The Relation Between Pore Water Chemistry and Benthic Fluxes of Nutrients and Manganese in Narragansett Bay, Rhode Island
Benthic fluxes of dissolved nutrients and manganese from biologically disturbed, relatively unpolluted sediment in Narragansett Bay, Rhode Island, have been measured. Analyses of the vertical gradients of chemical species dissolved in pore waters and the uptake of22Nafrom the overlying water permits...
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Veröffentlicht in: | Limnology and oceanography 1980-01, Vol.25 (1), p.31-44 |
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creator | McCaffrey, Richard J. Myers, Allen C. Davey, Earl Morrison, George Bender, Michael Luedtke, Nile Cullen, Douglas Froelich, Philip Klinkhammer, Gary |
description | Benthic fluxes of dissolved nutrients and manganese from biologically disturbed, relatively unpolluted sediment in Narragansett Bay, Rhode Island, have been measured. Analyses of the vertical gradients of chemical species dissolved in pore waters and the uptake of22Nafrom the overlying water permits evaluation of the contribution of biological advection and molecular diffusion to the transport of dissolved materials across the sediment-water interface. The activity of bottom-dwelling organisms appears to be about as important as molecular diffusion in most cases. The sum of the independently estimated contributions by both mechanisms is in good agreement with integrated benthic fluxes measured in situ. Sulfate and oxygen oxidize comparable amounts of organic matter in these sediments. |
doi_str_mv | 10.4319/lo.1980.25.1.0031 |
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Sulfate and oxygen oxidize comparable amounts of organic matter in these sediments.</description><subject>Advection</subject><subject>Ammonia</subject><subject>Diffusion coefficient</subject><subject>Manganese</subject><subject>Marine</subject><subject>Metabolites</subject><subject>Pumping</subject><subject>Sea water</subject><subject>Sediment transport</subject><subject>Sediments</subject><subject>Sulfates</subject><issn>0024-3590</issn><issn>1939-5590</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1980</creationdate><recordtype>article</recordtype><recordid>eNqFkMlOwzAQhi0EEmV5ACQOPnIgwRMvcQ4coGKTSkEIxNFy0wkNCjHYriBvj0sRV06z_d9o5ifkAFguOFQnncuh0iwvZA45Yxw2yAgqXmVSVmyTjBgrRMZTvk12QnhljFVSyhEZHhdIH7CzsXU9Pcf4idjTe-eRPtuIno4X-NaG6Adq-3kS9HHR1vSyW35hoK6h02X0beqGn_mt7V9sjwFp29Op9d6mMmCM9NwOx_Rh4eZIb0KXtHtkq7FdwP3fuEueLi8ex9fZ5O7qZnw2yazQEjJdlRqk1s0crapVo0SNvKxnZa1mZamAIYdGl4jzkikmrJo1hVBalgK0FELyXXK03vvu3ccSQzTpnxq7dAO6ZTCgmVZSywKSFNbS2rsQPDbm3bdv1g8GmFnZbDpnVjabQhowK5sTc7pmPtsOh_8BM5nerTqFhF_-cM2_huj8H19oLhVX_BuX8ouc</recordid><startdate>19800101</startdate><enddate>19800101</enddate><creator>McCaffrey, Richard J.</creator><creator>Myers, Allen C.</creator><creator>Davey, Earl</creator><creator>Morrison, George</creator><creator>Bender, Michael</creator><creator>Luedtke, Nile</creator><creator>Cullen, Douglas</creator><creator>Froelich, Philip</creator><creator>Klinkhammer, Gary</creator><general>American Society of Limnology and Oceanography</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope></search><sort><creationdate>19800101</creationdate><title>The Relation Between Pore Water Chemistry and Benthic Fluxes of Nutrients and Manganese in Narragansett Bay, Rhode Island</title><author>McCaffrey, Richard J. ; Myers, Allen C. ; Davey, Earl ; Morrison, George ; Bender, Michael ; Luedtke, Nile ; Cullen, Douglas ; Froelich, Philip ; Klinkhammer, Gary</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4851-89781588fdea6c6f64ce37cb7c6b77610e31f87eed70604a6bf24685741854453</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1980</creationdate><topic>Advection</topic><topic>Ammonia</topic><topic>Diffusion coefficient</topic><topic>Manganese</topic><topic>Marine</topic><topic>Metabolites</topic><topic>Pumping</topic><topic>Sea water</topic><topic>Sediment transport</topic><topic>Sediments</topic><topic>Sulfates</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>McCaffrey, Richard J.</creatorcontrib><creatorcontrib>Myers, Allen C.</creatorcontrib><creatorcontrib>Davey, Earl</creatorcontrib><creatorcontrib>Morrison, George</creatorcontrib><creatorcontrib>Bender, Michael</creatorcontrib><creatorcontrib>Luedtke, Nile</creatorcontrib><creatorcontrib>Cullen, Douglas</creatorcontrib><creatorcontrib>Froelich, Philip</creatorcontrib><creatorcontrib>Klinkhammer, Gary</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Limnology and oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>McCaffrey, Richard J.</au><au>Myers, Allen C.</au><au>Davey, Earl</au><au>Morrison, George</au><au>Bender, Michael</au><au>Luedtke, Nile</au><au>Cullen, Douglas</au><au>Froelich, Philip</au><au>Klinkhammer, Gary</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Relation Between Pore Water Chemistry and Benthic Fluxes of Nutrients and Manganese in Narragansett Bay, Rhode Island</atitle><jtitle>Limnology and oceanography</jtitle><date>1980-01-01</date><risdate>1980</risdate><volume>25</volume><issue>1</issue><spage>31</spage><epage>44</epage><pages>31-44</pages><issn>0024-3590</issn><eissn>1939-5590</eissn><abstract>Benthic fluxes of dissolved nutrients and manganese from biologically disturbed, relatively unpolluted sediment in Narragansett Bay, Rhode Island, have been measured. Analyses of the vertical gradients of chemical species dissolved in pore waters and the uptake of22Nafrom the overlying water permits evaluation of the contribution of biological advection and molecular diffusion to the transport of dissolved materials across the sediment-water interface. The activity of bottom-dwelling organisms appears to be about as important as molecular diffusion in most cases. The sum of the independently estimated contributions by both mechanisms is in good agreement with integrated benthic fluxes measured in situ. Sulfate and oxygen oxidize comparable amounts of organic matter in these sediments.</abstract><pub>American Society of Limnology and Oceanography</pub><doi>10.4319/lo.1980.25.1.0031</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record> |
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issn | 0024-3590 1939-5590 |
language | eng |
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source | JSTOR Archive Collection A-Z Listing; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection |
subjects | Advection Ammonia Diffusion coefficient Manganese Marine Metabolites Pumping Sea water Sediment transport Sediments Sulfates |
title | The Relation Between Pore Water Chemistry and Benthic Fluxes of Nutrients and Manganese in Narragansett Bay, Rhode Island |
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