The climate change has dramatically decreased the useful freshwater resources so raising the probability of severe droughts. Near-surface geophysics uses the investigational methods of geophysics leading to their massive use in all scientific sectors (geology, hydrogeology, engineering, archaeology, environmental problems). Moreover, the increasing challenge of quantifying extractable, economically viable, potable water supplies has led to the definition of a new subdiscipline of hydrology known as hydrogeophysics. Direct current (DC) electrical methods are probably the most widely used near surface geophysical techniques for environmental investigations. DC methods are increasingly used in different approaches to cover a larger field of applications. In hydrogeological applications, the electrical resistivity distribution can provide important information that allows to characterize the heterogeneity of the aquifers and soil, to reconstruct the geometry of the aquifers and/or waterproof, to study the relationships between freshwater and seawater, or from groundwater different salinity.

Direct Current Electrical Methods for Hydrogeological Purposes

Giampaolo V
2022

Abstract

The climate change has dramatically decreased the useful freshwater resources so raising the probability of severe droughts. Near-surface geophysics uses the investigational methods of geophysics leading to their massive use in all scientific sectors (geology, hydrogeology, engineering, archaeology, environmental problems). Moreover, the increasing challenge of quantifying extractable, economically viable, potable water supplies has led to the definition of a new subdiscipline of hydrology known as hydrogeophysics. Direct current (DC) electrical methods are probably the most widely used near surface geophysical techniques for environmental investigations. DC methods are increasingly used in different approaches to cover a larger field of applications. In hydrogeological applications, the electrical resistivity distribution can provide important information that allows to characterize the heterogeneity of the aquifers and soil, to reconstruct the geometry of the aquifers and/or waterproof, to study the relationships between freshwater and seawater, or from groundwater different salinity.
2022
Istituto di Metodologie per l'Analisi Ambientale - IMAA
978-3-031-08261-0
Conductivity
DC
Electrical resistivity
Hydrogeological
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/412527
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