Joint 72nd Annual Southeastern/ 58th Annual Northeastern Section Meeting - 2023

Paper No. 33-5
Presentation Time: 1:30 PM-5:30 PM

SEDIMENT RECENCY IN THE WESTERN LAKE ERIE BASIN


DUFF, Teaghan1, DEYRUP, Caroline1, PITERA, Anneka1, JOHNSON, Averey1, SCHMIDT, Amanda2, MATHIE, Devan3, WILLIAMSON, Tanja4, HOOD, J.5 and KARWAN, Diana6, (1)Geosciences, Oberlin College, Oberlin, OH 44074, (2)Geology, Oberlin College, Oberlin, OH 44074, (3)The Ohio State University, 202 Orton Hall, Columbus, OH 43210, (4)U. S. Geological Survey, 8505 Research Way, Middleton, WI 53562, (5)Ecology, Organismal, and Evolutionary Biology, The Ohio State University, Columbus, OH 43210, (6)Department of Forest Resources, University of Minnesota, 301G Green Hall, 1530 Cleveland Avenue North, St. Paul, MN 55108

Phosphorus (P) cycling in the Western Lake Erie Basin (WLEB) as a result of agricultural runoff has long been known to promote harmful algal blooms, yet there is a lack of data on sediment-bound phosphorus (sedP) recency and origin. Fallout radionuclides 7Be and excess 210Pb (210Pbex) can fill important knowledge gaps related to the emergence of sedP in WLEB tributaries.

We measured 7Be and 210Pbex in baseflow sediment samples from mainstem (Auglaize River and Maumee River) and headwater (Little Flatrock Creek and Black Creek) tributaries collected in 8-9/21, and 9/22. We also analyzed 7Be and 210Pbex in suspended sediment collected during 3 storm events in Black Creek 3/22, 5/22, and 7/22.

In our preliminary data, suspended sediment from the storm samples had higher concentrations of 7Be than bed sediments, which tended to have low 7Be activity and low but present 210Pb activity. March storm sediments had much higher 7Be values than those measured during other storms while July storm sediments had much lower 210Pb values.

7Be and 210Pbex concentrations in bed sediment suggest it has been in the river for relatively long periods of time. These sediments had low 7Be (T1/2 = 53 days), implying sediment was last exposed to direct rainfall hundreds of days ago. The presence, albeit with low activity, of 210Pbex suggests sediment was decades old, rather than centuries. Bed sediment from 9/2022 had higher 7Be values than sediment collected in 8-9/2021. This could be due to extremely low discharges in 2022 leading to wetted channel area contraction and thus direct dosing of channel bed sediment by infrequent rain events.

Storm sediment samples had the highest levels of 7Be, suggesting that sediment was recently exposed to rainfall. In samples where 7Be was present but 210Pbex was not, we hypothesize that sediment was sourced from deeply eroded horizontal surfaces, possibly the pasture and cropland sources identified in previous studies. Significantly more rain during the March storm was correlated with the highest 7Be levels.

Other parts of this project will determine sedP levels and sediment origin to provide a thorough understanding of P loading in the watershed. Given these data, this research will further differentiate P in the stream from upstream runoff from agricultural fields relative to re-mobilization of in-channel storage.