In this work, we study the abiotic remineralization of ferrihydrite under reducing conditions, obtained by adding zero-valent iron to a suspension of ferrihydrite particles. Under similar conditions, the system (ferrihydrite and zero-valent iron) proceeded along two different transformation pathways differentiated by whether a magnetic stirrer or an overhead stirrer was used for mixing. X-ray diffraction characterization of the solid products showed that magnetite was the sole product of ferrihydrite transformation when a magnetic stirrer was used, whereas both goethite and magnetite were formed when an overhead stirrer was used. The system also behaved differently in terms of transformation kinetics and amount of magnetite formed. The quantification of magnetite generated was performed using a procedure developed in this study. The role of four mechanisms was investigated to explain these observed differences, namely - (i) presence/absence of high local Fe2+ concentrations, (ii) mechanical abrasion, (iii) presence/absence of a magnetic field, and (iv) presence/absence of a crystalline ZVI surface. Ferrous ions are expected to be concentrated near the magnetic bead on the magnetic stirrer as opposed to a more dispersed distribution on the overhead stirrer. This mechanistic study concluded that the presence of high local Fe2+ concentrations in the system leads to magnetite formation and the absence of the same leads to mixed goethite/magnetite or magnetite-free systems. These findings have significant implications for the mobilization of arsenic from iron (III) hydroxides as the conditions move from oxidizing to reducing, such as often occurs in engineered landfills and natural carbon-rich sediments.