Uranium
(U) speciation was investigated in anoxically preserved
porewater samples of a natural mountain wetland in Gola di Lago, Ticino,
Switzerland. U porewater concentrations ranged from less than 1 μg/L
to tens of μg/L, challenging the available analytical approaches
for U speciation in natural samples. Asymmetrical flow field-flow
fractionation coupled with inductively coupled plasma mass spectrometry
allowed the characterization of colloid populations and the determination
of the size distribution of U species in the porewater. Most of the
U was associated with three fractions: <0.3 kDa, likely including
dissolved U and very small U colloids; a 1–3 kDa fraction containing
humic-like organic compounds, dispersed Fe, and, to a small extent,
Fe nanoparticles; and a third fraction (5–50 nm), containing
a higher amount of Fe and a lower amount of organic matter and U relative
to the 1–3 kDa fraction. The proportion of U associated with
the 1–3 kDa colloids varied spatially and seasonally. Using
anion exchange resins, we also found that a significant proportion
of U occurs in its reduced form, U(IV). Tetravalent U was interpreted
as occurring within the colloidal pool of U. This study suggests that
U(IV) can occur as small (1–3 kDa), organic-rich, and thus
potentially mobile colloidal species in naturally reducing wetland
environments.