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Slope-area discharge with three sections

Short answer

With fall 0.35 m over 260 m, geometric mean conveyance K_m=5310.8. First Q=194.9 m³/s; after iterative correction for velocity heads and eddy loss (k_c=0.1), discharge converges to 185.2 m³/s.

For the purpose of discharge measurement in a stream by Slope-Area method the following data has been obtained.

U/S SectionMiddle SectionD/S Section
Area (m2^2)105.75102.6396.63
Wetted perimeter (m)64.2560.2058.00
Gauge reading (m)315.5-315.15
Manning's roughness0.0250.0270.029

Determine the stream discharge for length between U/S and D/S sections as 260 m assuming coefficient of contraction KcK_c as 0.1.

Given: reach length L=260L=260 m between the u/s and d/s sections; fall =315.50−315.15=0.35=315.50-315.15=0.35 m; contraction coefficient kc=0.1k_c=0.1 (area decreasing downstream); α=1\alpha=1. Roughness differs at each section (n=0.025,0.027,0.029n = 0.025, 0.027, 0.029).

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

With three sections of different roughness, the conveyance of each section is computed with its own nn:

SectionAA (m2^2)PP (m)RR (m)nnKK
U/S105.7564.251.6460.0255896.7
Middle102.6360.201.7050.0275424.5
D/S96.6358.001.6660.0294682.8

The mean conveyance of the reach is taken as the geometric mean of the three sections:

Km=(K1K2K3)1/3=5310.8K_m=(K_1K_2K_3)^{1/3}=5310.8

The middle section has no gauge reading, so the fall is that between the end sections, and the eddy loss is applied between the end sections.

Step 2: First trial (no velocity head)

Sf=0.35260,Q1=KmSf=194.853 m3/sS_f=\frac{0.35}{260},\qquad Q_1=K_m\sqrt{S_f}=194.853\ \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|

Velocity heads are taken at the u/s and d/s sections, and he=kc∣hv1−hv2∣h_e=k_c|h_{v1}-h_{v2}| with kc=0.1k_c = 0.1.

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}
1194.8531.84262.01650.173040.207250.003420.31237184.082
2184.0821.74071.90500.154440.184970.003050.31642185.269
6185.1541.75091.91610.156250.187130.003090.31603185.155

The trials converge to hfh_f and QQ shown in the last row (trials 3 to 5 are not shown).

Answer: Discharge Q≈185.2 m3/sQ \approx 185.2\ \text{m}^3/\text{s}.

✓ Answer checked by Claude Sonnet 5.5

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