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Horizontal Infiltration Method for Determining Brooks-Corey Model Parameters

^a Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Building 917, 3 Datun Road, Anwai, Beijing 100101, China
^b Dep. of Agronomy, Iowa State Univ., Ames, IA 50011
^c State Key Lab. of Soil Erosion and Dryland Farming, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, 712100, China

View larger version (16K): [in a new window]   Fig. 1. Cumulative infiltration and infiltration rate versus wetting front distance for three numerical conditions: (a) and (d) are for numerical Soil 1, (b) and (e) are for numerical Soil 2, and (c) and (f) are for numerical Soil 3.

View larger version (9K): [in a new window]   Fig. 2. Wetting front distance squared versus time for three numerical conditions: (a) is for numerical Soil 1, (b) is for numerical Soil 2, and (c) is for numerical Soil 3.

View larger version (16K): [in a new window]   Fig. 3. Given and estimated water retention curves and hydraulic conductivity functions for three numerical conditions: (a) and (d) are for numerical Soil 1, (b) and (e) are for numerical Soil 2, and (c) and (f) are for numerical Soil 3.

View larger version (8K): [in a new window]   Fig. 4. Numerically calculated and assumed distributions of hd/h for three numerical soil conditions: (a) is for numerical Soil 1, (b) is for numerical Soil 2, and (c) is for numerical Soil 3.