Rare earth carbonates play a significant
role in preparing
rare
earth oxides. This study examines the structure and composition of
amorphous dysprosium carbonate (ADC) precursors produced through chemical
precipitation. Next, how the amorphous phase changed throughout the
hydrothermal process is analyzed. The precursor is identified as the
Dy2(CO3)3·xH2O with spherical morphology (40 nm), as characterized
by TEM, XRD, TG-MS, and FT-IR. It was found that ADC will undergo
numerous morphological and structural transformations with the progress
of the hydrothermal treatment. First, a metastable Dy2(CO3)3·xH2O is formed,
and then a stable crystalline basic dysprosium carbonate Dy(OH)CO3 is obtained. The self-assembly of amorphous precursor units
results in 1D and 3D structures according to the theory of negative
ion coordination. The transformation mechanism of dysprosium carbonate
follows Ostwald’s rule of stages, where the metastable phase
dissolves and recrystallizes to form the stable basic dysprosium carbonate
phase.