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Right arrow Vadose Zone Processes and Chemical Transport

Estimating Uncertain Flow and Transport Parameters Using a Sequential Uncertainty Fitting Procedure

K. C. Abbaspoura,*, C. A. Johnsona and M. Th. van Genuchtenb

a Swiss Federal Inst. for Environmental Science and Technology (EAWAG), Ueberlandstrasse 133, P.O. Box 611, CH-8600 Dübendorf, Switzerland
b USDA-ARS, George E. Brown, Jr. Salinity Lab., 450 West Big Springs Road, Riverside, CA 92507



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Fig. 1. Water retention and hydraulic conductivity curves as used in MACRO.

 


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Fig. 2. An example showing the partitioning of a response signal into different compartments: base flow (c1), the recession or rise (c2), intermediate peaks (c3), and large peaks (c4). The weights are calculated such that each compartment contributes equally to the objective function.

 


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Fig. 3. Calibration results for flow and transport at Lostorf. The blue curves represent the 95% prediction uncertainty (95PPU), the red curve represents the measured data, and the green curve shows the best fit of optimization.

 


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Fig. 4. Test results of flow and transport at Lostorf. The blue curves represent the 95% prediction uncertainty (95PPU), the red curve represents the measured data, and the green curve shows the best fit of optimization.

 


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Fig. 5. (A) Calibration and (B) test results for flow at Seckenberg. The blue curves represent the 95% prediction uncertainty (95PPU), the red curve represents the measured data, and the green curve shows the best fit of optimization.

 


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Fig. 6. The d-3–hb-3 response surface obtained after 2000 simulations. All other parameters were kept constant.

 


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Fig. 7. The d-3–{theta}b-3 response surface obtained after 2000 simulations. All other parameters were kept constant.

 


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Fig. 8. The d-3–n* response surface obtained after 2000 simulations. All other parameters were kept constant.

 


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Fig. 9. The d-3–n* response surface obtained after 10000 simulations. All other parameters were kept constant.

 


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Fig. 10. The d-3–{theta}b response surface obtained after 10000 simulations. Parameters d-3, {theta}b-3, hb-3, and n* were varied simultaneously, while all others were kept constant.

 





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