Scheda di dettaglio – i prodotti della ricerca
| Dato | Valore |
|---|---|
| Title | INTEGRATION OF ELECTRIC RESISTIVITY PROFILE AN INFILTROMETER MEASUREMENTS TO CALIBRATE A NUMERICAL MODEL OF VERTICAL FLOW IN FRACTURED AND KARSTIC LIMESTONE |
| Abstract | Karstic and fractured aquifers are among the most important drinking water resources. At the same time, they are particularly vulnerable to contamination. A detailed scientific knowledge of the behavior of these aquifers is essential for the development of sustainable groundwater management concepts. Due to their special characteristics of extreme anisotropy and heterogeneity, research aimed at a better understanding of flow, solute transport, and biological processes in these hydrogeologic systems is an important scientific challenge. This study integrates a geophysical technique with an infiltrometer test to better calibrate a mathematical model that quantifies the vertical flow in karstic and fractured limestone overlying the deep aquifer of Alta Murgia (Southern Italy). Knowledge of the rate of unsaturated zone percolation is needed to investigate the vertical migration of pollutants and the vulnerability of the aquifer. Sludge waste deposits in the study area have caused soil-subsoil contamination with toxics. The experimental test consisted of infiltrometer flow measurements, more commonly utilized for unconsolidated granular porous media, during which subsoil electric resistivity data were collected. A ring infiltrometer 2 m in diameter and 0.3 m high was sealed to the ground with gypsum. This large diameter yielded infiltration data representative of the anisotropic and heterogeneous rock, which could not be sampled adequately with a small ring. The subsurface resistivity was measured using a Wenner-Schlumberger electrode array. Vertical movement of water in a fracture plane under unsaturated conditions has been investigated by means of a numerical model. The finite difference method was used to solve the flow equations. An internal iteration method was used at every time step to evaluate the nodal value of the pressure head, in agreement with the mass-balance equation and the characteristic functional relationships of the coefficients. |
| Source | 2007 AMERICAN GEOPHYSICAL UNION (AGU) FALL MEETING, AMERICAN GEOPHYSICAL UNION, SAN FRANCISCO - CALIFORNIA - U |
| Year | 2007 |
| Type | Contributo in atti di convegno |
| Authors | CAPUTO M.C., DE CARLO L., MASCIOPINTO C., NIMMO J.R. |
| Text | 89595 2007 INTEGRATION OF ELECTRIC RESISTIVITY PROFILE AN INFILTROMETER MEASUREMENTS TO CALIBRATE A NUMERICAL MODEL OF VERTICAL FLOW IN FRACTURED AND KARSTIC LIMESTONE CAPUTO M.C., DE CARLO L., MASCIOPINTO C., NIMMO J.R. Water Research Institute IRSA CNR, Bari, Italy US Geological Survey, Menlo Park, CA, USA Karstic and fractured aquifers are among the most important drinking water resources. At the same time, they are particularly vulnerable to contamination. A detailed scientific knowledge of the behavior of these aquifers is essential for the development of sustainable groundwater management concepts. Due to their special characteristics of extreme anisotropy and heterogeneity, research aimed at a better understanding of flow, solute transport, and biological processes in these hydrogeologic systems is an important scientific challenge. This study integrates a geophysical technique with an infiltrometer test to better calibrate a mathematical model that quantifies the vertical flow in karstic and fractured limestone overlying the deep aquifer of Alta Murgia Southern Italy . Knowledge of the rate of unsaturated zone percolation is needed to investigate the vertical migration of pollutants and the vulnerability of the aquifer. Sludge waste deposits in the study area have caused soil subsoil contamination with toxics. The experimental test consisted of infiltrometer flow measurements, more commonly utilized for unconsolidated granular porous media, during which subsoil electric resistivity data were collected. A ring infiltrometer 2 m in diameter and 0.3 m high was sealed to the ground with gypsum. This large diameter yielded infiltration data representative of the anisotropic and heterogeneous rock, which could not be sampled adequately with a small ring. The subsurface resistivity was measured using a Wenner Schlumberger electrode array. Vertical movement of water in a fracture plane under unsaturated conditions has been investigated by means of a numerical model. The finite difference method was used to solve the flow equations. An internal iteration method was used at every time step to evaluate the nodal value of the pressure head, in agreement with the mass balance equation and the characteristic functional relationships of the coefficients. 2007 AMERICAN GEOPHYSICAL UNION AGU FALL MEETING, AMERICAN GEOPHYSICAL UNION SAN FRANCISCO CALIFORNIA U Internazionale Contributo Contributo in atti di convegno mariaclementina.caputo CAPUTO MARIA CLEMENTINA costantino.masciopinto MASCIOPINTO COSTANTINO TA.P05.006.007 Fattori critici dei rischi di siccita e strategie dintervento |