Question: A storm with 1 0 cm precipitation produced a direct surface runoff of 5 . 3 cm in the equivalent depth unit. The time distribution

A storm with 10 cm precipitation produced a direct surface runoff of 5.3 cm in the equivalent depth unit. The time distribution of the storm is given in the table.
(a) Estimate the \(\emptyset \)-index of the storm and the excess rainfall hyetogrph.
(b) Calculate the runoff coefficient.
(c) If the \(\emptyset \)-index method is not good enough, we want to use Green-Ampt method for correction. The field survey shows the soil parameters as: \(\mathrm{K}=0.34\mathrm{~cm}/\mathrm{h},\psi=\)\(9.98\mathrm{~cm},\theta e=0.34\), and \( S e=0.2\). What kind of soil you think it is?
(d) Use Green-Ampt method to calculate the abstraction and excess rainfall.
(e) Calculate the runoff coefficient
(f) Now we still want use \(\emptyset \)-index method to simplify this problem. Any suggestion to adjust the \(\varnothing \)-index? Just let me know higher or lower will be fine.
(g) Assume the \(\emptyset \)-index is more accurate and we know the value of hydraulic conductivity is not certain. Do you think we overestimate or underestimate K , how you calibrate the value? Why? (Please give a brief answer. Do not try to calculate the correct K value.)
(h) A senior engineering told you try to calibrate the suction head instead of conductivity. What's your opinion of \(\psi \)? Did we overestimate or underestimate it? Why? (Same, please give a brief answer. Do not try to calculate the correct \(\psi \) value.)
A storm with 1 0 cm precipitation produced a

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