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Flood Estimation and Routing Questions and Answers

1.

The relationship between outflow Q in m3 s−1 and storage S in m3 for an emergency spillway in a reservoir is Q = S/4000. Inflow, outflow and storage are assumed to be zero at time t = 0. If the inflow rate is 300 m3 s−1 at the end of t = 3 hours, the outflow rate in m3 s−1 is

Exam Year(s)

GATE AG - 2012,

Answer: C

The keyed outflow is 172.34 m3 s−1.

The key follows the storage (continuity) equation applied over a single 3-hour routing interval, with the inflow rising linearly from 0 to 300 m3 s−1 and the outflow averaged over the interval. With \(\Delta t = 10800\) s and \(S = 4000\,Q\):

\[ \begin{aligned} \tfrac{I_{1}+I_{2}}{2}\Delta t - \tfrac{Q_{1}+Q_{2}}{2}\Delta t &= S_{2} - S_{1} \\ \tfrac{300}{2}(10800) - \tfrac{Q_{2}}{2}(10800) &= 4000\,Q_{2} \\ 1620000 &= 9400\,Q_{2} \\ Q_{2} &= 172.34 \end{aligned} \]

Splitting the 3 hours into shorter steps, or solving the differential equation exactly, gives a somewhat higher value of about 196 m3 s−1, which is not offered; the paper's options are built on the one-step calculation. The other values do not come from either form of the equation.

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2.

The information needed for estimating the design flood using Rational formula is

Exam Year(s)

GATE AG - 2023,

Answer: D

The Rational formula needs the time of concentration of the catchment.

The formula is \(Q = CIA/360\) (Q in m3/s, I in mm/h, A in ha). The rainfall intensity I must be taken for a storm duration equal to the time of concentration, the time for water from the most remote point to reach the outlet, because that is when the whole catchment contributes and the peak occurs.

Cumulative infiltration and antecedent moisture are not inputs; their effect is lumped into the runoff coefficient C (they matter in the SCS curve number method). A catchment shape factor is not part of the Rational formula either, though shape influences the time of concentration.

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