The coprecipitation of magnetite (Fe3O4)
with arsenic (As) is a potential remediation technique for As-contaminated
groundwater that can be applied to meet increasingly stringent As
drinking water limits. However, knowledge of the fate of As coprecipitated
with magnetite during aging for extended periods is lacking, which
is critical to predict the long-term efficiency of this As treatment
strategy. In this work, I combined aqueous As measurements with solid-phase
characterization by synchrotron-based Fe and As K-edge X-ray absorption
spectroscopy (XAS) to track the transformation of magnetite and the
speciation of coprecipitated As(V) or As(III) for up to a year in
oxic or anoxic conditions. It was determined that the initial magnetite
particle increased in crystallinity for all aging experiments, but
some differences in solid-phase Fe speciation were detected depending
on aging conditions. For the anoxic aging samples with initial As(V),
a significant fraction (15% of the total Fe) of maghemite (a magnetic
Fe oxide spinel with formula γ-Fe2O3)
was identified, which was coupled to As(V) reduction [As(III) was
∼30% of the total sorbed As], suggesting electron transfer
between magnetite and particle-bound As(V). In the oxic aging experiments,
the initial particle crystallized, with a large fraction of Fe(III)
(oxyhydr)oxides (i.e., maghemite and lepidocrocite, γ-FeOOH)
in the final products. Despite increased crystallinity suggested by
Fe XAS analysis, sorbed As was not released from the particles in
any experiment (aqueous As never exceeded 1 μg/L). This remarkable
stability of As coprecipitated with magnetite was revealed by As K-edge
XAS to be largely due to the formation of distinct multinuclear As
uptake modes [i.e., As(V) incorporation; hexanuclear 3C
As(III) complexes]. These results demonstrate the unique potential
of magnetite for long-term As sequestration.