Uranium
[U(VI)] mining activity resulted in the discharge of uranium
containing acid wastewater. It is necessary for immobilizing the uranium
from wastewater to avoid its environmental pollution. In this work,
a novel hydrothermal mineralization strategy is proposed for uranium
stabilization. Three reaction systems such as Mg3(PO4)2 + UO2
2+, Mg2+ + PO4
3– + UO2
2+, and Mg2+ + PO4
3– + Mg3(PO4)2 + UO2
2+ were designed to investigate the uranium mineralization and stabilization
performance. The consumed molar quantities of magnesium and phosphate
were calculated to understand the mineralization mechanisms. The molar
ratios of Mg/U and P/U in the experimental results were in agreement
with those of thermodynamic calculation in the presence of dissolved
Mg2+ and PO4
3– under the hydrothermal
process. The calculated saturated index indicated the facile crystallization
of uranium into the saleeite and chernikovite through hydrothermal
mineralization at the pH value of 5 and 473 K. Crystallization into
saleeite and chernikovite contributed to uranium stabilization, resulting
in the negligible leaching rate of 5% due to the high crystallinity
of 97.23%. Thus, hydrothermal mineralization of uranium crystallization
into saleeite and chernikovite was promising for uranium stabilization
with long-term stability.