Skip to main content

Muskingum routing, K=10, x=0.20

Short answer

Muskingum coefficients: C0=0.0476, C1=0.4286, C2=0.5238 for K=10h, x=0.2, Δt=5h. Routing yields peak inflow 45 m³/s at 15h, peak outflow 35.00 m³/s at 25h. Attenuation = 10.00 m³/s, lag = 10 h.

Route the following hydrograph through a river reach with routing parameters K and x as 10 and 0.20, respectively. Take outflow discharge at the start of inflow flood as 5 m3^3/s. Also estimate attenuation and lag of peak.

Time (hr)0510152025303540
Inflow (m3^3/s)5103045403018128

Method

Muskingum routing: O2=C0I2+C1I1+C2O1O_2 = C_0 I_2 + C_1 I_1 + C_2 O_1, where

C0=−Kx+0.5ΔtK−Kx+0.5Δt,C1=Kx+0.5ΔtK−Kx+0.5Δt,C2=K−Kx−0.5ΔtK−Kx+0.5ΔtC_0 = \frac{-Kx + 0.5\Delta t}{K - Kx + 0.5\Delta t},\quad C_1 = \frac{Kx + 0.5\Delta t}{K - Kx + 0.5\Delta t},\quad C_2 = \frac{K - Kx - 0.5\Delta t}{K - Kx + 0.5\Delta t}

Here K=10K = 10 h, x=0.2x = 0.2, Δt=5\Delta t = 5 h, so K−Kx+0.5Δt=10.5K - Kx + 0.5\Delta t = 10.5 h.

C0=−(10)(0.2)+2.510.5=0.0476C1=(10)(0.2)+2.510.5=0.4286C2=8−2.510.5=0.5238\begin{aligned} C_0 &= \frac{-(10)(0.2) + 2.5}{10.5} = 0.0476\\ C_1 &= \frac{(10)(0.2) + 2.5}{10.5} = 0.4286\\ C_2 &= \frac{8 - 2.5}{10.5} = 0.5238\end{aligned}

Check: C0+C1+C2=1.0000C_0 + C_1 + C_2 = 1.0000.

Routing table

t (h)IC0·I2C1·I1C2·O1O (m³/s)
05.00---5.00
510.000.482.142.625.24
1030.001.434.292.748.46
1545.002.1412.864.4319.43
2040.001.9019.2910.1831.37
2530.001.4317.1416.4335.00
3018.000.8612.8618.3332.05
3512.000.577.7116.7925.07
408.000.385.1413.1318.66

Peak attenuation and lag

  • Peak inflow = 45 m³/s at t = 15 h
  • Peak outflow = 35.00 m³/s at t = 25 h
  • Attenuation of peak = 45 − 35.00 = 10.00 m³/s (22.2 % of the inflow peak)
  • Lag of peak = 25 − 15 = 10 h (to the nearest time step)

✓ Answer checked by Claude Sonnet 5.5

All Engineering Hydrology chapter 7 questions →