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Groundwater Storage in a Karst Vadose Zone Evidenced Using Gravimetric and Surface-to-borehole ERT Monitoring SystemsNormal access

Authors: A. Watlet, O. Kaufmann, O. Francis and M. Van Camp
Event name: Near Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics
Session: Hydrogeophysical Characterization of Shallow Aquifers
Publication date: 06 September 2015
DOI: 10.3997/2214-4609.201413708
Organisations: EAGE
Language: English
Info: Extended abstract, PDF ( 1.43Mb )
Price: € 20

Summary:
Hydrogeophysical tools allow characterizing the heterogeneity of karsts and evidencing groundwater storage in their subsurface. A permanent gravimetric monitoring highlights seasonal variations in gravity that can be related to vadose zone effects after the discrimination of the saturated zone signature with direct measurements. A surface ERT monitoring improved with daily borehole-to-surface measurements through the vadose zone allows identifying preferential flow paths. Groundwater storage variation is then monitored by time-lapse inversion of the ERT datasets.


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