Gold deposited on the FeO(001) surface at room temperature was
studied using Scanning Tunneling Microscopy (STM) and X-ray photoelectron
spectroscopy (XPS). This surface forms a ()R45
reconstruction, where pairs of Fe and neighboring O ions are slightly displaced
laterally producing undulating rows with narrow' and wide’ hollow sites. At
low coverages, single Au adatoms adsorb exclusively at the narrow sites, with
no significant sintering up to annealing temperatures of 400 C. We
propose the strong site preference to be related to charge and orbital ordering
within the first subsurface layer of FeO(001)-($\sqrt2 \times
\sqrt2^{\circ}$. Due to its high thermal stability, this could prove an
ideal model system for probing the chemical reactivity of single atomic
species.

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