We
present a theoretical study of the Henry constant for water
adsorbed on graphite decorated with functional groups at the edges
of the graphene layers. A general expression for the Henry constant
is developed to describe the initial adsorption on the basal plane,
functional groups, and confinement in micropores. To shed further
light on the role of functional groups, we have investigated the effects
of partial charge, acidity and basicity, orientation, and separation
between functional groups. Our main conclusions are (1) the strength
of adsorption is sensitive to the accessibility of water to the functional
groups, (2) a basic functional group can be as strong as an acidic
functional group, (3) the affinity varies significantly with orientation
and the separation between the functional groups, and (4) adsorption
in microporous crevices may compete with functional group adsorption
at very low loadings. While thermodynamics suggests that a Henry law
region should always exist at low loading, this is not always observed
in water/carbon systems because of the broad energy distribution of
the possible adsorption sites (functional group, basal plane, and
confinement) or because the Henry law region, corresponding to the
strongest adsorbing sites, falls well below the measurable pressure
range.