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Published online 13 May 2005
Published in Vadose Zone J 4:291-299 (2005)
DOI: 10.2136/vzj2004.0103
© 2005 Soil Science Society of America
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Simplified Method to Estimate the Green–Ampt Wetting Front Suction and Soil Sorptivity with the Philip–Dunne Falling-Head Permeameter

C. M. Regaladoa,*, A. Rittera, J. Álvarez-Benedíb and R. Muñoz-Carpenac

a Instituto Canario Investigaciones Agrarias (ICIA), Dep. Suelos y Riegos, Apdo. 60 La Laguna, 38200 La Laguna, Spain
b Instituto Tecnológico Agrario de Castilla y León, Apdo. 172, 47080 Valladolid, Spain
c Agricultural and Biological Engineering Dep., University of Florida, 101 Frazier Rogers Hall, P.O. Box 110570, Gainesville, FL 32611-0570



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Fig. 1. Geometrical analog of the Philip–Dunne falling-head permeameter.

 


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Fig. 2. (a) tmax/tmed vs. {Psi}, and (b) tmax/tmed vs. {tau}max relationships for the 308 measurements performed in eight different soils (represented by different symbols). Insert in (b) represents tmax/tmed vs. {tau}max values where {Psi} is positive.

 


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Fig. 3. Goodness of fit of both derived equations (Eq. [8] and [9]) to compute Ks, {Psi}, and S evaluated by comparing these with the solution obtained by solving numerically the full system (Eq. [6]).

 


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Fig. 4. Plot of the data pairs (tmax/tmed, {Psi} > 0) and the curve tmax/tmed = f ({Delta}{theta}, {Psi}) obtained from Eq. [6] for two different water content increments: {Delta}{theta} = 0.05m3 m–3 (lower curve) and {Delta}{theta} = 0.5 m3 m–3 (upper curve). Notice that the axes are inverted with respect to Fig. 2.

 


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Fig. 5. Sensitivity analysis of Ks, {Psi}, and S (OY axes) to variations of parameters: ho, tmax, tmed, {Delta}{theta}, and gc (represented by different line types) within the interval [–20%, 20%], for various initial ratios tmax/tmed = 2.61, 3.74, and 5.38 (from left to right). In those cases where the parameter combination yielded {Psi} < 0, the solving algorithm ceases to compute and thereby no SC was calculated. The sensitivity coefficient, SC, represents the percentage of variation with respect to the initial value (OY axes).

 


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Fig. 6. Sensitivity analysis of Ks, {Psi}, and S (OY axes) to variations of parameters: ho, tmax, tmed, {Delta}{theta}, and gc (represented by different line types) within the interval [–20%, 20%], for an initial ratio tmax/tmed = 5.38 with different initial values of {Delta}{theta} = 0.10, 0.26, and 0.35 m3 m–3 (from left to right). In those cases where the parameter combination yielded {Psi} < 0, the solving algorithm ceases to compute and thereby no SC was calculated. The sensitivity coefficient, SC, represents percentage of variation with respect to the initial value (OY axes).

 





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