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Modeling subsurface iron removal

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Stagnant zones. Or: Biological activity? Complexes? Change groundwater ... Implementation stagnant zones. Influence conclusions on accumulation. Finish model ... – PowerPoint PPT presentation

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Title: Modeling subsurface iron removal


1
Modeling subsurface iron removal
  • Geochemical modeling of subsurface aeration at
    Schuwacht Lekkerkerk

Harmen van der Laan
Faculty of Civil EngineeringMsc. Water
Management Specilization Drinking Water
2
Content
  • Subsurface iron removal
  • Objective research
  • Results
  • Conclusions
  • Next steps Recommendations

3
Content
  • Subsurface iron removal
  • Objective research
  • Results
  • Conclusions
  • Next steps Recommendations

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3
4
Subsurface iron removal
Injection
Extraction
injected water
Fe2 front
Fe2 front
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5
Measured data
5
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Measured data
July 1998 June 2000
March 2004 June 2005
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7
Original Model
V/Vi
7
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Expanded model
8
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Content
  • Subsurface iron removal
  • Objective research
  • Results
  • Conclusions
  • Next steps Recommendations

November 11, 2009
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10
Objective
  • The objective of this research project is to
  • Find a theoretical foundation to explain the
    development of the iron front over the successive
    cycles
  • Enhance the existing model to obtain a proper
    description of the measured iron concentrations

10
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11
Content
  • Subsurface iron removal
  • Objective research
  • Results
  • Conclusions
  • Next steps Recommendations

November 11, 2009
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12
Results
  • Goethite / Ferrihydrite
  • Ion exchange vs. Adsorption
  • Transport modeling

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13
Goethite vs. Ferrihydrite
  • Ferrihydrite
  • Hfo, FeOH3, Fe5HO84H2O
  • Unstable, unstructured
  • Amorphous / Aquaeous
  • Spec. area 600 m2/g
  • 2 sites / nm2
  • pHPZC 8.1
  • Solubility log K 2 4.5
  • Observed by KIWA Research
  • Goethite
  • a-FeOOH
  • Stable
  • Crystalline
  • Spec. area 60 m2/g
  • 2 - 10 sites / nm2
  • pHPZC 8.7
  • Solubility log K -1
  • Observed by Mettler (2002)

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14
Surface complexation theory
Fe2
Fe2
Fe2
OH
OH
OH
OH
OH
/ - depends on pH
Surface area
Number of sites
15
Site density
16
Surface characterization
17
Goethite vs. Ferrihydrite ?
  • Variations in site density and surface area only
    result in small bandwidth
  • Differences between Goethite and Ferrihydrite not
    the main limitation

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18
Results
  • Goethite / Ferrihydrite
  • Ion exchange vs. Adsorption
  • Transport modeling

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19
Exchange
20
Exchange
21
Results
  • Goethite / Ferrihydrite
  • Ion exchange vs. Adsorption
  • Transport modeling

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22
Retardation / Front spreading
23
Macrodispersivity
Microdispersion
24
Dispersion
25
Stagnant zones
26
Stagnant zones
27
Results
  • Subsurface iron removal
  • Objective research
  • Results
  • Preliminary Conclusions
  • Next steps Recommendations

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28
Preliminary Conclusions
  • Objective is Theoretical foundation and a better
    model
  • Many flavors, but I need too pick one
  • Model starts to describe the correct
    retardationmainly because of dispersion /
    stagnant zones

29
Possible explanation
Ferric iron
  • Kinetics decrease SI in time / combination
    Ferrihydrite Goethite
  • Stagnant zones
  • OrBiological activity?Complexes? Change
    groundwater composition?

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30
Next steps Recommendations
  • Next steps
  • Tracer in groundwater for dispersion?
  • Implementation stagnant zones
  • Influence conclusions on accumulation
  • Finish model
  • Recommendations
  • Column experiments separate transport model
    from geochemistry
  • Research Ferrihydrite / Goethite

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31
Questions?
November 11, 2009
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