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The ITRAX core scanner, a useful tool to distinguish anthropic vs. climatic influences in lagoon of Aveiro (N Portugal)
This paper aims to distinguish anthropic and climatic influences in sediments from the lagoon of Aveiro (Portugal). This study is based on a core (240-cm long) collected in Murtosa Channel. Optical and X-radiographic images and high-resolution elemental profiles were acquired with ITRAX micro-X-ray...
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Published in: | Journal of coastal research 2013-01, Vol.1 (65), p.70-70 |
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creator | Martins, Virginia A Dias, Joao A Bernardes, Cristina Rubio, Belen Bernabeu, Ana Rey, Daniel Soares, Antonio M Sobrinho, Frederico Laut, Lazaro M Frontalini, Fabrizio Terroso, Denise Miranda, Paulo Fernandez-Fernandez, Sandra Rodrigues, Maria Antonieta Figueira, Rubens Sousa, Silvia Amaral, Paula Mahiques, Michel Rocha, Fernando |
description | This paper aims to distinguish anthropic and climatic influences in sediments from the lagoon of Aveiro (Portugal). This study is based on a core (240-cm long) collected in Murtosa Channel. Optical and X-radiographic images and high-resolution elemental profiles were acquired with ITRAX micro-X-ray fluorescence (XRF) core scanner. Samples collected at each approximately 3 cm along the core were analysed for grain size and total organic carbon. Furthermore, the fine fraction of selected layers was subjected to geochemical analysis by ICP-MS, after total acid digestion of the sediments, and mineralogical analysis, by XRD techniques. Sediments along the core are composed by fine and medium sand, with several mud layers. The progressive increase of Si/Al, Cl/Al, Rb/Al, K/Al and Br/Al and reduced Al concentrations, from the base to the top of this core, are interpreted as being related to higher marine influence and greater differences in tidal currents with longer exposition to air of the sediments with the consequent formation of brines favouring minerals precipitation in the area (e.g. anhydrite). |
doi_str_mv | 10.2112/SI65-013 |
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This study is based on a core (240-cm long) collected in Murtosa Channel. Optical and X-radiographic images and high-resolution elemental profiles were acquired with ITRAX micro-X-ray fluorescence (XRF) core scanner. Samples collected at each approximately 3 cm along the core were analysed for grain size and total organic carbon. Furthermore, the fine fraction of selected layers was subjected to geochemical analysis by ICP-MS, after total acid digestion of the sediments, and mineralogical analysis, by XRD techniques. Sediments along the core are composed by fine and medium sand, with several mud layers. The progressive increase of Si/Al, Cl/Al, Rb/Al, K/Al and Br/Al and reduced Al concentrations, from the base to the top of this core, are interpreted as being related to higher marine influence and greater differences in tidal currents with longer exposition to air of the sediments with the consequent formation of brines favouring minerals precipitation in the area (e.g. anhydrite).</description><identifier>ISSN: 0749-0208</identifier><identifier>EISSN: 1551-5036</identifier><identifier>DOI: 10.2112/SI65-013</identifier><language>eng</language><publisher>Fort Lauderdale: Allen Press Inc</publisher><subject>Aluminum ; Carbon ; Channels ; Coastal ; Coasts ; Environmental impact ; Lagoons ; Organic carbon ; Sand ; Sediments ; Tidal currents ; X-ray fluorescence</subject><ispartof>Journal of coastal research, 2013-01, Vol.1 (65), p.70-70</ispartof><rights>Copyright Allen Press Publishing Services 2013</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Martins, Virginia A</creatorcontrib><creatorcontrib>Dias, Joao A</creatorcontrib><creatorcontrib>Bernardes, Cristina</creatorcontrib><creatorcontrib>Rubio, Belen</creatorcontrib><creatorcontrib>Bernabeu, Ana</creatorcontrib><creatorcontrib>Rey, Daniel</creatorcontrib><creatorcontrib>Soares, Antonio M</creatorcontrib><creatorcontrib>Sobrinho, Frederico</creatorcontrib><creatorcontrib>Laut, Lazaro M</creatorcontrib><creatorcontrib>Frontalini, Fabrizio</creatorcontrib><creatorcontrib>Terroso, Denise</creatorcontrib><creatorcontrib>Miranda, Paulo</creatorcontrib><creatorcontrib>Fernandez-Fernandez, Sandra</creatorcontrib><creatorcontrib>Rodrigues, Maria Antonieta</creatorcontrib><creatorcontrib>Figueira, Rubens</creatorcontrib><creatorcontrib>Sousa, Silvia</creatorcontrib><creatorcontrib>Amaral, Paula</creatorcontrib><creatorcontrib>Mahiques, Michel</creatorcontrib><creatorcontrib>Rocha, Fernando</creatorcontrib><title>The ITRAX core scanner, a useful tool to distinguish anthropic vs. climatic influences in lagoon of Aveiro (N Portugal)</title><title>Journal of coastal research</title><description>This paper aims to distinguish anthropic and climatic influences in sediments from the lagoon of Aveiro (Portugal). This study is based on a core (240-cm long) collected in Murtosa Channel. Optical and X-radiographic images and high-resolution elemental profiles were acquired with ITRAX micro-X-ray fluorescence (XRF) core scanner. Samples collected at each approximately 3 cm along the core were analysed for grain size and total organic carbon. Furthermore, the fine fraction of selected layers was subjected to geochemical analysis by ICP-MS, after total acid digestion of the sediments, and mineralogical analysis, by XRD techniques. Sediments along the core are composed by fine and medium sand, with several mud layers. The progressive increase of Si/Al, Cl/Al, Rb/Al, K/Al and Br/Al and reduced Al concentrations, from the base to the top of this core, are interpreted as being related to higher marine influence and greater differences in tidal currents with longer exposition to air of the sediments with the consequent formation of brines favouring minerals precipitation in the area (e.g. anhydrite).</description><subject>Aluminum</subject><subject>Carbon</subject><subject>Channels</subject><subject>Coastal</subject><subject>Coasts</subject><subject>Environmental impact</subject><subject>Lagoons</subject><subject>Organic carbon</subject><subject>Sand</subject><subject>Sediments</subject><subject>Tidal currents</subject><subject>X-ray 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ITRAX core scanner, a useful tool to distinguish anthropic vs. climatic influences in lagoon of Aveiro (N Portugal)</title><author>Martins, Virginia A ; Dias, Joao A ; Bernardes, Cristina ; Rubio, Belen ; Bernabeu, Ana ; Rey, Daniel ; Soares, Antonio M ; Sobrinho, Frederico ; Laut, Lazaro M ; Frontalini, Fabrizio ; Terroso, Denise ; Miranda, Paulo ; Fernandez-Fernandez, Sandra ; Rodrigues, Maria Antonieta ; Figueira, Rubens ; Sousa, Silvia ; Amaral, Paula ; Mahiques, Michel ; Rocha, Fernando</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p164t-aedbaefa4c2a51414c063dc40d2b5559de63b15afbb27afb44ea1713273de9e53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Aluminum</topic><topic>Carbon</topic><topic>Channels</topic><topic>Coastal</topic><topic>Coasts</topic><topic>Environmental impact</topic><topic>Lagoons</topic><topic>Organic 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This study is based on a core (240-cm long) collected in Murtosa Channel. Optical and X-radiographic images and high-resolution elemental profiles were acquired with ITRAX micro-X-ray fluorescence (XRF) core scanner. Samples collected at each approximately 3 cm along the core were analysed for grain size and total organic carbon. Furthermore, the fine fraction of selected layers was subjected to geochemical analysis by ICP-MS, after total acid digestion of the sediments, and mineralogical analysis, by XRD techniques. Sediments along the core are composed by fine and medium sand, with several mud layers. The progressive increase of Si/Al, Cl/Al, Rb/Al, K/Al and Br/Al and reduced Al concentrations, from the base to the top of this core, are interpreted as being related to higher marine influence and greater differences in tidal currents with longer exposition to air of the sediments with the consequent formation of brines favouring minerals precipitation in the area (e.g. anhydrite).</abstract><cop>Fort Lauderdale</cop><pub>Allen Press Inc</pub><doi>10.2112/SI65-013</doi><tpages>1</tpages></addata></record> |
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subjects | Aluminum Carbon Channels Coastal Coasts Environmental impact Lagoons Organic carbon Sand Sediments Tidal currents X-ray fluorescence |
title | The ITRAX core scanner, a useful tool to distinguish anthropic vs. climatic influences in lagoon of Aveiro (N Portugal) |
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