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Soil Wetting and Texture Effects on Aggregate Stability, Seal Formation, and Erosion

M. Lado*, M. Ben-Hur and I. Shainberg

Institute of Soil, Water and Environmental Sciences, the Volcani Centre, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel



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Fig. 1. Infiltration rate as a function of cumulative rainfall for the three soils (with 230, 410, and 620 g kg–1 clay), two WR treatments (1 and 5 mm h–1), and three antecedent moisture content (AMC) treatments (air dry, 0.25 and 0.5 field capacity). Rain intensity was 42 mm h–1. Bars indicate standard deviation.

 


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Fig. 2. Final infiltration rate of the three air-dried soils and the three soils prewetted to AMC of 0.5 FC with a WR of 1 mm h–1. Values of a treatment in different soils followed by the same upper case letter and values of the treatments within a soil followed by the same lower case letter are not significantly different ({alpha} = 0.05).

 


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Fig. 3. (A) Mean weight diameter (MWD) determined by fast and slow wettings as a function of clay content in the soil. Regressions are significant at P < 0.05. (B) Slaking values (difference between fast and slow MWD) as a function of the clay content in the soil. Bars indicate standard deviation.

 


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Fig. 4. Final infiltration rate of the three soils as a function of wetting rate (WR) and antecedent moisture content (AMC) treatments. Values of a treatment in different soils followed by the same upper case letter and values of the treatments within a soil followed by the same lower case letter are not significantly different ({alpha} = 0.05).

 


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Fig. 5. Total soil loss of the three soils obtained with three wetting rates (WR) and three antecedent moisture content (AMC) treatments. Values of a treatment in different soils followed by the same upper case letter and values of the treatments within a soil followed by the same lower case letter are not significantly different ({alpha} = 0.05).

 





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