“…Whereas in anhydrous environments, it appears that the (0 0 1) surface displays several types of terminations depending on the partial pressure of oxygen and temperature [28,38], including the stoichiometric Fe-termination [37,36] and in coexistence with Otermination [39,30,26,31,29,34,32], and exclusively O-terminations [28]. Because of the low P H 2 O to hydroxylate the hematite (0 0 1) surface [16,41], the surface hydroxyl groups may form spontaneously during sample transfer or characterization.…”