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Use of Brooks-Corey Parameters to Improve Estimates of Saturated Conductivity from Effective Porosity

D.J. Timlina, L.R. Ahujab, Ya. Pachepskyc, R.D. Williamsd, D. Gimeneze and W. Rawlsf

a USDA-ARS Systems Research Lab, Bldg. 007, Rm 116, 10300 Baltimore Ave, Beltsville, MD 20705 USA
b USDA-ARS Great Plains Systems Research Unit, P.O. Box E, Ft. Collins, CO 80522 USA
c Dept of Botany, Duke University, Durham, NC 27708 USA
d USDA-ARS Grazing Lands Research Laboratory, P.O. Box 1199, El Reno, OK 73036-1199 USA
e Dept. of Environmental Sciences, Rutgers, The State University of NJ, 14 College Farm Rd., New Brunswick, NJ 08901 USA
f USDA-ARS Hydrology Laboratory, Bldg 007, Rm 112, 10300 Baltimore Ave., Beltsville, MD 20705 USA



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Fig. 1 Pore-size distribution index vs. Ks for the Southern Region (SR) and Rawls (RA) data sets. Values are means for textural classes

 


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Fig. 2 Predicted and measured Ks for the Southern Region data set determined using (a) effective porosity ({phi}e) only as a predictor and (b) effective porosity ({phi}e) and the pore size distribution index ({lambda})

 


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Fig. 3 The intercept of the Kozeny-Carman equation (B) as a function of (a) {lambda}, and (b) hb. The value of B is calculated as Ks ({phi}e2.5). The data are means for textural classes

 


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Fig. 4 Relationship between the intercept B and R/l for Southern Region (SR) and Rawls (RA) data sets. The value of B is calculated as Ks ({phi}2.5e). The data are means for textural classes

 


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Fig. 5 Calculated and measured values of Ks, where the intercept (B) for Eq. [1] has been calculated using values of {lambda} and hb, and the relationship between B and R/l for the Rawls data set given in Fig. 4

 


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Fig. 6 Relationship between measured Ks and values predicted using Eq. [2] when fit to the Southern Region (SR) data set

 


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Fig. 7 Probability plot of measured Ks and values estimated by the four models. Ks values are from the full Southern Region (SR) data set

 





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