The infiltration capacity of a soil follows Horton's exponential model
f=C1+C2e−kt. During an experiment, the initial 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, up to two decimal places) is
- 0.99