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Temporal Trends of Dissolved Trace Metals in Jamaica Bay, NY: Importance of Wastewater Input and Submarine Groundwater Discharge in an Urban Estuary.
Beck, Aaron J. , Cochran, J. K. and Sañudo-Wilhelmy, S. A. (2009) Temporal Trends of Dissolved Trace Metals in Jamaica Bay, NY: Importance of Wastewater Input and Submarine Groundwater Discharge in an Urban Estuary. Estuaries and Coasts, 32 (3). pp. 535-550. DOI 10.1007/s12237-009-9140-5.
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Abstract
Jamaica Bay, NY, is a highly urbanized estuary within the boroughs of New York City conspicuously lacking published information on dissolved trace metal concentrations. The current study examines the distribution and cycling of trace metals in that embayment with data gathered during cruises in November 2004, April 2005, and June 2006. Most of the metal distributions (Fe, Zn, Co, Ag, Cu, Pb, Ni) in the water column are explained by the input of substantial volumes of treated wastewater effluent. However, several lines of evidence suggest that submarine groundwater discharge (SGD) is also an important source of dissolved Fe, Zn, Co, Ni, and isotopically distinct stable Pb ratios (206Pb, 207Pb, 208Pb) in the Bay. Conversely, the recirculated seawater component of SGD is an apparent sink for dissolved Mo. This study provides the first measurements of dissolved trace metals in the Jamaica Bay water column and subterranean estuary and provides evidence for trace metal input due to SGD.
Document Type: | Article |
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Keywords: | Trace metals . Submarine groundwater discharge . SGD .Wastewater . Jamaica Bay. New York |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | Springer |
Date Deposited: | 10 Oct 2017 13:21 |
Last Modified: | 09 Mar 2018 08:24 |
URI: | https://oceanrep.geomar.de/id/eprint/39822 |
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