We
present a theoretical investigation of the prismatic (011̅0)
surface of troilite in an oxidizing environment, which aims to elucidate
the presence of oxygen detected experimentally in the pyrrhotite Fe1–x
S nanoparticles. We find that atomic
oxygen adsorbs in Fe–O–Fe bridging motifs, which are
thermodynamically stable under ambient conditions. During the first
oxidation steps, the formation of the S–O bond is less favored
than Fe–O, suggesting that the sulfur oxides detected experimentally
form only subsequently. We predict, moreover, that substitution of
sulfur for oxygen can occur. The appearance of Fe–O–Fe–O–Fe
bridging motifs due to successive adsorptions points toward a clustering
growth of the oxidic units. In agreement with the experimental observations,
the oxidation of troilite is exothermic, where the equilibrium between
adsorption and substitution is influenced by the presence of Fe vacancies.