Bernoulli Equation Calculator
Solve downstream pressure from fluid velocity, elevation, density, and inlet pressure.
About the Bernoulli Equation
Bernoulli Equation Examples
Ideal-flow examples showing how velocity and elevation affect pressure.
| Flow Conditions | Point 2 Pressure | Interpretation |
|---|---|---|
| P1 101325 Pa, v1 2 m/s, z1 10 m, v2 5 m/s, z2 5 m, water | 139,875 Pa | Elevation drop exceeds velocity-pressure loss |
| P1 200000 Pa, v1 4 m/s, z1 2 m, v2 2 m/s, z2 2 m, water | 206,000 Pa | Slower flow raises static pressure |
| P1 150000 Pa, v1 3 m/s, z1 0 m, v2 3 m/s, z2 4 m, water | 110,760 Pa | Elevation gain lowers static pressure |
How to Use the Bernoulli Calculator
- Enter pressure, velocity, and elevation at the known upstream point.
- Enter velocity and elevation at the downstream point.
- Enter the fluid density using units consistent with the SI inputs.
- Calculate and review the downstream pressure and pressure-head values.
- Add pump, turbine, and loss terms separately when the ideal assumptions do not apply.
Bernoulli Equation FAQ
What does Bernoulli's equation calculate?
It relates pressure, flow velocity, and elevation through conservation of mechanical energy. This version solves the unknown pressure at a second point.
Can I use gauge pressure?
Yes, gauge pressure works when both pressure values use the same atmospheric reference. Do not combine an absolute input with a gauge result.
Does this calculator include pipe friction?
No, it represents ideal flow without energy loss. Real pipe calculations should add Darcy-Weisbach and fitting losses to the energy equation.
Can Bernoulli's equation be used for gases?
It can approximate low-speed gas flow when density changes are negligible. Compressible-flow equations are more appropriate when pressure and density vary substantially.
Why can downstream pressure increase?
Pressure can rise when velocity decreases or the fluid moves to a lower elevation. The increase reflects conversion of kinetic or gravitational energy into static pressure.