Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/3057
Title: Diffusive and kinetic fluxes of phosphorus from sediments in relation to phosphorus dynamics in Lake Pepin, Upper Mississippi River
Authors: Water Operations Technical Support Program (U.S.)
James, William F.
Barko, John W.
Eakin, Harry L.
Keywords: Equilibrium phosphate concentration
Lake Pepin
Minnesota
External phosphorus loading
Phosphorus
Internal phosphorus loading
Eutrophication
Upper Mississippi River
Water quality
Issue Date: Sep-1999
Publisher: Environmental Laboratory (U.S.)
Engineer Research and Development Center (U.S.)
Description: Miscellaneous Paper
Abstract: Over a 3-year period (1994-96), suspended seston and phosphorus (P) dynamics were examined in the Upper Mississippi River (UMR) and naturally impounded Lake Pepin, with special attention to external and internal P loading processes that may be contributing to deteriorating water quality conditions. The Minnesota River accounted for most of the annual and summer suspended seston (~81 percent) and total phosphorus (~44 percent) load, while the Metropolitan Wastewater Treatment Plant (Metro Plant) accounted for ~48 percent of annual soluble reactive phosphorus (SRP) loading to the UMR. External loading during the summer of suspended seston, total P, and SRP to Lake Pepin averaged ~30,000 m⁻² day⁻¹, and ~60 mg m⁻² day⁻¹, respectively. The lake retained a substantial portion of the summer suspended seston load and was also a sink for total P. While total P concentrations generally declined in Lake Pepin from headwaters to outflow, SRP exhibited a trend of increasing concentration from headwaters to outflow with net SRP export during the summer. These contrasting patterns in total P and SRP indicated the occurrence of internal P loading and/or transformations in the water column of P from particulate to soluble phases. Internal diffusive P flux from profundal sediments, estimated from laboratory incubation systems under different temperature and redox conditions, averaged ~7.5 mg m⁻² day⁻¹, during the summer under predominately oxic conditions over all years. Although this oxic rate was high relative to other eutrophic lakes, it accounted for <15 percent of both the external total P and SRP loads to Lake Pepin. It did, however, account for 30 to 56 percent of the net SRP export from the lake during the summer. Sediments in Lake Pepin also had a high equilibrium P concentration (EPC = 0.162 mg/L ± 0.018 S.E.) and native adsorbed P pool (NAP = 0.178 mg/g ± 0.058 S.E.) at equilibrium. During the summer, SRP concentrations of flows entering Lake Pepin were lower than the EPC because of dilution effects by the St. Croix River, located 10 miles upstream of the lake, indicating a strong potential for P desorption from suspended seston entering the lake. When converted to a rate of internal P loading, estimated P desorption from suspended seston was very high (range = 2.3 - 3.7 mg m⁻² day⁻¹) and equivalent to rates of P release from eutrophic sediments in aquatic systems under anoxic conditions. When incorporated into the overall P budget for Lake Pepin, P desorption from suspended seston accounted for 25 percent to nearly 40 percent of the measured internal P load (i.e., diffusive plus kinetic) to the lake and was, thus, an important internal flux that is not commonly included in P budgets of lakes.
URI: http://hdl.handle.net/11681/3057
Appears in Collections:Miscellaneous Paper

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