Published online 24 August 2006
Published in Vadose Zone J 5:978-989 (2006)
DOI: 10.2136/vzj2006.0003
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
Quantifying the Pore Size Spectrum of Macropore-Type Preferential Pathways under Transient Flow
K.-J.S. Kunga,*,
E. J. Kladivkob,
C. S. Hellingc,
T. J. Gishd,
T. S. Steenhuise and
D. B. Jaynesf
a Dep. Soil Science, Univ. of Wisconsin, Madison, WI 53706-1299
b Dep. Agronomy, Purdue Univ., West Lafayette, IN 47907
c Sustainable Perennial Crops Lab., USDA-ARS, BARC-W, Beltsville, MD 20705-2350
d Hydrology and Remote Sensing Lab., USDA-ARS, BARC-W, Beltsville, MD 20705-2350
e Dep. Biological and Environmental Engineering, Cornell University, Ithaca, NY 14850
f National Soil Tilth Lab., USDA-ARS, Ames, IA 50011

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Fig. 1. Normalized tracer mass flux breakthrough patterns. The open symbols were measured values from Kung et al. (2000a). The solid lines are the best-fitted breakthrough curves based on pore spectra with parameters shown in Table 3.
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Fig. 2. Normalized tracer mass flux breakthrough patterns. The open symbols were measured from the second irrigation event. The solid lines are the best-fitted breakthrough curves based on pore spectra with parameters shown in Table 4.
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Fig. 3. Normalized tracer mass flux breakthrough patterns. The open symbols were measured from the third irrigation event. The solid lines are the best-fitted breakthrough curves based on pore spectra with parameters shown in Table 5.
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Fig. 4. The portions of normalized tracer mass flux breakthrough patterns that had tail slopes nearly equal to 3 on log-log scale. The suffix of each label indicates irrigation event (e.g., PFBA-1 indicates the tracer breakthrough curve from the first irrigation event).
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Fig. 5. Four hypothetical pore spectra to demonstrate how each parameter would alter the shape of a spectrum.
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Fig. 6. Pore spectra with parameters (Table 3) based on best fit of four sequentially applied tracers mass flux breakthrough patterns from Kung et al. (2000a).
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Fig. 8. Volumetric water flux of pores with spectra shown in Fig. 6.
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Fig. 9. Pore spectra with parameters (Table 4) based on best fit of four tracers mass flux breakthrough patterns from the second irrigation event. Bromide #1 (broken line) is the pore spectrum of bromide from Fig. 6.
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Fig. 10. Pore spectra with parameters (Table 5) based on best fit of four tracers mass flux breakthrough patterns from the third irrigation event. Bromide #1 (broken line) is the pore spectrum of bromide from Fig. 6.
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Fig. 11. Tile flow and concentration breakthrough patterns of four tracers and nitrate from Kung et al. (2000a).
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Copyright © 2006 by the Soil Science Society of America.