Scheda di dettaglio – i prodotti della ricerca
| Dato | Valore |
|---|---|
| Title | Quantitative interpretation of time-lapse MALM measurements during a saline tracer injection in an alluvial aquifer |
| Abstract | This study presents the results of a saline tracer test conducted on an unconfined alluvial aquifer placed in the Alento River Valley (Campania region, South-Western Italy) and monitored by Mise-à-la-Masse measurements. The aim of this test is the investigation of groundwater flow field by a time-lapse analysis. The work first introduces the local hydrogeology of the investigated system and the experimental set-up. The results of the geophysical tracer test are then described and followed by the discussion of several simulations conducted on a 3D electrical model of the system. Finally, the comparison between real and simulated datasets is discussed in order to highlight advantages and limitations of Mise-à-la Masse technique when applied for hydrogeological purposes. |
| Source | Near Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics, Torino, 06-10/09/2015 |
| Keywords | Geophysics and hydrology |
| Year | 2015 |
| Type | Contributo in atti di convegno |
| Authors | Perri, M. T.; De Vita, P.; Cassiani, G.; Masciale, R.; Portoghese, I.; Chirico, G. B. |
| Text | 420859 2015 Scopus 2 s2.0 84958093689 Geophysics and hydrology Quantitative interpretation of time lapse MALM measurements during a saline tracer injection in an alluvial aquifer Perri, M. T.; De Vita, P.; Cassiani, G.; Masciale, R.; Portoghese, I.; Chirico, G. B. Istituto di Ricerca Sulle Acque, Bari; Universita degli Studi di Napoli Federico II; Universita degli Studi di Padova This study presents the results of a saline tracer test conducted on an unconfined alluvial aquifer placed in the Alento River Valley Campania region, South Western Italy and monitored by Mise a la Masse measurements. The aim of this test is the investigation of groundwater flow field by a time lapse analysis. The work first introduces the local hydrogeology of the investigated system and the experimental set up. The results of the geophysical tracer test are then described and followed by the discussion of several simulations conducted on a 3D electrical model of the system. Finally, the comparison between real and simulated datasets is discussed in order to highlight advantages and limitations of Mise a la Masse technique when applied for hydrogeological purposes. 9781510814127 Published version http //www.scopus.com/record/display.url eid=2 s2.0 84958093689 origin=inward Near Surface Geoscience 2015 21st European Meeting of Environmental and Engineering Geophysics Torino 06 10/09/2015 Internazionale Contributo Contributo in atti di convegno ivan.portoghese PORTOGHESE IVAN rita.masciale MASCIALE RITA |