Abstract
According to classical nucleation theory, nucleation from solution involves the formation of small atomic clusters. Most formulations of classical nucleation use continuum "droplet" approximations to describe the properties of these clusters. However, the discrete atomic nature of very small clusters may cause deviations from these approximations. Here, we present a self-consistent framework for describing the nature of these deviations. We use our framework to investigate the formation of "polycube" atomic clusters on a cubic lattice, for which we have used combinatoric data to calculate the thermodynamic properties of clusters with 17 atoms or less. We show that the classical continuum droplet model emerges as a natural approach to describe the free energy of small clusters, but with a size-dependent surface tension. However, this formulation only arises if an appropriate "site-normalized" definition is adopted for the free energy of formation. These results are independently confirmed through the use of Monte Carlo calculations. Our results show that clusters formed from sparingly soluble materials (μM solubility range) tend to adopt compact configurations that minimize the solvent-solute interaction energy. As a consequence, there are distinct minima in the cluster-size-energy landscape that correspond to especially compact configurations. Conversely, highly soluble materials (1M) form clusters with expanded configurations that maximize configurational entropy. The effective surface tension of these clusters tends to smoothly and systematically decrease as the cluster size increases. However, materials with intermediate solubility (1 mM) are found to have a balanced behavior, with cluster energies that follow the classical "droplet" scaling laws remarkably well.
Highlights
The nucleation of particles from solution is a critical step in many processes of mineral precipitation, materials synthesis, and nanoparticle generation
We show that the classical continuum droplet model emerges as a natural approach to describe the free energy of small clusters, but with a size-dependent surface tension
In this paper we have investigated the energetic properties of small atomic clusters in a lattice solution
Summary
The nucleation of particles from solution is a critical step in many processes of mineral precipitation, materials synthesis, and nanoparticle generation. Most classical nucleation models treat these small clusters as “droplets” of the precipitating phase so that their thermodynamic work of formation can be approximated with simple geometric scaling laws. In some cases the critical cluster size that comprises a nucleus may contain just tens of atoms or less. This is especially common for the highly insoluble materials that form nanoparticles. In this size range, it seems likely that the energy landscape for cluster formation may deviate significantly from the classical scaling laws, but the nature of these deviations is generally unknown
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