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CEGR 4145 5145 Groundwater Resources Engineering

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Explain observed aquifer behavior. Predict response in future, under ... Aquifer deformation. GW Flow and Solute Transport. Models based on ... Aquifer ... – PowerPoint PPT presentation

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Title: CEGR 4145 5145 Groundwater Resources Engineering


1
CEGR 4145 / 5145 Groundwater Resources
Engineering
  • Groundwater Modeling (Ch. 13)
  • Physical Scale Models
  • Analog Models
  • Mathematical Models
  • Excel-based modeling
  • Visual MODFLOW

2
Reasons for Modeling
  • Explain observed aquifer behavior
  • Predict response in future, under various
    stresses
  • Primary GW models
  • Groundwater flow
  • Solute flow
  • Heat flow
  • Aquifer deformation

3
GW Flow and Solute Transport
  • Models based on equations to describe
  • Porous Media
  • Fractured Media
  • Saturated Zone
  • Unsaturated Zone

4
Data Requirements
  • GW Flow
  • Physical dimensions, strata thicknesses, boundary
    conditions, formation constants (T, K and S),
    recharge, head distribution, etc.
  • Solute Transport
  • In addition to GW flow data, effective porosity,
    aquifer dispersivity, fluid density variability,
    contaminant source and strength, soil reactivity
    (distribution coefficients), etc.

5
Model Calibration and Verification
  • For GW Flow models, a primary goal is often to
    develop the potentiometric surface for a given
    area
  • This model is calibrated against known values
    of head (from an observation well). Aquifer
    properties are adjusted.
  • Matching the model-predicted values of head to
    those previously produced (or in the future) in
    response to a transient event provides
    verification

6
Mathematical Model Types
  • Finite Difference (Fig. 13.1, 13.2 text)
  • Real geometry is discretized into grid nodes
  • Finite Element (Fig. 13.5 text)
  • Real geometry is discretized into elements
  • In either case, the governing differential
    equations can be simplified

7
Governing Equations
  • Conservation of Energy, Darcys Law in 3D.(pages
    125-128)
  • Equation 4.42, p. 128 (unsteady state)
  • Laplaces Equation, (Eq. 4.43, steady state)
  • Finite Difference Notation Solution is much
    simplerEq. 13.1, p. 521 (without recharge)
  • Function of head and distance
  • Boundary Conditions-Known Head or Known Flow

8
GW Models
  • Excel-based Modeling (Ex., p. 531)
  • Visual MODFLOW
  • MODFLOW, the code is from the USGS
  • Waterloo Hydrogeologic makes it easier to work
    with
  • Generally working with an accepted model is
    better than developing a new one, particularly
    from a regulatory perspective
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