Skip to main content

Slope-area discharge, 10 km reach

Short answer

Slope-area method with Manning’s conveyance and trial correction for velocity head and expansion eddy loss (ke=0.3) gives discharge ≈ 44.2 m³/s.

The high flow water surface elevations of a stream at two sections 10 km apart are 306.920 m and 306.650 m. The cross-sectional area and wetted perimeters are as follows:

SectionArea (m2^2)Wetted perimeter (m)
A73.326.80
B93.430.23

Assume n = 0.02. The eddy loss coefficient is 0.30 for gradual expansion and 0.10 for gradual contraction. Estimate the discharge in the stream. Section A is upstream of B.

Given: A1=73.3A_1=73.3 m2^2, P1=26.80P_1=26.80 m, A2=93.4A_2=93.4 m2^2, P2=30.23P_2=30.23 m, n=0.02n=0.02, L=10L=10 km, fall h1−h2=306.920−306.650=0.27h_1-h_2 = 306.920-306.650 = 0.27 m. Velocity-head coefficients are taken as α1=α2=1\alpha_1=\alpha_2=1. The area increases downstream, so the reach is an expansion and ke=0.3k_e = 0.3.

Method: Manning's equation gives conveyance K=1nAR2/3K=\dfrac{1}{n}AR^{2/3} and Q=KSfQ = K\sqrt{S_f}. The friction slope is found from the energy equation between the two sections, so the discharge is found by trial.

Step 1: Conveyance

R1=73.326.8=2.7351 m,R2=93.430.23=3.0896 mR_1=\frac{73.3}{26.8}=2.7351\ \text{m},\qquad R_2=\frac{93.4}{30.23}=3.0896\ \text{m} K1=10.02×73.3×2.73512/3=7167.8,K2=10.02×93.4×3.08962/3=9906.6K_1=\frac{1}{0.02}\times73.3\times2.7351^{2/3}=7167.8,\qquad K_2=\frac{1}{0.02}\times93.4\times3.0896^{2/3}=9906.6 Km=K1K2=8426.6K_m=\sqrt{K_1K_2}=8426.6

Step 2: First trial (no velocity head)

Sf=0.2710000,Q1=KmSf=43.786 m3/sS_f=\frac{0.27}{10000},\qquad Q_1=K_m\sqrt{S_f}=43.786\ \text{m}^3/\text{s}

Step 3: Correct for velocity head and eddy loss

hf=(h1−h2)+(α1v122g−α2v222g)−he,he=ke∣α1v122g−α2v222g∣h_f=(h_1-h_2)+\left(\frac{\alpha_1v_1^2}{2g}-\frac{\alpha_2v_2^2}{2g}\right)-h_e,\qquad h_e=k_e\left|\frac{\alpha_1v_1^2}{2g}-\frac{\alpha_2v_2^2}{2g}\right|

Here v2<v1v_2<v_1 (expansion), so he=0.3(hv1−hv2)h_e = 0.3(h_{v1}-h_{v2}).

TrialQQ assumedv1v_1v2v_2α1v12/2g\alpha_1 v_1^2/2gα2v22/2g\alpha_2 v_2^2/2gheh_ehfh_fQ=Kmhf/LQ=K_m\sqrt{h_f/L}
143.7860.59740.46880.018190.011200.002100.2748944.181
244.1810.60270.47300.018520.011400.002130.2749844.188
344.1880.60280.47310.018520.011410.002130.2749844.188

The trials converge to hfh_f and QQ shown in the last row.

Answer: Discharge Q≈44.2 m3/sQ \approx 44.2\ \text{m}^3/\text{s}.

✓ Answer checked by Claude Sonnet 5.5

All Engineering Hydrology chapter 4 questions →