at 130 °C. Two different temperature regions were observed, in which the normalised dissolution rates of LaPO4 have a diverging temperature dependence, indicating two different mechanisms of dissolution: namely surface-controlled dissolution (T = 50–90 °C; Ea = 44 kJ mol−1) and transport-controlled dissolution (T = 90–130 °C; Ea = 7.5 kJ mol−1). Complementary thermodynamic modelling studies of the dissolution of LaPO4 at the experimental conditions show that La-rhabdophane (LaPO4·0.667H2O) is the thermodynamically favoured phosphate phase in aqueous environments below about 100 °C. Apparently, the hydration of monazite and the formation of a thin surface layer consisting of rhabdophane is an intermediate step controlling the dissolution kinetics of the LaPO4 monazite ceramics in low temperature aqueous environments.Keywords
LB - PUB:(DE-HGF)16
UR - <Go to ISI:>//WOS:000442483300054
DO - DOI:10.1016/j.jnucmat.2018.07.009
UR - https://juser.fz-juelich.de/record/849928
ER -