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Spatial and Statistical Similarities of Local Soil Water Fluxes

Bing Cheng Si*

Dep. of Soil Science, University of Saskatchewan, Saskatoon, SK. Canada S7N 5A8



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Fig. 1. Measured local soil water flux (solid line) and application rate (dashed line) during constant flux infiltration experiments for application rates of (a) 0.9, (b) 1.5, (c) 2.6, and (d) 3.3 cm h-1 for 0.2-m depth.

 


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Fig. 2. Measured local soil water flux (solid line) and application rate (dashed line) during constant flux infiltration experiments for application rates of (a) 0.9, (b) 1.5, (c) 2.6, and (d) 3.3 cm h-1 for 0.4-m depth.

 


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Fig. 3. Measured local soil water flux (solid line) and application rate (dashed line) during constant flux infiltration experiments for application rates of (a) 0.9, (b) 1.5, (c) 2.6, and (d) 3.3 cm h-1 for 0.6-m depth.

 


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Fig. 4. Measured local soil water flux (solid line) and application rate (dashed line) during constant flux infiltration experiments for application rates of (a) 0.9, (b) 1.5, (c) 2.6, and (d) 3.3 cm h-1 for 0.8-m depth.

 





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The Plant Genome
Copyright © 2002 by the Soil Science Society of America.