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DatoValore
TitleHydrogeophysical approach to measure hydraulic parameters on unsaturated rocks
AbstractIn the past decade, over-exploitation has led to a de- pletion of water resources, with impact both on quality and quantity. A sustainable groundwater management needs a detailed scientific knowledge of the behaviour of the un- saturated zone. Particularly, the evaluation of the flow- rate in the unsaturated zone is important to estimate the travel time of the infiltrated water in the subsurface and, hence, to assess the recharge rate and groundwater vul- nerability. A quarry of calcarenite near the town of Canosa, in South Italy, has been chosen to perform the field tests using an integrated hydrogeophysical approach, combin- ing infiltrometer measurements with electrical resistivity tomography (ERT). The infiltration data were collected using a metallic infiltrometer ring of 0.5 m in diameter, installed directly on the rock, filled with about 8 L of water. The test was conducted for many hours at falling head condition, and the water level within the ring was measured by means of a pressure transductor and a metric rod fixed to the ring. Simultaneously, electrical resistivity measurements were carried out using "time-lapse" technique, in order to monitor the dynamics of infiltration/redistribution of the water in the unsaturated zone. Hydrogeophysical data have been acquired for sev- eral hours to obtain a reliable hydrogeological model of the subsurface investigated. Field-saturated hydraulic conductivity has been de- termined for the calcarenite, and ERT surveys support these results.
SourceFresenius environmental bulletin 21, pp. 3007–3082
Keywordshydrogeophysicsinfiltrometer testERT
JournalFresenius environmental bulletin
EditorParlar Scientific Publications, Freising, Germania
Year2012
TypeArticolo in rivista
AuthorsCaputo M.C., De Carlo L., Masciale R.
Text191715 2012 hydrogeophysics infiltrometer test ERT Hydrogeophysical approach to measure hydraulic parameters on unsaturated rocks Caputo M.C., De Carlo L., Masciale R. In the past decade, over exploitation has led to a de pletion of water resources, with impact both on quality and quantity. A sustainable groundwater management needs a detailed scientific knowledge of the behaviour of the un saturated zone. Particularly, the evaluation of the flow rate in the unsaturated zone is important to estimate the travel time of the infiltrated water in the subsurface and, hence, to assess the recharge rate and groundwater vul nerability. A quarry of calcarenite near the town of Canosa, in South Italy, has been chosen to perform the field tests using an integrated hydrogeophysical approach, combin ing infiltrometer measurements with electrical resistivity tomography ERT . The infiltration data were collected using a metallic infiltrometer ring of 0.5 m in diameter, installed directly on the rock, filled with about 8 L of water. The test was conducted for many hours at falling head condition, and the water level within the ring was measured by means of a pressure transductor and a metric rod fixed to the ring. Simultaneously, electrical resistivity measurements were carried out using time lapse technique, in order to monitor the dynamics of infiltration/redistribution of the water in the unsaturated zone. Hydrogeophysical data have been acquired for sev eral hours to obtain a reliable hydrogeological model of the subsurface investigated. Field saturated hydraulic conductivity has been de termined for the calcarenite, and ERT surveys support these results. 21 Published version Hydrogeophysical approach to measure hydraulic parameters on unsaturated rocks F_2011_925_Original_Paper_pp3077_3082_hydrogeopysical_approach.pdf Articolo in rivista Parlar Scientific Publications 1018 4619 Fresenius environmental bulletin Fresenius environmental bulletin Fresenius environ. bull. Fresenius environmental bulletin. FEB Freising. Print Fresenius environmental bulletin Print mariaclementina.caputo CAPUTO MARIA CLEMENTINA rita.masciale MASCIALE RITA lorenzo.decarlo DE CARLO LORENZO TA.P04.005.006 Gestione a scala di bacino delle risorse idriche e sostenibilita dell uso irriguo in agricoltura