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Discharge from depth and mean velocity data

Short answer

Mid-section method with strip widths determined from adjacent distances. Multiplying each strip width by depth and given mean velocity, then summing gives total discharge ≈ 232 m³/s.

At known distances from an initial point on the stream bank, the measured depth and velocity of a river are shown in table. Calculate the corresponding discharge at this location.

Distance from initial point (m)010203040506070809099
Depth (m)01.01.52.02.53.03.53.02.01.50
Mean velocity (m/s)00.60.81.01.21.41.61.31.00.50

Mean velocities are given directly, so the mid-section method is applied: each vertical represents a strip from halfway to the previous vertical to halfway to the next, wi=(xi+1−xi−1)/2w_i = (x_{i+1} - x_{i-1})/2, and ΔQi=widiVi\Delta Q_i = w_i d_i V_i.

Computation

x (m)Width (m)Depth (m)V (m/s)Area (m²)ΔQ (m³/s)
10101.00.610.006.000
20101.50.815.0012.000
30102.01.020.0020.000
40102.51.225.0030.000
50103.01.430.0042.000
60103.51.635.0056.000
70103.01.330.0039.000
80102.01.020.0020.000
90(99 − 80)/2 = 9.51.50.514.257.125
Total199.25232.125
Q=∑widiVi=232.1 m3/sQ = \sum w_i d_i V_i = 232.1\ \text{m}^3/\text{s}

Answer: Discharge ≈ 232 m³/s.

(By the mean-section method, averaging depth and velocity of adjacent verticals for each 10 m panel, Q=225.9Q = 225.9 m³/s; the mid-section result is normally reported.)

✓ Answer checked by Claude Opus 5.5 (high effort)

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