Li Wenqi,Ding Xingeng,Meng Cheng,Ren Chunrong,Wu Huating,Yang Hui
Rare earth phosphates (REPO 4 ) are considered as promising materials to immobilize the high-level radioactive waste. In the paper, Gd 1− x Yb x PO 4 ( x = 0, 0.1, 0.2, 0.4, 0.6, 0.8 and 1.0) series were prepared via the solid-state reaction using Gd as the surrogate for minor actinide Am and Cm, and the structure, phase transformation and morphology were characterized by XRD, Raman, TEM and SEM. With the calcination temperature ranging from 1200 to 1500 °C, the coexisted phases of monazite- and xenotime-type structure are observed in Gd 0.9 Yb 0.1 PO 4 . The monophasic xenotime-type Gd 0.9 Yb 0.1 PO 4 is obtained at 1600 °C. The monazite → xenotime transformation of Gd 1− x Yb x PO 4 depends on the substitution of Gd 3+ by Yb 3+ ions. With the decrease in Gd 3+ content, the gradual changes of FWHM and the hypsochromic shift of P-O symmetrical stretching vibration (Vs) are observed in the Raman spectra, indicating that the distortion of PO 4 tetrahedra occurs during the phase transformation process. The chemical durability test is measured by the ASTM product consistency test leaching method, and the normalized mass loss (NL Gd ) of Gd and (NL Yb ) of Yb is extremely low and shown in the order of 10 −6 –10 −7 g/m 2 for all the ceramics.
Cheng Meng,Xingeng Ding,Junchuan Zhao,Chunrong Ren,Huiqin Fu,Hui Yang
Rare-earth phosphates (REPO 4 ) represent one candidate to contain minor actinides separated from used nuclear fuel. In this work, the Gd 1 − x Yb x PO 4 (0 ≤ x ≤ 1) series is synthesized via conventional solid-state reaction using Gd as the surrogate for trivalent actinides (Am, Cm), with microstructure/phase structure characterized by XRD , XPS, HRTEM and SEM as well. Solid solutions of monazite- and xenotime-type compounds are observed in the system. The structural boundary between two phases is based on the experimental temperature. The monazite → xenotime transformation is most likely to occur on a (2 0 0) monazite plane along the [0 2 0] zone. The pure xenotime-type crystalline phase with Gd 0.9 Yb 0.1 PO 4 composition is obtained at 1600 °C.