Abstract
Weathered/fractured hardrock aquifers are complex, heterogeneous groundwater systems with overall low storage. This work develops a methodology using computer coding to estimate hardrock aquifers' storage properties applying Archie (AR) and Waxman & Smits (WS) petrophysical models, and further assess their sensitivity and uncertainty. The data consists in both surface and borehole hydrogeophysical measurements in a micaschist aquifer in Ireland. In this case study, WS appears as most suitable because it allows to account for the significant clay content present in the subsurface as a result bedrock weathering. This property is not accounted for in AR, which therefore largely overestimates the pore space. An important finding is the high sensitivity of both models to the cementation factor. WS models are in addition highly sensitive to the clay properties, namely the cation exchange capacity. Uncertainty analyses determined the higher uncertainty in the deep, high resistivity, massive bedrock, with WS being the most affected. Availability and accuracy of spatial data on the cementation factor and clay properties are key to achieve realistic storage models with high confidence.
Original language | English |
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Title of host publication | 25th European Meeting of Environmental and Engineering Geophysics |
Subtitle of host publication | Near Surface Geoscience Conference and Exhibition 2019 |
Edition | NSG 2019 |
DOIs | |
Publication status | Published - 2019 |
Event | 25th European Meeting of Environmental and Engineering Geophysics, Held at Near Surface Geoscience Conference and Exhibition 2019, NSG 2019 - The Hague, Netherlands Duration: 8 Sept 2019 → 12 Sept 2019 |
Conference
Conference | 25th European Meeting of Environmental and Engineering Geophysics, Held at Near Surface Geoscience Conference and Exhibition 2019, NSG 2019 |
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Country/Territory | Netherlands |
City | The Hague |
Period | 8/09/19 → 12/09/19 |
Bibliographical note
Funding Information:We thank the Geological Survey of Ireland and the National Council of Science and Technology and Secretariat of Energy of Mexico (CONACYT-SENER) for the funding to conduct this research.