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NUTRIENT RELEASE RATES FROM THE SEDIMENTS OF SAGINAW BAY, LAKE HURON
Citation:
Ullman, W. AND R. Aller. NUTRIENT RELEASE RATES FROM THE SEDIMENTS OF SAGINAW BAY, LAKE HURON. U.S. Environmental Protection Agency, Washington, D.C., EPA/600/J-89/428 (NTIS PB90264839), 1989.
Description:
Direct measurements of net production rates and pore water profiles of solutes in the fine-grained sediments of Saginaw Bay, imply corresponding steady-state fluxes to the overlying water of 1.1-1.3 (I), 450-1010 (NH4+), 1250-2650 (Si(OH)4), 3000-3400 (Ca2+), 440-1330 (Mg2+), 1.5-728 (Fe2+), and 179-281 (Mn2+), umoles/m2/day and 11.0-11.8 (alkalinity) meq/m2/day at 17.5 degrees C. ilica production rates in sediments apparently follow first order kinetics with a rate coefficient of 0.09/day and a steady-state silica concentration of 1.2 mM at 23.5 degrees C. he remaining solutes follow kinetics approximately independent of solute concentration over the range of concentrations observed. easured solute production rates are consistent with observed solute profiles only if lateral diffusion gradients are maintained in the sediments by the burrowing and irrigation activity of benthic organisms such as Chironmous, the domninant borrower in Saginaw Bay. ssuming that solute fluxes from Saginaw Bay are representative of all of the post-glacial sediments of Lake Huron, the iodine flux from sediments is comparable to the total fluvial input of iodine. he extrapolated silica fluxes from Lake Huron sediments balance the estimated biogenic silica flux to the sediments.
