In this study, a Pb-containing (Y–Gd–Ce) rare-earth phosphate with the general chemical formula of (Y
0.1Pb
0.1Ce
0.4Gd
0.4)PO
4 was synthesized by two methods, namely the sol–gel and the metallurgical method. The sol–gel route consists of an external gel precipitation method, followed by two calcinations at 873 and 1473 K; and the dry route was a natural sintering at 1473 K of a mixture of micropowders activated at 873 K. The sol–gel route of synthesis gives a stronger and harder monazite mineral than the one obtained by the dry route of synthesis, both of them have a very low porosity. The sintering densities are 4.70 and 4.55 g/cm
3 for both the sol–gel and dry-route made monazites. The X-ray diffraction (XRD) analysis shows a main monoclinic crystalline structure for the two ways of synthesis. However, a secondary anorthic phosphate phase appears for the dry-route made monazite. Three leaching tests simulating several radiological events were performed: an acidic static test at different pH, a static water leach test in an argilous media and a dynamic microwave leach test.
For the whole of leaching processes, the kinetic of dissolution is fast. The acidic tests at pH 1, 4 and 7 gave few amounts of dissolved Ce in the leachates, about 5.668, 0.189 and 0.346 × 10−2 g/m2 day at the steady-state, respectively. The Pb was totally dissolved at pH 1 and 3. The sol–gel made monazite has a weak chemical durability in acidic media. In neutral pH, both the sol–gel and the dry-route made monazites give comparable values of Ce normalized dissolution rates (0.346 × 10−2 and 0.389 × 10−2 g/m2 day, respectively). The leaching in kaolin media decreases with a ten factor the amounts of leached Ce. However, for the whole of the leaching tests performed in neutral pH conditions, the monazite materials have a good chemical durability. The dissolution of the minerals under the microwave leaching is partially achieved, with only 3.5 % and 4.0 % of solubilised minerals, for both the sol–gel and dry-route made monazites, respectively, showing the good chemical durability of the studied monazite mineral.