We evaluated the growth and dissolution
behavior of the primary
α phase, Sr(NO3)2, and peritectic β
phase, Sr(NO3)2·4H2O, coexisting
in aqueous solutions above or below the peritectic temperature (T
p) in situ. Above T
p, when the two phases simultaneously grew in close proximity, the
metastable β phase began to partially dissolve where it approached
the α phase, although the remaining portion of the β phase
was still growing. Overall, the growing α phase could not approach
the dissolving face of the β phase; thus, a peritectic microstructure
with the α phase enclosing the β phase was not formed.
Conversely, below T
p, regardless of whether
the metastable α phase was growing or dissolving, the stable
β phase engulfed the α phase, resulting in a peritectic
microstructure with the β phase enveloping the α phase.
This demonstrated that it is necessary for the stable phase to dominate
the metastable phase in growth kinetics for bringing about a peritectic
microstructure consisting of the metastable phase in the core and
the stable phase in the periphery.