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Modeling a Large-Scale Historic Aquifer Test: Insight into the Hydrogeology of a Regional Fault Zone
Daniel R Hadley, Daniel B Abrams1, George S Roadcap1
1University of Illinois, Illinois State Water Survey, 2204 Griffith Drive, Champaign, IL, 61820.
The Sandwich Fault Zone acts as a significant barrier to groundwater flow, reducing hydraulic conductivity by tenfold. This fault zone
Area of Science:
- Hydrogeology
- Geology
- Environmental Science
Background:
- Fault zones significantly impact groundwater flow by creating permeability heterogeneity.
- The Sandwich Fault Zone's deep hydrogeology is poorly understood due to burial and fault orientation.
- Understanding fault behavior is crucial for managing regional water resources.
Purpose of the Study:
- To investigate the hydrogeology of the Sandwich Fault Zone.
- To determine the role of the fault zone as a barrier or conduit for groundwater flow.
- To assess the impact of the fault zone on regional groundwater availability.
Main Methods:
- Utilized a large-scale historic aquifer test conducted in 1942.
- Employed a transient MODFLOW-USG model with the CLN package for simulations.
- Calibrated the model to drawdown data from production and observation wells, testing various fault conceptualizations.
Main Results:
- The Sandwich Fault Zone acts as a low-permeability barrier, inhibiting lateral groundwater movement.
- Horizontal hydraulic conductivity within the fault core is at least an order of magnitude lower than in surrounding sandstone.
- Simulations indicate significant regional drawdown north of the fault zone, sensitive to fault parameters.
Conclusions:
- The Sandwich Fault Zone functions as a substantial groundwater flow barrier.
- The fault's low permeability has critical implications for future groundwater availability in the region.
- Effective groundwater management strategies must account for the hydrogeologic influence of this fault zone.
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