“…[16,17] In recent years, a number of papers have appeared, tackling the complex task of developing models able to provide a reli-able description of the atomic details of this mineral interface. [18][19][20][21][22][23][24][25][26][27][28][29][30][31] Most of these studies focus on the interaction of hydrogen, water, or carbon dioxide with the (010) surface of forsterite (where both M sites are occupied by magnesium) as modeled either with interatomic potentials, [19,24] or with firstprinciple methods based on the density functional theory (DFT). [25,27,30,31] Of the latter, one presents a study on the adsorption of H 2 molecules on the (010) surface of forsterite performed at the hybrid meta-generalized gradient approximation (GGA) level of theory, though structures were optimized using interatomic potentials [27] ; four deal with the adsorption of either water molecules or H atoms and H 2 molecules on the same surface, simulated at the GGA [25,28,31] and B3LYP-D* [30] levels.…”