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Using MODFLOW 2000 to model ET and recharge for shallow ground water problems.

Rebecca C Doble1, Craig T Simmons, Glen R Walker

  • 1CSIRO Land and Water, PMB 2 GlenOsmond, South Australia 5064, Australia. rebecca.doble@csiro.au

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Summary

Shallow groundwater systems require continuous modeling of recharge and evapotranspiration. This study modifies MODFLOW to better represent these fluxes, improving accuracy for water table dynamics and salinization studies.

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Area of Science:

  • Hydrogeology
  • Environmental Science
  • Water Resource Management

Background:

  • Shallow groundwater systems exhibit significant flux variations due to small water table changes.
  • Accurate modeling requires nonlinear relationships for recharge and evapotranspiration in thin unsaturated zones.
  • Existing MODFLOW packages may not adequately represent dynamic shallow groundwater conditions.

Purpose of the Study:

  • To modify MODFLOW's recharge and evapotranspiration packages for continuous, head-dependent flux representation.
  • To improve the modeling of groundwater systems with shallow water tables.
  • To investigate salinization patterns on a floodplain using enhanced groundwater flux modeling.

Main Methods:

  • Modified MODFLOW 2000 recharge and segmented evapotranspiration packages.
  • Developed a continuous recharge-discharge function dependent on head.
  • Applied the modified model to a saline, semiarid floodplain.

Main Results:

  • The enhanced function allows for continuous representation of groundwater flux as a function of head.
  • The modified model accurately captures recharge and evapotranspiration dynamics in shallow groundwater environments.
  • Spatial salinization patterns were analyzed on the floodplain.

Conclusions:

  • Continuous groundwater flux modeling is essential for shallow groundwater systems.
  • The modified MODFLOW approach enhances the representation of recharge and evapotranspiration.
  • This methodology aids in understanding and managing salinization in arid and semiarid regions.