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Estimating hydraulic parameters when poroelastic effects are significant.

Steven J Berg1, Paul A Hsieh, Walter A Illman

  • 1Waterloo Institute for Groundwater Research, Department of Earth & Environmental Sciences, University of Waterloo, Waterloo, Canada N2L 3G1. sjberg@uwaterloo.ca

Ground Water
|January 6, 2011
PubMed
Summary

Deformation-induced head changes from poroelastic effects in aquifers can be managed. Traditional groundwater theory methods can estimate hydraulic parameters if pumping is long enough for these effects to dissipate.

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Area of Science:

  • Hydrogeology
  • Geotechnical Engineering
  • Poroelasticity

Background:

  • Deformation-induced head changes due to poroelastic effects are observed in multilayered aquifer-aquitard systems during pumping tests.
  • These effects arise from aquifer deformation during water release, influencing pore pressure and drawdown curves beyond traditional groundwater theory predictions.
  • Current practical guidelines for interpreting pumping test data influenced by poroelastic effects are lacking.

Purpose of the Study:

  • To investigate the impact of poroelastic effects on hydraulic parameter estimation during aquifer pumping tests.
  • To assess the applicability of traditional groundwater theory methods in the presence of significant deformation-induced head changes.

Main Methods:

  • Generation of synthetic pumping test data for three distinct aquifer-aquitard settings using a poroelasticity model.
  • Analysis of synthetic data using traditional type curves and parameter estimation techniques that do not account for poroelastic effects.

Main Results:

  • Poroelastic effects can cause significant deformation-induced head changes, deviating from traditional groundwater theory predictions.
  • Reasonable estimates of hydraulic parameters are achievable using traditional methods, even with substantial poroelastic influences.
  • Sufficiently long pumping durations allow deformation-induced effects to dissipate, improving parameter estimation accuracy.

Conclusions:

  • Traditional groundwater theory methods can be applied to estimate hydraulic parameters in systems influenced by poroelastic effects, provided pumping is extended.
  • The findings offer practical insights for interpreting pumping test data in complex hydrogeological settings.
  • Further research may refine guidelines for managing poroelastic effects in aquifer analysis.