“…A robust understanding of the geochemical behavior of Sb is critical to dealing with existing contamination as well as controlling Sb mobilization from future activities. − Previous studies have shown that Sb(V) is typically the predominant Sb oxidation state in near-surface soils and sediments, often even under reducing flooded conditions. ,,, A strong association of Sb(V) with Fe(III) oxides [a term used here to include oxides, hydroxides, and (oxy)hydroxides] has been found by in situ observations of Sb enrichment in Fe(III) oxide minerals, ,, selective extraction analyses on soils/sediments, macroscopic sorption studies using pure mineral phases, ,− and synchrotron-based X-ray absorption spectroscopy (XAS) to characterize in situ Sb speciation. ,,, Sorption of Sb(V) by Fe(III) oxides therefore plays a critical role in controlling Sb behavior in natural environments (e.g., soils, sediments, oxidized ore bodies) as well as engineered systems (e.g., tailings and waste rock repositories, reactive barriers, water-treatment wetlands).…”