Our understanding of the process
of mineral nucleation is starting
to evolve from the solely thermodynamical aspects in classical nucleation
theory toward a mechanistic study of reactions influenced by solvation
structures of ions and their dynamics. A knowledge of how these atomic
and molecular interactions respond to changing solution composition
and/or the nature of an interface will form a fundamental foundation
to understand rate-limiting reactions and processes for nucleation
and growth. Here, we review recent advances from multidisciplinary
experimental and computational approaches of the structure and dynamics
of aqueous solutions and mineral–liquid interfaces that will
influence rates of nucleation (and growth behavior) both homogeneously
in aqueous solutions and heterogeneously at mineral–liquid
interfaces. These processes include structure (and extent) of solute
clustering, solvent degrees of freedom, and the presence of noninnocent
charge-balancing ions, all of which can drive the selectivity and
exert control over nucleation mechanisms. Similar controlling reactions
can also occur at interfaces with the added complexities of how solute
ions interact with and assemble on surface sites and use different
mechanisms from bulk solutes, such as lateral solvent exchanges between
distinct surface sites. To gain a predictive understanding of nucleation
chemistry, we emphasize several key knowledge gaps that will need
to be addressed in this field and highlight the importance of combining
computations and experiments.