Nucleation
of barite (BaSO4) has broad implications
in geological, environmental, and materials sciences. While impurity
metals are common, our understanding of how they impact nucleation
remains dim. Here, we used classical optical microscopy compared to
fast X-ray nanotomography (XnT) to investigate heterogeneous nucleation
of barite on silica in situ with Sr2+ as an impurity ion.
The observed barite nucleation rates were consistent with classical
nucleation theory (CNT), where barite crystals displayed a nonuniform
size distribution, exhibiting distinct morphologies and incubation
periods in Sr-free solutions. While undetectable with optical microscopy,
nanotomography revealed that addition of Sr2+ enhances
nucleation rates driven by the pre-factor in CNT, likely because both
adsorbed Ba2+ and Sr2+ act as precursor sites
on which nucleation occurs. Sr2+ simultaneously inhibits
growth, however, leading to a homogeneous distribution of smaller
crystals. This finding will enable an improved predictive understanding
of nucleation in natural and synthetic environments.