The release of dissolved nutrients and metals from coastal sediments due to resuspension

• Published in: Marine chemistry Vol. 121; no. 1; pp. 224 - 235
• Main Authors: Kalnejais, Linda H., Martin, William R., Bothner, Michael H.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 20.08.2010; Elsevier
• Subjects: Boston Harbor; Chambers; Coastal; Copper; Dissolution; Earth sciences; Earth, ocean, space; Erosion; Erosion chamber; Exact sciences and technology; External geophysics; Geochemistry; Harbors; Marine; Mineralogy; Nutrients; Physical and chemical properties of sea water; Physics of the oceans; Sediment resuspension; Sediments; Shear stress; Silicates; Silver; Trace metals; Water geochemistry; United States; Massachusetts; Boston Harbor; Silver; Sediment resuspension; Trace metals; Erosion chamber; mixing; fine-grained materials; metals; resuspension; North America; manganese; nutrients; coupling; currents; shear stress; solution; copper; particles; suspension; waves; models; solutes; harbors; concentration; hydrodynamics; lead; grains; depth; erosion; iron; silver
• ISSN: 0304-4203; 1872-7581
• DOI: 10.1016/j.marchem.2010.05.002

Coastal sediments in many regions are impacted by high levels of contaminants. Due to a combination of shallow water depths, waves, and currents, these sediments are subject to regular episodes of sediment resuspension. However, the influence of such disturbances on sediment chemistry and the release of solutes is poorly understood. The aim of this study is to quantify the release of dissolved metals (iron, manganese, silver, copper, and lead) and nutrients due to resuspension in Boston Harbor, Massachusetts, USA. Using a laboratory-based erosion chamber, a range of typical shear stresses was applied to fine-grained Harbor sediments and the solute concentration at each shear stress was measured. At low shear stress, below the erosion threshold, limited solutes were released. Beyond the erosion threshold, a release of all solutes, except lead, was observed and the concentrations increased with shear stress. The release was greater than could be accounted for by conservative mixing of porewaters into the overlying water, suggesting that sediment resuspension enhances the release of nutrients and metals to the dissolved phase. To address the long-term fate of resuspended particles, samples from the erosion chamber were maintained in suspension for 90 h. Over this time, 5–7% of the particulate copper and silver was released to the dissolved phase, while manganese was removed from solution. Thus resuspension releases solutes both during erosion events and over a longer timescale due to reactions of suspended particles in the water column. The magnitude of the annual solute release during erosion events was estimated by coupling the erosion chamber results with a record of bottom shear stresses simulated by a hydrodynamic model. The release of dissolved copper, lead, and phosphate due to resuspension is between 2% and 10% of the total (dissolved plus particulate phase) known inputs to Boston Harbor. Sediment resuspension is responsible for transferring a significant quantity of solid phase metals to the more bioavailable and mobile dissolved phase. The relative importance of sediment resuspension as a source of dissolved metals to Boston Harbor is expected to increase as continuing pollutant control decreases the inputs from other sources.