Antimony mobility in sulfidic systems: Coupling with
Transformation of the Sb-bearing ferrihydrite to more crystalline Fe(III) oxides in this experiment can be considered as a consequence of Fe(II) interaction with the ferrihydrite. It is well recognized that goethite forms during the Fe(II)-catalyzed conversion of ferrihydrite (e.g. Boland et al., 2014, Burton et al., 2019, Hansel et al., 2005, Jones et al., 2017, Karimian et al., 2019b, Latta
