Published online 28 June 2005
Published in Soil Sci Soc Am J 69:1196-1208 (2005)
DOI: 10.2136/sssaj2004.0208
© 2005 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
Quantifying Pore-Size Spectrum of Macropore-Type Preferential Pathways
K.-J. S. Kunga,*,
M. Hankea,
C. S. Hellingb,
E. J. Kladivkoc,
T. J. Gishb,
T. S. Steenhuisd and
D. B. Jaynese
a Dep. Soil Science, Univ. of Wisconsin-Madison, Madison, WI 53706-1299
b Hydrology Lab., USDA-ARS, BARC-W, Beltsville, MD 20705-2350
c Dep. Agronomy, Purdue Univ., West Lafayette, IN 47907
d Dep. Biological and Environmental Engineering, Cornell Univ., Ithaca, NY 14850
e National Soil Tilth Lab., USDA-ARS, Ames, IA 50011

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Fig. 1. Bromide breakthrough curve from tile drain under a 4.4 mm h1 steady-state irrigation rate (from Gish et al., 2004). Calculated curve is best fit of Eq. [5] to data.
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Fig. 2. Tracer breakthrough curves from tile drain under a 2.4 mm h1 steady-state irrigation rate. The o-TFMBA (o-trifluoromethylbenzoic acid) experiment was conducted in autumn 2001, while the PFBA (pentafluorobenzoic acid) experiment was conducted in spring 2002. Calculated curves are best fit of Eq. [5] to data.
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Fig. 3. Pentafluorobenzoic acid (PFBA) breakthrough curve from tile drain under a 1.2 mm h1 steady-state irrigation rate. Calculated curve is best fit of Eq. [5] to data.
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Fig. 4. Theoretical pore spectra based on constraints from conventional conceptualization as steady-state infiltration rates increase.
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Fig. 5. Pore spectra for three infiltration rates based on fitted parameters after relaxing initial constraints. The spectra labeled with show the difference between two adjacent spectra.
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Fig. A1. Three phases of convective transport of a chemical through a capillary tube. r is the distance from the center of the tube (m), r1 is the location where the new water front reaches the exit, and r2 is the location where the chemical front reaches the exit.
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Fig. A2. Typical mass flux breakthrough pattern during the three phases of convective transport of a chemical through a capillary tube.
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Copyright © 2005 by the Soil Science Society of America.