3D alluvial aquifer reconstruction in polluted areas by means of GPR (Sabiñánigo, N Spain)
Assumptions of simple geometries for alluvial deposits (related to main rivers) can preclude determination of complexities that are revealed as fundamental controls in underground flow. Although subhorizontal contacts between alluvial and substratum materials are expected, previous sedimentary or er...
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| Veröffentlicht in: | Environmental earth sciences 2014-12, Vol.72 (11), p.4291-4302 |
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| creator | Pueyo Anchuela, Ó Ipas-Lloréns, J. F Gil Garbí, H Casas-Sainz, A. M Pocoví Juan, A Garijo, M. L Fernández-Martos, J. G Fernández-Cascán, J |
| description | Assumptions of simple geometries for alluvial deposits (related to main rivers) can preclude determination of complexities that are revealed as fundamental controls in underground flow. Although subhorizontal contacts between alluvial and substratum materials are expected, previous sedimentary or erosional processes can result in irregular geometries, only accessible through detailed analysis. The studied case presents the 3D reconstruction of a Quaternary terrace in the proximities of Sabiñánigo (Southern Pyrenees, Northeastern Spain), lying on homogeneous Eocene marls. The studied area is located in an industrialized area supporting strongly pollutant chemical industry (chlorinated pesticides) for the past 50 years. The objective of the study was to constrain the groundwater pathway along the area to subsequently analyze leakage of chemicals to the water table. In order to reveal preferred flow paths, a detailed characterization of the internal structure of the alluvial deposits (0.5–13 m thick) and their relations with the Tertiary substratum was carried out by means of ground penetrating radar (GPR, 50 and 100 MHz antennas). The obtained models permit identifying several topographic highs in the alluvial/substratum contact, determining preferred pathways in water flow, favoring particular conditions associated with low levels of the water table. The presented results support the interest of application of GPR surveys in order to characterize the groundwater pathways in expected homogeneous areas and their importance in order to establish the contaminant surveillance network. |
| doi_str_mv | 10.1007/s12665-014-3326-2 |
| format | Article |
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F ; Gil Garbí, H ; Casas-Sainz, A. M ; Pocoví Juan, A ; Garijo, M. L ; Fernández-Martos, J. G ; Fernández-Cascán, J</creator><creatorcontrib>Pueyo Anchuela, Ó ; Ipas-Lloréns, J. F ; Gil Garbí, H ; Casas-Sainz, A. M ; Pocoví Juan, A ; Garijo, M. L ; Fernández-Martos, J. G ; Fernández-Cascán, J</creatorcontrib><description>Assumptions of simple geometries for alluvial deposits (related to main rivers) can preclude determination of complexities that are revealed as fundamental controls in underground flow. Although subhorizontal contacts between alluvial and substratum materials are expected, previous sedimentary or erosional processes can result in irregular geometries, only accessible through detailed analysis. The studied case presents the 3D reconstruction of a Quaternary terrace in the proximities of Sabiñánigo (Southern Pyrenees, Northeastern Spain), lying on homogeneous Eocene marls. The studied area is located in an industrialized area supporting strongly pollutant chemical industry (chlorinated pesticides) for the past 50 years. The objective of the study was to constrain the groundwater pathway along the area to subsequently analyze leakage of chemicals to the water table. In order to reveal preferred flow paths, a detailed characterization of the internal structure of the alluvial deposits (0.5–13 m thick) and their relations with the Tertiary substratum was carried out by means of ground penetrating radar (GPR, 50 and 100 MHz antennas). The obtained models permit identifying several topographic highs in the alluvial/substratum contact, determining preferred pathways in water flow, favoring particular conditions associated with low levels of the water table. The presented results support the interest of application of GPR surveys in order to characterize the groundwater pathways in expected homogeneous areas and their importance in order to establish the contaminant surveillance network.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-014-3326-2</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Alluvial aquifers ; Alluvial deposits ; alluvium ; Aquifers ; Biogeosciences ; Chemical industry ; chlorination ; Contaminants ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Environmental Science and Engineering ; Eocene ; Exact sciences and technology ; Geochemistry ; Geology ; Ground penetrating radar ; Groundwater ; Groundwater pollution ; Hydrogeology ; Hydrology ; Hydrology. Hydrogeology ; Hydrology/Water Resources ; Industrial areas ; industrialization ; monitoring ; Original Article ; Pathways ; Pesticides ; Pollution, environment geology ; Quaternary ; Reconstruction ; rivers ; surveys ; Terraces ; Terrestrial Pollution ; Three dimensional ; Water flow ; Water table ; Water tables</subject><ispartof>Environmental earth sciences, 2014-12, Vol.72 (11), p.4291-4302</ispartof><rights>Springer-Verlag Berlin Heidelberg 2014</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a529t-9cab7c7a55b0a62068b4171a6e6bef4c88174cf3c5355459021f51f935fea8813</citedby><cites>FETCH-LOGICAL-a529t-9cab7c7a55b0a62068b4171a6e6bef4c88174cf3c5355459021f51f935fea8813</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12665-014-3326-2$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-014-3326-2$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28915400$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Pueyo Anchuela, Ó</creatorcontrib><creatorcontrib>Ipas-Lloréns, J. F</creatorcontrib><creatorcontrib>Gil Garbí, H</creatorcontrib><creatorcontrib>Casas-Sainz, A. M</creatorcontrib><creatorcontrib>Pocoví Juan, A</creatorcontrib><creatorcontrib>Garijo, M. L</creatorcontrib><creatorcontrib>Fernández-Martos, J. G</creatorcontrib><creatorcontrib>Fernández-Cascán, J</creatorcontrib><title>3D alluvial aquifer reconstruction in polluted areas by means of GPR (Sabiñánigo, N Spain)</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>Assumptions of simple geometries for alluvial deposits (related to main rivers) can preclude determination of complexities that are revealed as fundamental controls in underground flow. Although subhorizontal contacts between alluvial and substratum materials are expected, previous sedimentary or erosional processes can result in irregular geometries, only accessible through detailed analysis. The studied case presents the 3D reconstruction of a Quaternary terrace in the proximities of Sabiñánigo (Southern Pyrenees, Northeastern Spain), lying on homogeneous Eocene marls. The studied area is located in an industrialized area supporting strongly pollutant chemical industry (chlorinated pesticides) for the past 50 years. The objective of the study was to constrain the groundwater pathway along the area to subsequently analyze leakage of chemicals to the water table. In order to reveal preferred flow paths, a detailed characterization of the internal structure of the alluvial deposits (0.5–13 m thick) and their relations with the Tertiary substratum was carried out by means of ground penetrating radar (GPR, 50 and 100 MHz antennas). The obtained models permit identifying several topographic highs in the alluvial/substratum contact, determining preferred pathways in water flow, favoring particular conditions associated with low levels of the water table. The presented results support the interest of application of GPR surveys in order to characterize the groundwater pathways in expected homogeneous areas and their importance in order to establish the contaminant surveillance network.</description><subject>Alluvial aquifers</subject><subject>Alluvial deposits</subject><subject>alluvium</subject><subject>Aquifers</subject><subject>Biogeosciences</subject><subject>Chemical industry</subject><subject>chlorination</subject><subject>Contaminants</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Environmental Science and Engineering</subject><subject>Eocene</subject><subject>Exact sciences and technology</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Ground penetrating radar</subject><subject>Groundwater</subject><subject>Groundwater pollution</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Hydrology/Water Resources</subject><subject>Industrial areas</subject><subject>industrialization</subject><subject>monitoring</subject><subject>Original Article</subject><subject>Pathways</subject><subject>Pesticides</subject><subject>Pollution, environment geology</subject><subject>Quaternary</subject><subject>Reconstruction</subject><subject>rivers</subject><subject>surveys</subject><subject>Terraces</subject><subject>Terrestrial Pollution</subject><subject>Three dimensional</subject><subject>Water flow</subject><subject>Water table</subject><subject>Water tables</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqNkd1qFDEYhgexYFl7AR4ZEKGCY_PlbyaHUrUKpRXXngnhm5gsKbPJNpkRejlegtfQGzPLlCIeiDlJ4HvelyRP0zwD-gYo7U4KMKVkS0G0nDPVskfNIfRKtYpp_fjh3NMnzVEp17QuDlxTddh84-8IjuP8I-BI8GYO3mWSnU2xTHm2U0iRhEh2qTKT-04wOyxkuCVbh7GQ5MnZ5y_keI1DuPt19zOGTXpNLsh6hyG-etoceByLO7rfV83Vh_dfTz-255dnn07fnrcomZ5abXHobIdSDhQVo6ofBHSAyqnBeWH7HjphPbeSSymkpgy8BK-59A7rkK-a46V3l9PN7MpktqFYN44YXZqLAaXqN_Va8P9ABVPAerFvffEXep3mHOtDKsUYo50GVSlYKJtTKdl5s8thi_nWADV7O2axY6ods7djWM28vG_GYnH0GaMN5SHIeg1SVEerhi1cqaO4cfmPG_yj_PkS8pgMbnItvlozCrJaB8EZ578BBHOl7A</recordid><startdate>20141201</startdate><enddate>20141201</enddate><creator>Pueyo Anchuela, Ó</creator><creator>Ipas-Lloréns, J. 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F ; Gil Garbí, H ; Casas-Sainz, A. M ; Pocoví Juan, A ; Garijo, M. L ; Fernández-Martos, J. G ; Fernández-Cascán, J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a529t-9cab7c7a55b0a62068b4171a6e6bef4c88174cf3c5355459021f51f935fea8813</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Alluvial aquifers</topic><topic>Alluvial deposits</topic><topic>alluvium</topic><topic>Aquifers</topic><topic>Biogeosciences</topic><topic>Chemical industry</topic><topic>chlorination</topic><topic>Contaminants</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Environmental Science and Engineering</topic><topic>Eocene</topic><topic>Exact sciences and technology</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Ground penetrating radar</topic><topic>Groundwater</topic><topic>Groundwater pollution</topic><topic>Hydrogeology</topic><topic>Hydrology</topic><topic>Hydrology. Hydrogeology</topic><topic>Hydrology/Water Resources</topic><topic>Industrial areas</topic><topic>industrialization</topic><topic>monitoring</topic><topic>Original Article</topic><topic>Pathways</topic><topic>Pesticides</topic><topic>Pollution, environment geology</topic><topic>Quaternary</topic><topic>Reconstruction</topic><topic>rivers</topic><topic>surveys</topic><topic>Terraces</topic><topic>Terrestrial Pollution</topic><topic>Three dimensional</topic><topic>Water flow</topic><topic>Water table</topic><topic>Water tables</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pueyo Anchuela, Ó</creatorcontrib><creatorcontrib>Ipas-Lloréns, J. F</creatorcontrib><creatorcontrib>Gil Garbí, H</creatorcontrib><creatorcontrib>Casas-Sainz, A. M</creatorcontrib><creatorcontrib>Pocoví Juan, A</creatorcontrib><creatorcontrib>Garijo, M. L</creatorcontrib><creatorcontrib>Fernández-Martos, J. 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F</au><au>Gil Garbí, H</au><au>Casas-Sainz, A. M</au><au>Pocoví Juan, A</au><au>Garijo, M. L</au><au>Fernández-Martos, J. G</au><au>Fernández-Cascán, J</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>3D alluvial aquifer reconstruction in polluted areas by means of GPR (Sabiñánigo, N Spain)</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2014-12-01</date><risdate>2014</risdate><volume>72</volume><issue>11</issue><spage>4291</spage><epage>4302</epage><pages>4291-4302</pages><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>Assumptions of simple geometries for alluvial deposits (related to main rivers) can preclude determination of complexities that are revealed as fundamental controls in underground flow. Although subhorizontal contacts between alluvial and substratum materials are expected, previous sedimentary or erosional processes can result in irregular geometries, only accessible through detailed analysis. The studied case presents the 3D reconstruction of a Quaternary terrace in the proximities of Sabiñánigo (Southern Pyrenees, Northeastern Spain), lying on homogeneous Eocene marls. The studied area is located in an industrialized area supporting strongly pollutant chemical industry (chlorinated pesticides) for the past 50 years. The objective of the study was to constrain the groundwater pathway along the area to subsequently analyze leakage of chemicals to the water table. In order to reveal preferred flow paths, a detailed characterization of the internal structure of the alluvial deposits (0.5–13 m thick) and their relations with the Tertiary substratum was carried out by means of ground penetrating radar (GPR, 50 and 100 MHz antennas). The obtained models permit identifying several topographic highs in the alluvial/substratum contact, determining preferred pathways in water flow, favoring particular conditions associated with low levels of the water table. The presented results support the interest of application of GPR surveys in order to characterize the groundwater pathways in expected homogeneous areas and their importance in order to establish the contaminant surveillance network.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s12665-014-3326-2</doi><tpages>12</tpages></addata></record> |
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| subjects | Alluvial aquifers Alluvial deposits alluvium Aquifers Biogeosciences Chemical industry chlorination Contaminants Earth and Environmental Science Earth Sciences Earth, ocean, space Engineering and environment geology. Geothermics Environmental Science and Engineering Eocene Exact sciences and technology Geochemistry Geology Ground penetrating radar Groundwater Groundwater pollution Hydrogeology Hydrology Hydrology. Hydrogeology Hydrology/Water Resources Industrial areas industrialization monitoring Original Article Pathways Pesticides Pollution, environment geology Quaternary Reconstruction rivers surveys Terraces Terrestrial Pollution Three dimensional Water flow Water table Water tables |
| title | 3D alluvial aquifer reconstruction in polluted areas by means of GPR (Sabiñánigo, N Spain) |
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