The correct answer is (d) ft = fC + (fO – fC) e^-K.t
Explanation: Horton’s equation assumes an infinite water supply at the surface i.e. it assumes the saturation conditions at the soil surface. The infiltration rate at any time‘t’ is given by –
ft = fC + (fO – fC) e^-K.t
Where fC = final constant rate of infiltration at saturation, fO = initial rate of infiltration capacity, k is the decay constant depending upon soil and vegetation and t = time from the beginning of the storm.