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Discharge in 20 km pipe between reservoirs

Short answer

Low velocity suggests laminar flow. Hagen-Poiseuille gives V=0.0301 m/s, Re=589 (<2000). Discharge Q = 9.44 × 10⁻⁶ m³/s (0.0094 L/s, 34 L/h).

A 2 cm diameter 20 km long pipeline connects two reservoirs filled with water open to the atmosphere. What is the discharge in the pipeline if the surface elevation difference of the reservoirs level is 5 m? νwater=1.02×10−6\nu_{water} = 1.02 \times 10^{-6} m²/s.

Data. D=0.02D = 0.02 m, L=20 000L = 20\,000 m, H=5H = 5 m, ν=1.02×10−6\nu = 1.02\times10^{-6} m²/s. The pipe is very long and thin, so the velocity will be small; try laminar flow first.

Laminar flow assumption

The available head is used up in friction (velocity head and minor losses are negligible against 5 m over 20 km). Hagen-Poiseuille:

hf=32νLVgD2=H  ⇒  V=gD2H32νL=9.81(0.02)2(5)32(1.02×10−6)(20 000)=0.0301 m/sh_f = \frac{32\nu LV}{gD^2} = H \;\Rightarrow\; V = \frac{gD^2H}{32\nu L} = \frac{9.81(0.02)^2(5)}{32(1.02\times10^{-6})(20\,000)} = 0.0301\ \text{m/s}

Check

Re=VDν=0.0301(0.02)1.02×10−6=589<2000Re = \frac{VD}{\nu} = \frac{0.0301(0.02)}{1.02\times10^{-6}} = 589 < 2000

The flow is laminar, so the assumption is right. (Velocity head V2/2g=4.6×10−5V^2/2g = 4.6\times10^{-5} m is negligible against 5 m.)

Discharge

Q=π4D2V=π4(0.02)2(0.0301)=0.0000094 m3/s=0.00944 l/s≈34.0 l/hourQ = \frac{\pi}{4}D^2V = \frac{\pi}{4}(0.02)^2(0.0301) = 0.0000094\ \text{m}^3/\text{s} = 0.00944\ \text{l/s} \approx 34.0\ \text{l/hour}

Answer: Q≈9.44×10−6Q \approx 9.44\times10^{-6} m³/s (about 0.0094 l/s, 34 l/h); laminar flow with Re≈589Re \approx 589.

✓ Answer checked by Claude Opus 5.5 (high effort)

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