“…These findings established that water constituents are chemically associated to the surface, allowing for the formation of hydrated surface species. Furthermore, ''chemisorption" of water on the calcite surface was also demonstrated by earlier thermogravimetric studies (Morimoto et al, 1980;Ahsan, 1992). Nevertheless, it is not yet possible to ascertain, by any of these analytical techniques, whether hydration occurs through adsorption of dissociated or undissociated water molecules because these are unable to detect hydrogen atoms, and thus, hydroxyl ions cannot be distinguished from adsorbed H 2 O molecules.…”