Logo: to the web site of Uppsala University

Rhabdophane LnPO(4)center dot 0.667H(2)O (Ln = La to Dy) is an important precipitation-enrichment barrier to isolate actinides from groundwater. However, the bearing capacity of different actinides in rhabdophane has been poorly understood due to the complex coordination environment induced by water molecules. In this work, the precipitation behaviors of NdxSmxLa(1-2x)PO(4)center dot 0.667H(2)O (x = 0.1-0.5) solid solutions are systematically investigated to understand the simulated actinides occupancy and the chemical precipitation processes. The results show that Nd3+ and Sm3+ can be removed over 99% after 12 h in an approximate pH = 1 solution. NdxSmxLa12xPO4 center dot 0.667H(2)O single-phase has been observed by refined XRD, although the composition distribution of nanograins is extremely uneven. The distribution of simulated actinides can be homogeneous after prolonging reaction time to 12 days or sintering temperature over 1000.C. Both Nd3+ and Sm3+ are preferentially incorporated on non-hydrated lattice sites when x = 0.1. Besides, the chemical stability of La0.332Nd0.334Sm0.334PO4 center dot 0.667H(2)O rhabdophane is compared with associated monazite to understand the leaching activities of simulated actinides incorporated on hydrated and non-hydrated sites. The leaching rates of monazite are smaller than that of rhabdophane, suggesting that [LnO(9)] polyhedrons in monazite have a stronger energy threshold than [LnO(8)] and [LnO(8)center dot H2O] polyhedrons in rhabdophane.