The infiltration capacity of a soil follows the Horton's exponential model f = c₁ + C₂ e-kt. During an experiment, the intial infiltration capacity was observed to be 200 mm/hr. After a long time the infiltration capacity was reduced to 25 mm/h. If the infiltration capacity after 1 hour was 90 mm/ h the value of the decay rate constant k (in h-¹,
The infiltration capacity of a soil follows the Horton's exponential model f = c₁ + C₂ e-kt. During an experiment, the intial infiltration capacity was observed to be 200 mm/hr. After a long time the infiltration capacity was reduced to 25 mm/h. If the infiltration capacity after 1 hour was 90 mm/ h the value of the decay rate constant k (in h-¹,
Chapter2: Loads On Structures
Section: Chapter Questions
Problem 1P
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