Abstract

Traditionally, the enhancement of nucleation rates in the presence of heterogeneous surfaces in crystallisation processes has been attributed to the modification of the interfacial energy of the system according to the classical nucleation theory. However, recent developments have shown that heterogeneous surfaces instead alter the pre-exponential factor of nucleation. In this work, the nucleation kinetics of glycine and diglycine in aqueous solutions have been explored in the presence and absence of a heterogeneous surface. Results from induction time experiments show that the presence of a heterogeneous surface increases the pre-exponential factor by 2-fold or more for both glycine and diglycine, while the interfacial energy remains unchanged for both species. This study suggests that the heterogeneous surface enhances the nucleation rate via hydrogen bond formation with both glycine and diglycine. This is verified by hydrogen bond propensity calculations, molecular functionality analysis, and calculation of the time taken for a solute molecule to attach to the growing nucleus, which is an order of magnitude shorter than the estimated lifetime of the hydrogen bond. The effect of the heterosurface is of greater magnitude for diglycine than for glycine, which may be due to the heightened molecular complementarity between the hydrogen bond donor and acceptor sites on diglycine and the heterosurface.

Highlights

  • The universal nature of crystallization has been explored in every aspect of sDcOieI: n10c.1e0,39f/rDo1FmD00101A organics to inorganics to bio-organics, and from atmospherics to minerals

  • The Metastable zone width (MSZW) of glycine is narrower in aqueous solution but wider when the initial glycine solution has a greater antisolvent mass fraction

  • The homogeneous and heterogeneous nucleation of glycine and diglycine in the absence and presence of glass beads was performed from aqueous solution

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Summary

Introduction

The universal nature of crystallization has been explored in every aspect of sDcOieI: n10c.1e0,39f/rDo1FmD00101A organics to inorganics to bio-organics, and from atmospherics to minerals. Crystallisation is a two-step process, with nucleation being the initial step of forming a stable new phase from a supersaturated medium. Nucleation is subsequently followed by growth as well as ripening, agglomeration, aggregation, and phase transformation. In both steps, supersaturation is the driving force, caused by the difference between the actual concentration of the crystallizing solute and the saturation concentration (solubility). Since physical properties of the crystals such as shape, structure, defects, and polymorphism are determined at the nucleation stage, this step is usually rate limiting for the crystallisation process.[1,2]

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