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Spatial Variability of Solute Leaching

Experimental Validation of a Quantitative Parameterization

Gerrit H. de Rooija and Frank Stagnittib

a Wageningen Univ., Dep. of Environmental Sci., Sub-dep. Water Resour., Nieuwe Kanaal 11, 6709 PA Wageningen, The Netherlands
b Deakin Univ., School of Ecology and Environ., Center for Applied Dynamical Systems and Environmental Modelling, P.O. Box 423, Warrnambool Victoria, Australia 3280



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Fig. 1 The cumulative distribution function (cdf) given by the integral of the beta distribution function P defined in Eq. [1]. When the cdf is fitted to data of fractional solute leaching (sorted in descending order) with fractional sampling area, the slope P(z) at any point on the curve (represented by the straight line) equals the ratio of the infiltration area (Ai) over the outflow area (Ao). Hence, P(z) quantifies the severity of preferential flow for one stream tube. The coordinates define the fractions of the sampling plane (z) and the soil surface (cumulative probability density) occupied by streamtubes with stronger preferential flow than that corresponding to P(z)

 


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Fig. 2 Spatial distribution of chloride leaching from the lysimeter bottom. The center of the lysimeter is at . Each grid point represents a measurement location. The flat areas in the corners are outside the lysimeter cylinder. Average leaching (28.1 mmol Cl-) is indicated by the bold contour line. Cumulative leaching amounts in excess of the average have contour lines at multiples of 25 mmol Cl-

 




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Fig. 3 Observed and fitted fractions of leached chloride with either the fraction of the entire lysimeter bottom (a), or with the fraction of quadrants (b) and octants (c) of the bottom. The displayed quadrants and octants are those with the smallest and largest value of the HI (see Eq. [2])

 


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Fig. 4 The effect of the size of the individual sampling areas on the fitted values of {alpha} and {zeta} (Eq. [1]) and the HI (Eq. [2])

 


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Fig. 5 Observations and fitted curves for 2n sampling locations randomly selected from a total of 300. The curves for n >= 5 (including the observed and fitted curves for all 300 samples) are nearly identical

 


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Fig. 6 Fitted values of parameters {alpha} and {zeta} (Eq. [1]), as well as the HI (Eq. [2]) as a function of the number of sampling locations used in the fitting procedure

 



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Fig. 7 Fitted curves of the cumulative beta distribution function (a), and the beta distribution function P (see Eq. [1]) (b), for different sample sizes (cm2). The curves for flow in a uniform soil with 25% of the soil occupied by fingers and a uniform soil without fingering are included for comparison

 





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