Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain)
Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescenc...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Mudarra, M. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2014 |
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| Übergeordnetes Werk: |
Enthalten in: Hydrogeology journal - Springer Berlin Heidelberg, 1995, 22(2014), 5 vom: 28. März, Seite 1027-1039 |
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| Übergeordnetes Werk: |
volume:22 ; year:2014 ; number:5 ; day:28 ; month:03 ; pages:1027-1039 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10040-014-1117-1 |
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OLC2040024409 |
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| 520 | |a Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). | ||
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10.1007/s10040-014-1117-1 doi (DE-627)OLC2040024409 (DE-He213)s10040-014-1117-1-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Mudarra, M. verfasserin aut Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) 2014 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). Carbonate aquifer Tracers Natural responses Infiltration processes Spain Andreo, B. aut Marín, A. I. aut Vadillo, I. aut Barberá, J. A. aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 22(2014), 5 vom: 28. März, Seite 1027-1039 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:22 year:2014 number:5 day:28 month:03 pages:1027-1039 https://doi.org/10.1007/s10040-014-1117-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 22 2014 5 28 03 1027-1039 |
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10.1007/s10040-014-1117-1 doi (DE-627)OLC2040024409 (DE-He213)s10040-014-1117-1-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Mudarra, M. verfasserin aut Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) 2014 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). Carbonate aquifer Tracers Natural responses Infiltration processes Spain Andreo, B. aut Marín, A. I. aut Vadillo, I. aut Barberá, J. A. aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 22(2014), 5 vom: 28. März, Seite 1027-1039 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:22 year:2014 number:5 day:28 month:03 pages:1027-1039 https://doi.org/10.1007/s10040-014-1117-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 22 2014 5 28 03 1027-1039 |
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10.1007/s10040-014-1117-1 doi (DE-627)OLC2040024409 (DE-He213)s10040-014-1117-1-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Mudarra, M. verfasserin aut Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) 2014 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). Carbonate aquifer Tracers Natural responses Infiltration processes Spain Andreo, B. aut Marín, A. I. aut Vadillo, I. aut Barberá, J. A. aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 22(2014), 5 vom: 28. März, Seite 1027-1039 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:22 year:2014 number:5 day:28 month:03 pages:1027-1039 https://doi.org/10.1007/s10040-014-1117-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 22 2014 5 28 03 1027-1039 |
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10.1007/s10040-014-1117-1 doi (DE-627)OLC2040024409 (DE-He213)s10040-014-1117-1-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Mudarra, M. verfasserin aut Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) 2014 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). Carbonate aquifer Tracers Natural responses Infiltration processes Spain Andreo, B. aut Marín, A. I. aut Vadillo, I. aut Barberá, J. A. aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 22(2014), 5 vom: 28. März, Seite 1027-1039 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:22 year:2014 number:5 day:28 month:03 pages:1027-1039 https://doi.org/10.1007/s10040-014-1117-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 22 2014 5 28 03 1027-1039 |
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Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) |
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Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) |
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Mudarra, M. |
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Mudarra, M. Andreo, B. Marín, A. I. Vadillo, I. Barberá, J. A. |
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combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the villanueva del rosario system (andalusia, southern spain) |
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Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) |
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Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). © Springer-Verlag Berlin Heidelberg 2014 |
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Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). © Springer-Verlag Berlin Heidelberg 2014 |
| abstract_unstemmed |
Abstract Analysis of natural responses of karst springs provides information on the behavior of the aquifers they drain. Detailed monitoring and qualitative and quantitative analyses of natural responses, and environmental—total organic carbon (TOC), $ NO_{3} $−, $ Cl^{−} $ and intrinsic fluorescence—and artificial (fluorescent dye) tracers, in the water drained by Villanueva del Rosario spring (southern Spain), suggest the existence of a conduit flow system with rapid flows and very short transit times of water through the aquifer. This is in agreement with uranine and eosin breakthrough curves and with simple numerical models done using these data. However, due to the low capacity for natural regulation, not all the recharge effects are simultaneously transmitted to the spring water; given a single input, the system modulates and transfers hydrodynamic variations faster than variations of chemical composition and of water temperature. Additionally, time lags between maximum concentrations of natural and artificial tracers show that the global system response (including diffuse infiltration) is faster and more sensitive than that produced from infiltration concentrated at a single point on the surface (sinkholes). © Springer-Verlag Berlin Heidelberg 2014 |
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Combined use of natural and artificial tracers to determine the hydrogeological functioning of a karst aquifer: the Villanueva del Rosario system (Andalusia, southern Spain) |
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