Interfaces between water and materials are ubiquitous
and are crucial
in materials sciences and in biology, where investigating the interaction
of water with the surface under ambient conditions is key to shedding
light on the main processes occurring at the interface. Magnesium
oxide is a popular model system to study the metal oxide–water
interface, where, for sufficient water loadings, theoretical models
have suggested that reconstructed surfaces involving hydrated Mg2+ metal ions may be energetically favored. In this work, by
combining experimental and theoretical surface-selective ambient pressure
X-ray absorption spectroscopy with multivariate curve resolution and
molecular dynamics, we evidence in real time the occurrence of Mg2+ solvation at the interphase between MgO and solvating media
such as water and methanol (MeOH). Further, we show that the Mg2+ surface ions undergo a reversible solvation process, we
prove the dissolution/redeposition of the Mg2+ ions belonging
to the MgO surface, and we demonstrate the formation of octahedral
[Mg(H2O)6]2+ and [Mg(MeOH)6]2+ intermediate solvated species. The unique surface,
electronic, and structural sensitivity of the developed technique
may be beneficial to access often elusive properties of low-Z metal
ion intermediates involved in interfacial processes of chemical and
biological interest.