Herein, we systematically investigated the mechanisms of Å OH production and arsenic (As(III)) oxidation induced by sulfur vacancy greigite (Fe 3 S 4 ) under anoxic and oxic conditions. Reactive oxygen species analyses revealed that sulfur vacancy-rich Fe 3 S 4 (SV-rich Fe 3 S 4 ) activated molecular oxygen to produce hydrogen peroxide (H 2 O 2 ) via a two-electron reduction pathway under oxic conditions. Subsequently, H 2 O 2 was decomposed to Å OH via the Fenton reaction. Additionally, H 2 O was directly oxidized to Å OH by surface high-valent iron (Fe(IV)) resulting from the abundance of sulfur vacancies in Fe 3 S 4 under anoxic/oxic conditions. These differential Å OH-generating mechanisms of Fe 3 S 4 resulted in higher Å OH production of SV-rich Fe 3 S 4 compared to sulfur vacancy-poor Fe 3 S 4 (SV-poor Fe 3 S 4 ). Moreover, the Å OH production rate of SV-rich Fe 3 S 4 under oxic conditions (19.3 ± 1.0 lMh À1 ) was 1.6 times greater than under anoxic conditions (11.8 ± 0.4 lMh À1 ). As(III) removal experiments and X-ray photoelectron spectra (XPS) showed that both Å OH production pathways were favorable for As(III) oxidation, and a higher concentration of As(V) was immobilized on the surface of SV-rich Fe 3 S 4 under oxic conditions. This study provides new insights concerning Å OH production and environmental pollutants removal mechanisms on surface defects of Fe 3 S 4 under anoxic and oxic conditions.