Arsenic (As)-bearing water treatment residuals (WTRs)
from household
sand filters are usually disposed on top of floodplain soils and may
act as a secondary As contamination source. We hypothesized that open
disposal of these filter-sands to soils will facilitate As release
under reducing conditions. To quantify the mobilization risk of As,
we incubated the filter-sand, the soil, and a mixture of the filter-sand
and soil in anoxic artificial rainwater and followed the dynamics
of reactive Fe and As in aqueous, solid, and colloidal phases. Microbially
mediated Fe(III)/As(V) reduction led to the mobilization of 0.1–4%
of the total As into solution with the highest As released from the
mixture microcosms equaling 210 μg/L. Due to the filter-sand
and soil interaction, Mössbauer and X-ray absorption spectroscopies
indicated that up to 10% Fe(III) and 32% As(V) were reduced in the
mixture microcosm. Additionally, the mass concentrations of colloidal
Fe and As analyzed by single-particle ICP-MS decreased by 77–100%
compared to the onset of reducing conditions with the highest decrease
observed in the mixture setups (>95%). Overall, our study suggests
that (i) soil provides bioavailable components (e.g., organic matter)
that promote As mobilization via microbial reduction of As-bearing
Fe(III) (oxyhydr)oxides and (ii) As mobilization as colloids is important
especially right after the onset of reducing conditions but its importance
decreases over time.