27 From Data to Decision: Integrating Geophysics, Data Systems, and Modeling for Aquifer Characterization in Data-Sparse Regions (Posters)
Advances in data acquisition, management, and analytics are transforming water-resources research in semi-arid, data-sparse regions. This session highlights the integration of geophysics, data systems, and modeling, including AEM, legacy data digitization, and cloud platforms. Contributions demonstrate how advances in data collection, management, analysis, and modeling approaches improve the characterization of fresh and brackish groundwater to support management, recharge, and long-term planning.
Tuesday, 19 May 2026
8:00 AM - 5:30 PM
Alvarado D/E
Integrated Hydro-geophysical Characterization of an Anthropogenic Perched Aquifer at the Waste Isolation Pilot Plant
Paper number: 27-2
Program: Technical Sessions
Time: 8:00 AM – 8:00 AM
Authors
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Dale RuckerhydroGEOPHYSICS, Inc., Tucson, Arizona
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Anderson WardWaste Isolation Pilot Plant (WIPP), Carlsbad, New Mexico
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Zachary LepchitzWaste Isolation Pilot Plant (WIPP), Carlsbad, New Mexico
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Kenneth CarrollNew Mexico State University, Las Cruces, NM
Abstract
An anthropogenic perched aquifer has formed due to the interaction of natural stratigraphy and discharges from unlined impoundments at the Waste Isolation Pilot Plant (WIPP) site in New Mexico. Characterizing its spatial extent and potential connectivity to the regional groundwater system requires a higher data density than is currently available using existing wells. This study develops an integrated hydro geophysical approach, combining electrical resistivity tomography, induced polarization, borehole resistivity, lithology, and water-quality data to characterize the perched aquifer. Archie’s law parameters were estimated from perched formation petrophysical properties. This approach characterizes the aquifer geometry, lateral extent, and hydrodynamic behavior, constraining the perched horizon that is localized between the lower-permeability Dewey Lake Redbeds and the overlying Santa Rosa Sandstones. Resistivity and chargeability data confirmed that the low-resistivity features are due to perched groundwater saturation and salinity (i.e., not elevated clay content), and a change in cementation forms the impervious horizon of the aquifer. Resistivity contours, which infer water-saturated conditions, closely matched piezometric equipotential elevations, exhibiting a strong correlation (R² = 0.89), and confirmed the geophysical characterization of the perched water table. This data fusion framework provides a systematic approach to delineate the geometry and extent of anthropogenic perched aquifers.
Geological Society of America Abstracts with Programs. Vol. 58, No. 4
doi: 10.1130/abs/2026RM-410501
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