Researchers Focus on How Heavy Rain Can Move Uranium Through a Wetland
By Tyjaha Steele

Map of Tims Branch study site, including sediment U activity, the location of the two most contaminated hot spots and the stream autosampler. (Photo courtesy of Daniel Kaplan)
Heavy rain can change the way water moves through a wetland, sending more water through streams and carrying sediment along with it. For researchers studying contaminated wetlands, those changes can also affect how contaminants move through the environment.
Researchers from the University of Georgia’s Savannah River Ecology Laboratory (SREL), Savannah River National Laboratory and Argonne National Laboratory studied how rainfall affects uranium movement in the Tims Branch wetland at the Savannah River Site in South Carolina. The study was led by Daniel I. Kaplan, senior research scientist in Environmental Molecular Sciences at SREL and associate director of the University of Georgia Artificial Intelligence Research Institute (UGARI), along with Karah Greene, Wei Xing, Arelis Rivera-Giboyeaux, Kenneth Kemner and Peng Lin.
The Tims Branch wetland has held onto most of the uranium released into the area more than 55 years ago. Because much of that uranium is attached to sediment, researchers wanted to understand what happens when heavy rain causes those sediments to move.
“Most of the uranium has remained stored in the wetland, but heavy rainfall gives us a window into how some of that uranium can become mobile again,” Kaplan said. “By understanding that relationship between rainfall, sediment and uranium, we can better understand how contaminants may move through wetlands over time.”
To study this, researchers collected stream water samples every hour during six rainfall events between February and September 2024. The storms brought between 0.69 and 9.87 centimeters of rain and caused streamflow to increase by as much as 11 times its normal level. Researchers measured the amount of uranium in both the water and the suspended sediment carried by the stream.
The results showed that most of the uranium being moved during storms was associated with suspended sediment rather than being dissolved in the water. In some samples, as much as 94% of the uranium was associated with suspended solids. Researchers also found a strong relationship between the amount of sediment in the water and the amount of uranium being transported.
This means that changes in how much sediment a stream carries can provide a useful way to understand how much uranium is being moved during rainfall events. Turbidity, which is a measure of how cloudy the water is, was also closely related to uranium concentrations.
Using rainfall and uranium measurements from the study, researchers estimated that a relatively small portion of the uranium stored in the wetland was remobilized during rainy days in 2024. The three days with the most rainfall accounted for about 29% of the uranium estimated to have moved that year.
The researchers also used historical rainfall data to estimate how much uranium may have been remobilized since the original release. Their calculations suggest that only a small percentage, about 2.2%, of the uranium originally released had been remobilized over the 55 years following the release.
While most of the uranium remains in the wetland, the findings show that rainfall can play a role in moving some of it through the system. The researchers note that increases in total rainfall and extreme rainfall events could increase the rate at which contaminants are transported from wetlands.
The study also builds on previous research showing that wetland sediments can strongly bind uranium, helping keep it in place for decades. During heavy rain, however, some of those sediments can become suspended in the water and move downstream.
Understanding how rainfall affects that movement gives researchers another way to examine how contaminants behave in wetlands over time, particularly as rainfall patterns change.
The study, “Uranium remobilization from a riparian wetland: Implications on long-term stewardship and extreme rain events,” was published in Applied Geochemistry and was authored by Daniel I. Kaplan, Karah M. Greene, Wei Xing, Arelis M. Rivera-Giboyeaux, Kenneth M. Kemner and Peng Lin.
















