Comprehensive Molecular-level Understanding of MgO Hydration through Computational Chemistry
Taichi Inagaki, Miho Hatanaka
TL;DR
This study addresses the molecular mechanism of MgO hydration to Mg(OH)$_2$ by modeling MgO(100) with a two-layer MgO/water interface using potential-scaling MD (PS-MD) and first-principles refinements. It reveals that dissociative water adsorption precedes Mg$^{2+}$ dissolution, which can be exothermic if vacancy stabilization is achieved by proximal protons, and proceeds via a highly heterogeneous, HB-network–driven process with a typical barrier of $12$ kcal/mol. Mg(OH)$_2$ nucleation occurs through dissolution-precipitation of Mg$^{2+}$ ions into the aqueous layer, forming Mg-OH chains that serve as nuclei, with well-ordered crystalline nuclei emerging in bulk water environments. The findings support the dissolution-precipitation mechanism as the dominant pathway and provide a foundational molecular framework for this class of complex solid-surface reactions, with implications for material design and industrial processes.
Abstract
The hydration of magnesium oxide (MgO) to magnesium hydroxide (Mg(OH)$_2$) is a fundamental solid-surface chemical reaction with significant implications for materials science. Yet its molecular-level mechanism from water adsorption to Mg(OH)$_2$ nucleation and growth remains elusive due to its complex and multi-step nature. Here, we elucidate the molecular process of MgO hydration based on structures of the MgO/water interface obtained by a combined computational chemistry approach of potential-scaling molecular dynamics simulations and first-principles calculations without any a priori assumptions about reaction pathways. The result shows that the Mg$^{2+}$ dissolution follows the dissociative water adsorption. We find that this initial dissolution can proceed exothermically even from the defect-free surface with an average activation barrier of $\sim$12 kcal/mol. This exothermicity depends crucially on the stabilization of the resulting surface vacancy, achieved by proton adsorption onto neighboring surface oxygen atoms. Further Mg$^{2+}$ dissolution then occurs in correlation with proton penetration into the solid. Moreover, we find that the Mg(OH)$_2$ nucleation and growth proceeds according to the dissolution-precipitation mechanism, rather than a solid-state reaction mechanism involving a direct topotactic transformation. In this process, Mg$^{2+}$ ions migrate away from the surface and form amorphous Mg-OH chains as precursors for Mg(OH)$_2$ nucleation. We also demonstrate that sufficient water facilitates the formation of more ordered crystalline nuclei. This computational study provides a comprehensive molecular-level understanding of MgO hydration, representing a foundational step toward elucidating the mechanisms of this class of complex and multi-step solid-surface chemical reactions.
