Skip to main content

Slope-area discharge, 1300 m reach

Short answer

With fall 0.4 m over 1300 m, geometric mean conveyance K_m=342,113, initial estimate 6001 m³/s. Iterative correction for velocity heads (no eddy loss) yields discharge 5754.8 m³/s.

Calculate the flood discharge of a stream by the slope area method given the following data:

Upstream flow area = 3500 m2^2 Upstream wetted perimeter = 650 m Upstream velocity head coefficient = 1.17 Downstream flow area = 3250 m2^2 Downstream wetted perimeter = 621 m Downstream velocity head coefficient = 1.21 Falling difference = 0.4 m Reach length = 1300 m Manning's coefficient n = 0.03

Given: A1=3500A_1=3500 m2^2, P1=650P_1=650 m, α1=1.17\alpha_1=1.17; A2=3250A_2=3250 m2^2, P2=621P_2=621 m, α2=1.21\alpha_2=1.21; fall =0.4=0.4 m, L=1300L=1300 m, n=0.03n=0.03. No eddy-loss coefficient is given, so he=0h_e=0 is assumed.

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=3500650=5.3846 m,R2=3250621=5.2335 mR_1=\frac{3500}{650}=5.3846\ \text{m},\qquad R_2=\frac{3250}{621}=5.2335\ \text{m} K1=10.03×3500×5.38462/3=358412.6,K2=10.03×3250×5.23352/3=326555.2K_1=\frac{1}{0.03}\times3500\times5.3846^{2/3}=358412.6,\qquad K_2=\frac{1}{0.03}\times3250\times5.2335^{2/3}=326555.2 Km=K1K2=342113.3K_m=\sqrt{K_1K_2}=342113.3

Step 2: First trial (no velocity head)

Sf=0.41300,Q1=KmSf=6001.064 m3/sS_f=\frac{0.4}{1300},\qquad Q_1=K_m\sqrt{S_f}=6001.064\ \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|

With he=0h_e=0: hf=0.4+(hv1−hv2)h_f = 0.4 + (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}
16001.0641.71461.84650.175310.210270.000000.365045732.829
25732.8291.63801.76390.159990.191890.000000.368105756.770
75754.8501.64421.77070.161220.193370.000000.367855754.850

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

Answer: Discharge Q≈5754.8 m3/sQ \approx 5754.8\ \text{m}^3/\text{s}.

(If a contraction loss of ke=0.1k_e=0.1 were included, QQ would be about 5732 m3^3/s, a change of 0.4 %.)

✓ Answer checked by Claude Sonnet 5.5

All Engineering Hydrology chapter 4 questions →