Extraction of the actinide-REE fraction and its subsequent incorporation into sparingly soluble crystalline phases (confinement matrices) is assumed in processing of spent nuclear fuel from high-level radioactive wastes (HLW). The chemical stability in the process of interaction with subsurface water governs the capability of a matrix phase to keep radionuclides from getting into the biosphere. In static experiments at 90 and 150°C, the chemical stability of ferrite garnets was investigated for three compositions with Th4+, Ce4+ and Gd3+ + serving as simulator components of the actinide fraction of HLW. Experiments were carried out in distilled water (pH 6.5), 0.01 M HCl solution (pH 2), and 0.01 M NaOH solution (pH 12). The behavior of ferrigarnet matrices depends on the acidity of the solution. In neutral and alkaline media, Th, Ce, and Gd are virtually not transferred into the liquid phase. Acid leaching promotes intense dissolution of garnet matrices. In this case, the leaching rate of Gd and Th from ceramics into the liquid phase is two orders of magnitude lower than the leaching rate of Ce because the Ce-doped phases contain less stable (relative to garnet) Ce-rich perovskite. Amorphization of the ferrigarnet structure due to 244Cm isotope decay leads to an increase in the leaching rate of Cm by no more than five times. In terms of radiation and chemical stability, ferrite garnets are not inferior to zirconolites and titanate pyrochlores. The experimental results suggest that garnet matrices can reliably immobilize actinides in subsurface repositories.
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