Bernoulli's Equation (Two Points)

Also known as bernoulli principle · energy equation · pressure head velocity head elevation head · total head · frictionless flow

P1+12ρv12+ρgz1=P2+12ρv22+ρgz2P_1 + \tfrac{1}{2}\rho v_1^{2} + \rho g z_1 = P_2 + \tfrac{1}{2}\rho v_2^{2} + \rho g z_2

Worked example: Water accelerating 2 → 8 m/s in a horizontal pipe drops 30 kPa — press Try an example to run it live, then adjust anything.

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Bernoulli's Equation (Two Points) explained

P1v1P2v2ρz1z2

Daniel Bernoulli published this in 1738, and every one of its three terms is an energy per unit volume: static pressure, the kinetic term 12ρv2\tfrac{1}{2}\rho v^2, and the potential term ρgz\rho g z. Their sum is fixed along a streamline, so any one of them can only grow at another's expense. Push water from 2 m/s to 8 m/s in a level pipe and the pressure must fall by 12×1000×(64−4)=30 kPa\tfrac{1}{2}\times 1000 \times (64 - 4) = 30\ \text{kPa}, which is the entire working principle of a Venturi, a carburettor, a laboratory aspirator and an aircraft wing.

The famous field mistake is applying it where its assumptions have quietly died. Bernoulli assumes no friction, no pump, no heat and constant density. Real pipe runs bleed head to friction, so a designer writes the extended form with an hfh_f term on the downstream side and gets that number from Darcy-Weisbach. Gases obey it only while Mach number stays under about 0.3, above which density stops being constant and compressible relations take over.

Here is the part that catches people out: the equation holds along a streamline, not across a flow field, unless the flow is irrotational. Two points in the same pipe cross-section can carry genuinely different totals, which is why a pitot traverse across a duct reads a curve rather than a plateau. And note that velocity enters squared, so this page's velocity brains return the positive root only. If your flow actually runs from 2 back to 1, swap the two ends rather than expecting a negative answer.

Bernoulli's Equation (Two Points)

P1+12ρv12+ρgz1=P2+12ρv22+ρgz2P_1 + \tfrac{1}{2}\rho v_1^{2} + \rho g z_1 = P_2 + \tfrac{1}{2}\rho v_2^{2} + \rho g z_2
Where
  • P1P_1= Pressure at point 1 (kPa)
  • v1v_1= Velocity at point 1 (m/s)
  • z1z_1= Elevation at point 1 (m)
  • P2P_2= Pressure at point 2 (kPa)
  • v2v_2= Velocity at point 2 (m/s)
  • z2z_2= Elevation at point 2 (m)
  • ρ\rho= Fluid density (kg/m³)