Tidally driven pore water exchange within offshore intertidal sandbanks: Part II numerical simulations
Field measurements presented by [Gibbes, B., Robinson, C., Li, L., Lockington, D.A., Carey, H., 2008. Tidally driven pore water exchange within offshore intertidal sandbanks: Part I Field measurements. Estuarine, Coastal and Shelf Science 79, pp. 121–132.] revealed a tidally driven pore water flow s...
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description | Field measurements presented by [Gibbes, B., Robinson, C., Li, L., Lockington, D.A., Carey, H., 2008. Tidally driven pore water exchange within offshore intertidal sandbanks: Part I Field measurements. Estuarine, Coastal and Shelf Science 79, pp. 121–132.] revealed a tidally driven pore water flow system within an offshore intertidal sandbank in Moreton Bay, Australia. The field data suggested that this flow system might be capable of delivering nutrients, and in particular bio-available iron, across the sediment–water interface. Bio-available iron has been implicated as a key nutrient in the growth of the toxic marine cyanobacteria
Lyngbya majuscula and therefore this pore water exchange process is of interest at sites where
L. majuscula blooms have been observed. In this study two-dimensional numerical simulations were used in conjunction with hydraulic data from field measurements to further investigate the tidally induced pore water flow patterns. Simulation results generally showed good agreement with the field data and revealed a more complex residual pore water flow system in the sandbank than shown by the field data. The flow system, strongly influenced by the geometry of the sandbank, was characterized by two circulation cells which resulted in pore water discharge at the bank edge and also to a permanently ponded area within the sandbank interior. Simulated discharge volumes in these two zones were in the order of 0.813
m
3 and 0.143
m
3 per meter width (along shore) of sandbank per tidal cycle at the bank edge and sandbank interior respectively. Transit times of pore water circulating through these cells were found to range from ≈ 17 days to
>
60 years with an average time of 780 days. The results suggest that the tidally driven flow systems might provide a mechanism for transport of bio-available iron across the sediment–water interface. This flow could constitute a previously unrecognized source of bio-available iron for
L. majuscula blooms in the Bay. |
doi_str_mv | 10.1016/j.ecss.2008.08.021 |
format | Article |
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Lyngbya majuscula and therefore this pore water exchange process is of interest at sites where
L. majuscula blooms have been observed. In this study two-dimensional numerical simulations were used in conjunction with hydraulic data from field measurements to further investigate the tidally induced pore water flow patterns. Simulation results generally showed good agreement with the field data and revealed a more complex residual pore water flow system in the sandbank than shown by the field data. The flow system, strongly influenced by the geometry of the sandbank, was characterized by two circulation cells which resulted in pore water discharge at the bank edge and also to a permanently ponded area within the sandbank interior. Simulated discharge volumes in these two zones were in the order of 0.813
m
3 and 0.143
m
3 per meter width (along shore) of sandbank per tidal cycle at the bank edge and sandbank interior respectively. Transit times of pore water circulating through these cells were found to range from ≈ 17 days to
>
60 years with an average time of 780 days. The results suggest that the tidally driven flow systems might provide a mechanism for transport of bio-available iron across the sediment–water interface. This flow could constitute a previously unrecognized source of bio-available iron for
L. majuscula blooms in the Bay.</description><identifier>ISSN: 0272-7714</identifier><identifier>EISSN: 1096-0015</identifier><identifier>DOI: 10.1016/j.ecss.2008.08.021</identifier><identifier>CODEN: ECSSD3</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>Animal and plant ecology ; Animal, plant and microbial ecology ; Biological and medical sciences ; Brackish ; Brackish water ecosystems ; Cyanobacteria ; Cyanophyta ; Freshwater ; Fundamental and applied biological sciences. Psychology ; intertidal system ; Lyngbya majuscula ; Moreton Bay ; numerical model ; offshore sandbank ; pore water exchange ; Sea water ecosystems ; Synecology</subject><ispartof>Estuarine, coastal and shelf science, 2008-12, Vol.80 (4), p.472-482</ispartof><rights>2008 Elsevier Ltd</rights><rights>2009 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a384t-78f44b32e87d77ab71ad64f692ae9e20b7349df92ab5ac4b1f96a46de9ccb2403</citedby><cites>FETCH-LOGICAL-a384t-78f44b32e87d77ab71ad64f692ae9e20b7349df92ab5ac4b1f96a46de9ccb2403</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.ecss.2008.08.021$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,777,781,3537,27905,27906,45976</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=20947091$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Gibbes, B.</creatorcontrib><creatorcontrib>Robinson, C.</creatorcontrib><creatorcontrib>Li, L.</creatorcontrib><creatorcontrib>Lockington, D.</creatorcontrib><creatorcontrib>Li, H.</creatorcontrib><title>Tidally driven pore water exchange within offshore intertidal sandbanks: Part II numerical simulations</title><title>Estuarine, coastal and shelf science</title><description>Field measurements presented by [Gibbes, B., Robinson, C., Li, L., Lockington, D.A., Carey, H., 2008. Tidally driven pore water exchange within offshore intertidal sandbanks: Part I Field measurements. Estuarine, Coastal and Shelf Science 79, pp. 121–132.] revealed a tidally driven pore water flow system within an offshore intertidal sandbank in Moreton Bay, Australia. The field data suggested that this flow system might be capable of delivering nutrients, and in particular bio-available iron, across the sediment–water interface. Bio-available iron has been implicated as a key nutrient in the growth of the toxic marine cyanobacteria
Lyngbya majuscula and therefore this pore water exchange process is of interest at sites where
L. majuscula blooms have been observed. In this study two-dimensional numerical simulations were used in conjunction with hydraulic data from field measurements to further investigate the tidally induced pore water flow patterns. Simulation results generally showed good agreement with the field data and revealed a more complex residual pore water flow system in the sandbank than shown by the field data. The flow system, strongly influenced by the geometry of the sandbank, was characterized by two circulation cells which resulted in pore water discharge at the bank edge and also to a permanently ponded area within the sandbank interior. Simulated discharge volumes in these two zones were in the order of 0.813
m
3 and 0.143
m
3 per meter width (along shore) of sandbank per tidal cycle at the bank edge and sandbank interior respectively. Transit times of pore water circulating through these cells were found to range from ≈ 17 days to
>
60 years with an average time of 780 days. The results suggest that the tidally driven flow systems might provide a mechanism for transport of bio-available iron across the sediment–water interface. This flow could constitute a previously unrecognized source of bio-available iron for
L. majuscula blooms in the Bay.</description><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Biological and medical sciences</subject><subject>Brackish</subject><subject>Brackish water ecosystems</subject><subject>Cyanobacteria</subject><subject>Cyanophyta</subject><subject>Freshwater</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>intertidal system</subject><subject>Lyngbya majuscula</subject><subject>Moreton Bay</subject><subject>numerical model</subject><subject>offshore sandbank</subject><subject>pore water exchange</subject><subject>Sea water ecosystems</subject><subject>Synecology</subject><issn>0272-7714</issn><issn>1096-0015</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNp9UEtr3DAQFqWFbtP8gZ50SW_eSrLWskMuJSTtQqA5JGcxlkZZbbzyRuPN49_XYkOPhYFh5nsM8zH2TYqlFLL5sV2iI1oqIdplKSU_sIUUXVMJIVcf2UIooypjpP7MvhBt561c1WrBwl30MAxv3Of4jInvx4z8BSbMHF_dBtLDPMZpExMfQ6BNgWOa4anoOEHyPaRHOue3kCe-XvN02GGOroBxdxhgimOir-xTgIHw9L2fsPvrq7vL39XNn1_ry583FdStnirTBq37WmFrvDHQGwm-0aHpFGCHSvSm1p0P89ivwOlehq4B3XjsnOuVFvUJ-3703efx6YA02V0kh8MACccDWSVkW9dNIaoj0eWRKGOw-xx3kN-sFLZEare2RGpLpLaUkrPo7N0daH4wZEgu0j-lEp02oiu8iyMP51efI2ZLLmJy6GNGN1k_xv-d-QtEho7I</recordid><startdate>20081210</startdate><enddate>20081210</enddate><creator>Gibbes, B.</creator><creator>Robinson, C.</creator><creator>Li, L.</creator><creator>Lockington, D.</creator><creator>Li, H.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7SN</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>M7N</scope></search><sort><creationdate>20081210</creationdate><title>Tidally driven pore water exchange within offshore intertidal sandbanks: Part II numerical simulations</title><author>Gibbes, B. ; Robinson, C. ; Li, L. ; Lockington, D. ; Li, H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a384t-78f44b32e87d77ab71ad64f692ae9e20b7349df92ab5ac4b1f96a46de9ccb2403</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Biological and medical sciences</topic><topic>Brackish</topic><topic>Brackish water ecosystems</topic><topic>Cyanobacteria</topic><topic>Cyanophyta</topic><topic>Freshwater</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>intertidal system</topic><topic>Lyngbya majuscula</topic><topic>Moreton Bay</topic><topic>numerical model</topic><topic>offshore sandbank</topic><topic>pore water exchange</topic><topic>Sea water ecosystems</topic><topic>Synecology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gibbes, B.</creatorcontrib><creatorcontrib>Robinson, C.</creatorcontrib><creatorcontrib>Li, L.</creatorcontrib><creatorcontrib>Lockington, D.</creatorcontrib><creatorcontrib>Li, H.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Ecology Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic 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) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Estuarine, coastal and shelf science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gibbes, B.</au><au>Robinson, C.</au><au>Li, L.</au><au>Lockington, D.</au><au>Li, H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Tidally driven pore water exchange within offshore intertidal sandbanks: Part II numerical simulations</atitle><jtitle>Estuarine, coastal and shelf science</jtitle><date>2008-12-10</date><risdate>2008</risdate><volume>80</volume><issue>4</issue><spage>472</spage><epage>482</epage><pages>472-482</pages><issn>0272-7714</issn><eissn>1096-0015</eissn><coden>ECSSD3</coden><abstract>Field measurements presented by [Gibbes, B., Robinson, C., Li, L., Lockington, D.A., Carey, H., 2008. Tidally driven pore water exchange within offshore intertidal sandbanks: Part I Field measurements. Estuarine, Coastal and Shelf Science 79, pp. 121–132.] revealed a tidally driven pore water flow system within an offshore intertidal sandbank in Moreton Bay, Australia. The field data suggested that this flow system might be capable of delivering nutrients, and in particular bio-available iron, across the sediment–water interface. Bio-available iron has been implicated as a key nutrient in the growth of the toxic marine cyanobacteria
Lyngbya majuscula and therefore this pore water exchange process is of interest at sites where
L. majuscula blooms have been observed. In this study two-dimensional numerical simulations were used in conjunction with hydraulic data from field measurements to further investigate the tidally induced pore water flow patterns. Simulation results generally showed good agreement with the field data and revealed a more complex residual pore water flow system in the sandbank than shown by the field data. The flow system, strongly influenced by the geometry of the sandbank, was characterized by two circulation cells which resulted in pore water discharge at the bank edge and also to a permanently ponded area within the sandbank interior. Simulated discharge volumes in these two zones were in the order of 0.813
m
3 and 0.143
m
3 per meter width (along shore) of sandbank per tidal cycle at the bank edge and sandbank interior respectively. Transit times of pore water circulating through these cells were found to range from ≈ 17 days to
>
60 years with an average time of 780 days. The results suggest that the tidally driven flow systems might provide a mechanism for transport of bio-available iron across the sediment–water interface. This flow could constitute a previously unrecognized source of bio-available iron for
L. majuscula blooms in the Bay.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.ecss.2008.08.021</doi><tpages>11</tpages></addata></record> |
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subjects | Animal and plant ecology Animal, plant and microbial ecology Biological and medical sciences Brackish Brackish water ecosystems Cyanobacteria Cyanophyta Freshwater Fundamental and applied biological sciences. Psychology intertidal system Lyngbya majuscula Moreton Bay numerical model offshore sandbank pore water exchange Sea water ecosystems Synecology |
title | Tidally driven pore water exchange within offshore intertidal sandbanks: Part II numerical simulations |
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