The peak discharge is given as \( 180 \, {m}^3/{s} \), and the base flow is \( 30 \, {m}^3/{s} \).
The infiltration loss is 0.2 cm/h, and the total rainfall depth is 6.6 cm.
The peak of the 3-hour unit hydrograph \( Q_p \) is calculated using the formula: \[ Q_p = \frac{{Peak discharge} - {Base flow}}{R - \phi t} \] Where: - Peak discharge = \( 180 \, {m}^3/{s} \)
- Base flow = \( 30 \, {m}^3/{s} \)
- \( R = 6.6 \, {cm} \) (rainfall depth)
- \( \phi = 0.2 \, {cm/h} \) (infiltration loss)
- \( t = 3 \, {hours} \) (duration of the storm) Substitute the values into the formula: \[ Q_p = \frac{180 - 30}{6.6 - 0.2 \times 3} = \frac{150}{5.4} = 27.78 \, {m}^3/{s} \] Thus, the peak value of the 3-hour unit hydrograph is \( 25 \, {m}^3/{s} \).
For the beam and loading shown in the figure, the second derivative of the deflection curve of the beam at the mid-point of AC is given by \( \frac{\alpha M_0}{8EI} \). The value of \( \alpha \) is ........ (rounded off to the nearest integer).
In levelling between two points A and B on the opposite banks of a river, the readings are taken by setting the instrument both at A and B, as shown in the table. If the RL of A is 150.000 m, the RL of B (in m) is ....... (rounded off to 3 decimal places).