Hematite (α-Fe2O3) has been identified as the dominant structure of the outermost layer of the passive film formed on iron surfaces in alkaline environment but chloride has been suggested to play a major role in the depassivation of this passive film under the same conditions. Here we study the effects of OH and Cl adsorption as well as co-adsorption at different coverages on the structure of α-Fe2O3 Fe-terminated (0001) surface using DFT+U. The adsorption of both OH and Cl alters the structure of the surface, by effecting mostly the positions of the top two layers. The structural change increases with coverage for two adsorbates on a (1x1) surface and the study on a larger (2x2) surface shows that the effects are localized. The large effect of the OH and coadsorption of OH and Cl on the surface suggest that OH could play an important role in the Clinduced depassivation process.