The results of near-surface Direct Current surveys have been interpreted with the analysis of 1-D and 2-D resistivity datasets and sediments' and pore fluids electrical properties, in order to obtain 3-D models of sand-gravel and silt-clay alluvial bodies of an area of the Po plain south of Milan (Italy). The definition of the hierarchical scales of the sedimentary bodies permits the integration between hydro-and electro-stratigraphy and to gain a valid representation of heterogeneities of alluvial aquifers necessary for a reliable conceptualization of the groundwater reservoirs needed for the mathematical modelling of flow and transport processes.
Near-surface electrostratigraphy as a tool to detect the connectivity of the sedimentary bodies / M. Mele, R. Bersezio, M. Giudici - In: Proceedings of the 18th international conference on computational methods in water resources / [a cura di] J. Carrera, X. SanchezVila, D. FernandezGarcia, D. Bolster. - Barcelona : Int center numerical methods engineering, 2010. - ISBN 9788496736931. - pp. 683-690 (( Intervento presentato al 18. convegno International Conference on Computational Methods in Water Resources tenutosi a Barcelona nel 2010.
Near-surface electrostratigraphy as a tool to detect the connectivity of the sedimentary bodies
M. MelePrimo
;R. Bersezio;M. Giudici
2010
Abstract
The results of near-surface Direct Current surveys have been interpreted with the analysis of 1-D and 2-D resistivity datasets and sediments' and pore fluids electrical properties, in order to obtain 3-D models of sand-gravel and silt-clay alluvial bodies of an area of the Po plain south of Milan (Italy). The definition of the hierarchical scales of the sedimentary bodies permits the integration between hydro-and electro-stratigraphy and to gain a valid representation of heterogeneities of alluvial aquifers necessary for a reliable conceptualization of the groundwater reservoirs needed for the mathematical modelling of flow and transport processes.File | Dimensione | Formato | |
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