310 likes | 526 Views
Modeling subsurface iron removal. Geochemical modeling of subsurface aeration at Schuwacht Lekkerkerk. Harmen van der Laan. Faculty of Civil Engineering Msc. Water Management Specilization Drinking Water. Content. Subsurface iron removal Objective research Results Conclusions
E N D
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
Content • Subsurface iron removal • Objective research • Results • Conclusions • Next steps & Recommendations
Content Subsurface iron removal Objective research Results Conclusions Next steps & Recommendations September 21, 2014 3
Subsurface iron removal Injection Extraction O2 front injected water injected water injected water O2 front 1 1 1 1 C/C0 C/C0 C/C0 C/C0 Fe2+ front Fe2+ front 0 0 0 0 Fe2+ front Fe2+ front September 21, 2014 4
Measured data September 21, 2014 5
Measured data July 1998 – June 2000 March 2004 – June 2005 September 21, 2014 6
‘Original’ Model V/Vi September 21, 2014 7
main limitation original model No explanation for the phenomena of the increasing spread of the (iron) front over the successive cycles Expanded model September 21, 2014 8
Content Subsurface iron removal Objective research Results Conclusions Next steps & Recommendations September 21, 2014 9
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 September 21, 2014 10
Content Subsurface iron removal Objective research Results Conclusions Next steps & Recommendations September 21, 2014 11
Results Goethite / Ferrihydrite Ion exchange vs. Adsorption Transport modeling September 21, 2014 12
Goethite vs. Ferrihydrite Ferrihydrite Hfo, FeOH3, Fe5HO8·4H2O 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 α-FeOOH • Stable • Crystalline • Spec. area ≈ 60 m2/g • 2 - 10 sites / nm2 • pHPZC 8.7 • Solubility log K = -1 • Observed by: Mettler (2002) September 21, 2014 13
Surface complexation theory Fe2+ Fe2+ Fe2+ OH OH OH OH OH + / - depends on pH Surface area Number of sites
Goethite vs. Ferrihydrite ? • Ferrihydrite • Variations in site density and surface area only result in small bandwidth • Differences between Goethite and Ferrihydrite not the main limitation • α-FeOOH ‘solubility’ decreases in time September 21, 2014 17
Results Goethite / Ferrihydrite Ion exchange vs. Adsorption Transport modeling September 21, 2014 18
Exchange • Exchange and adsorption hard to distinguish • Exchange capacity = lumped parameter • Empirical formula does not give correct output
Results Goethite / Ferrihydrite Ion exchange vs. Adsorption Transport modeling September 21, 2014 21
Macrodispersivity Microdispersion Injection well
Results Subsurface iron removal Objective research Results Preliminary Conclusions Next steps & Recommendations September 21, 2014 27
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
Possible explanation Ferric iron • Kinetics: decrease SI in time / combination Ferrihydrite – Goethite • Stagnant zones • Or:Biological activity?Complexes? Change groundwater composition? September 21, 2014 29
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 September 21, 2014 30
Questions? September 21, 2014 31