Progress beyond the state of the art has been achieved, typically by employing a combination of theory, simulation, and experiments.
At the microscale, the understanding of the relevant secondary nucleation mechanisms has been significantly deepened through the development of mechanistic models. These models have guided our experimental work, as they have revealed the important role of agitation and of the crystal’s surface properties in secondary nucleation. The availability of mechanistic models instead of empirical ones is expected to lead to significant improvements in the understanding of particularly of continuous crystallization.
In this spirit, we developed a new monitoring device that is able to observe the early stages of nuclei formation at the nano-scale, in the case of both secondary and primary nucleation, and to help estimating nucleation rates, which are notoriously difficult to obtain.
At the process-scale, we made significant progress in understanding the behavior of continuous crystallization processes of compounds that exhibit multiple solid forms (e.g. chiral and polymorphic species). In particular, we derived a new theory that predicts the stable steady state in continuous crystallizers as a function of operating conditions and crystallization kinetics. This theory, supported by experiments and simulations, is useful in providing ranges of operating conditions in which individual pure solid forms, both stable and metastable, are crystallized.
Finally, considering the crystallization of chiral compounds, a breakthrough has been achieved in clarifying the governing mechanism of solid-state-deracemization, which refers to a type of crystallization process in which a racemic suspension is transformed into an enantiopure one. Through the combination of theory, simulation, and experiments we could show that its underlying mechanism is both simple and ubiquitous and indeed, it does not even require secondary nucleation. This promises to support the further use of this process in industry, and to conceptualize the role it might have played in the origin of homochirality on Earth.