The fundamental processes of nucleation and crystallization
are
widely observed in systems relevant to material synthesis and biomineralization;
yet most often, their mechanism remains unclear. In this study, we
unravel the discrete stages of nucleation and crystallization of Fe3(PO4)2·8H2O (vivianite).
We experimentally monitored the formation and transformation from
ions to solid products by employing correlated, time-resolved in situ and ex situ approaches. We show
that vivianite crystallization occurs in distinct stages via a transient
amorphous precursor phase. The metastable amorphous ferrous phosphate
(AFEP) intermediate could be isolated and stabilized. We resolved
the differences in bonding environments, structure, and symmetric
changes of the Fe site during the transformation of AFEP to crystalline
vivianite through synchrotron X-ray absorption spectroscopy at the
Fe K-edge. This intermediate AFEP phase has a lower water content
and less distorted local symmetry, compared to the crystalline end
product vivianite. Our combined results indicate that a nonclassical,
hydration-induced nucleation and transformation driven by the incorporation
and rearrangement of water molecules and ions (Fe2+ and
PO4
3–) within the AFEP is the dominating
mechanism of vivianite formation at moderately high to low vivianite
supersaturations (saturation index ≤ 10.19). We offer fundamental
insights into the aqueous, amorphous-to-crystalline transformations
in the Fe2+–PO4 system and highlight
the different attributes of the AFEP, compared to its crystalline
counterpart.