“…These models can provide more detailed and fundamentally relevant information about the behavior of water in porous carbons. Typically these models [16][17][18][19][20][21][22] can predict the concentration of surface functional groups, the molecular size of water clusters, and the water adsorption capacity in the micropores as well as on the surface functional groups, and also estimate equilibrium rate constants. Such models are, for example, the Dubinin-Astakov (DA) equation [16], the Talu-Meunier equation [17], the cooperative multimolecular sorption (CMMS) theory [18], and the D.D.…”