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Slope-area discharge, 10 km reach, 104.77 m

Short answer

Conveyances K₁=7163.5, K₂=9902.5, Kₘ=8424.4; starting with fall 0.27 m over 10 km, then iterating with velocity head and expansion loss (ke=0.3) gives discharge Q ≈ 44.2 m³/s.

Calculate the discharge of a stream having high water surface elevations noted at two sections A and B, 10 km apart. These elevations and other salient hydraulic properties are given below.

SectionWater surface elevation (m)Area of x-section (m2^2)Hydraulic radius (m)
A104.7773.2932.733
B104.50093.3753.089

The eddy loss coefficient is 0.3 for gradual expansion, 0.1 for gradual contraction and Manning's roughness is 0.02.

Given: AA=73.293A_A=73.293 m2^2, RA=2.733R_A=2.733 m, AB=93.375A_B=93.375 m2^2, RB=3.089R_B=3.089 m, n=0.02n=0.02, L=10L=10 km, fall =104.77−104.50=0.27=104.77-104.50=0.27 m. Velocity-head coefficients are taken as 1. Section B has the larger area, so the reach expands and ke=0.3k_e=0.3. The wetted perimeter is found from P=A/RP=A/R (PA=26.82P_A=26.82 m, PB=30.23P_B=30.23 m).

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=73.29326.8178=2.7330 m,R2=93.37530.2282=3.0890 mR_1=\frac{73.293}{26.8178}=2.7330\ \text{m},\qquad R_2=\frac{93.375}{30.2282}=3.0890\ \text{m} K1=10.02×73.293×2.73302/3=7163.5,K2=10.02×93.375×3.08902/3=9902.5K_1=\frac{1}{0.02}\times73.293\times2.7330^{2/3}=7163.5,\qquad K_2=\frac{1}{0.02}\times93.375\times3.0890^{2/3}=9902.5 Km=K1K2=8422.4K_m=\sqrt{K_1K_2}=8422.4

Step 2: First trial (no velocity head)

Sf=0.2710000,Q1=KmSf=43.764 m3/sS_f=\frac{0.27}{10000},\qquad Q_1=K_m\sqrt{S_f}=43.764\ \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 vB<vAv_B<v_A (expansion), so he=0.3(hvA−hvB)h_e = 0.3(h_{vA}-h_{vB}).

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}
143.7640.59710.46870.018170.011200.002090.2748844.158
244.1580.60250.47290.018500.011400.002130.2749744.165
344.1650.60260.47300.018510.011400.002130.2749744.165

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

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