Water adsorption on the MnO(100) single crystal surface was quantitatively
monitored using chemical shifts in the O 1s core level spectra. We find tha
t the initial reactions at low water vapor pressures of 10(-8)-10(-4) Torr
are limited to a small fraction of a monolayer and involve dissociation of
water at or near defect centers resulting in surface hydroxyls. Even at the
se low pressures, there is an increase in water adsorption with increasing
dosing time. Water uptake increases dramatically for vapor pressures betwee
n 10(-4) and 10(-2) Torr and then stabilizes above 10(-2) Torr. At this pre
ssure, hydroxyl coverages slightly exceed a monolayer. Hydroxyl species for
med on this surface are unstable and can be removed by annealing to 200 deg
rees C. These data are compared with those from similar studies of the inte
raction of water vapor with MgO(100) and the surfaces of iron oxides (alpha
-Fe2O3 and Fe3O4), and some quantitative similarities and differences are d
iscussed. In particular, the role of cooperative interactions in the conden
sed water overlayer in surface hydroxylation is emphasized.