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Gas pipeline flow capacity

Gas flow rate from the inlet and outlet pressures — the general isothermal flow equation with the Colebrook-White friction factor; gas velocity, average pressure, Reynolds number.

Formula
Q_st = (π · d² / 4) · (T_st / P_st) · √[(P₁² − P₂²) · d · R / (λ · L · Z · T · M)]M = 28.96 · γ_g g/mol; Re = 4 · ṁ / (π · d · μ); λ: Colebrook-WhiteP_avg = (2/3) · (P₁ + P₂ − P₁ · P₂ / (P₁ + P₂))

Steady isothermal flow on a horizontal line; the kinetic energy change is neglected (negligible for sections longer than about 1 km). Z and T are section averages. Elevation matters for gas only in hilly terrain. With liquids in the gas (associated gas with condensate and water) the capacity is overstated.

Source: General flow equation (Menon E.S., Gas Pipeline Hydraulics, 2005); Colebrook-White formula

Inputs

You can change a field's unit: the value is converted to the formula's units automatically.

P₁

For gauge pressure choose the MPa(g) unit; it is converted automatically.

P₂
D
t
L
γ_g

Dry gas 0.56–0.65, associated gas 0.7–1.0.

T
Z

At the average pressure P_avg (see the results) and average temperature.

μ

Natural gas 0.011–0.014 mPa·s.

ε

New pipe 0.02–0.05 mm, internally coated about 0.01 mm.

Unit converter for this formulaPressure · Length · Temperature · Viscosity · Gas rate · Velocity
Metric
  • MPa1
  • kPa1,000
  • bar10
  • atm9.86923
  • kgf/cm²10.1972
  • mmHg7,500.62
  • MPa(g)0.898675
  • barg8.98675
US field units
  • psi145.038
  • psia145.038
  • psig130.342
  • ksi0.145038

psi and psia are absolute pressure; gauge units (barg, MPa(g), psig) are above atmospheric (101.325 kPa = 14.696 psi). Pressure differences in the formulas do not depend on this.

All units
Result
Q_stGas flow rate at standard conditions
Fill in all fields
  • v₂Gas velocity at the outlet
  • P_avgAverage pressure in the section
  • ReReynolds number
  • λDarcy friction factor

More in Pipelines

Results are engineering estimates from standard formulas; for design decisions check them against the codes, project documents and specialists' calculations. The formulas carried over from the original set are unchanged, and their errors are described in the notes.