Wetlands are dynamic ecosystems that can immobilize contaminants for extended periods but can also release them when hydrological and/or biogeochemical conditions change. Although this behavior is well recognized, the field-scale processes controlling the retention and release of certain contaminants such as iodine-129 (129I) remain poorly understood, particularly in a contaminated wetland at the U.S. Department of Energy's Savannah River Site. In this study, we hypothesized that seasonal variations in groundwater flux regulate 129I behavior by altering the biogeochemistry of the wetland seeps and underlying sediments. To test this hypothesis, we combined soil and water sampling, microbial analysis, iodine speciation, and autonomous sensor monitoring. Our results show that 129I is preferentially retained in the organic-rich surface soil, with concentrations peaking at 0.22 Bq g−1 within the upper 0.15 m followed by a decrease with depth. Pronounced seasonal fluctuations in 129I concentrations were observed in surface water, increasing from 0.9–2 Bq L−1 in winter to 3–8 Bq L−1 in summer, while groundwater concentrations remained consistently lower (0.2–0.6 Bq L−1) and exhibited minimal seasonal variability. These variations correspond to seasonal changes in groundwater flux towards the seeps: higher flux during winter flushes the seeps causing 129I concentrations in surface water to be close to groundwater concentrations, while reduced flux during summer promotes stagnant and anoxic conditions that facilitate the release of bound 129I from the organic-rich soil into surface water. Iodine speciation analysis indicates that 78 to 99 % of total iodine in surface water existed as organoiodine, suggesting organic matter degradation drives 129I remobilization. These observations were integrated into a field-scale conceptual site model, linking hydrological and biogeochemical processes to the retention and release of 129I occurring in the wetlands.
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