Bernoulli Equation Calculator
Calculate pressure, velocity, or height at two points in a fluid flow using Bernoulli's equation. The principle states that P + ½ρv² + ρgh remains constant along a streamline for ideal fluid flow.
Bernoulli's equation expresses the conservation of energy for an ideal flowing fluid: along any streamline, the sum of pressure energy, kinetic energy, and potential energy per unit volume stays constant. This single relationship explains an enormous range of phenomena — why airplanes generate lift, why a shower curtain pulls inward when you turn on the water, how a Venturi meter measures flow, why a fast-moving stream of water creates low pressure at its sides.
The classical form is P + ½ρv² + ρgh = constant. As fluid speeds up, its pressure must drop (kinetic up, pressure down). As it climbs, pressure also drops (potential up, pressure down). This trade-off, applied at two points along a streamline, lets you solve for any unknown if you know the others.
Bernoulli's equation assumes ideal conditions: steady (not time-varying), incompressible (constant density), inviscid (no friction), and irrotational flow along a single streamline. Real fluids violate these assumptions to varying degrees — water in a smooth pipe is close to ideal; air at supersonic speeds, viscous oil, or highly turbulent flow needs corrections.
Common applications: aerodynamics (wing lift), pipe flow design, Venturi flowmeters, pitot tubes (measuring aircraft airspeed), spray systems, chimney draft, and countless introductory fluid-mechanics problems.
Inputs
Results
Pressure at Point 2
61,395 Pa
Total Pressure
103,325 Pa
Dynamic P₂
12500.0 Pa
Bernoulli Equation Results
| Parameter | Value |
|---|---|
| Fluid Density | 1000 kg/m³ |
| Point 1: Static Pressure | 101,325 Pa |
| Point 1: Dynamic Pressure | 2000.00 Pa |
| Point 1: Hydrostatic (ρgh) | 0.00 Pa |
| Total Pressure (constant) | 103,325 Pa |
| Point 2: Dynamic Pressure | 12500.00 Pa |
| Point 2: Hydrostatic (ρgh) | 29430.00 Pa |
| Point 2: Static Pressure | 61,395 Pa |
| Pressure Difference | 39,930 Pa |
| Formula | P + ½ρv² + ρgh = constant |
Formula
How to use this calculator
- Enter fluid density (1000 for water, 1.225 for air at sea level).
- Enter pressure, velocity, and height at point 1 (upstream).
- Enter velocity and height at point 2 (downstream).
- Calculator solves for pressure at point 2.
- Use SI units throughout to avoid conversion errors.
- Remember: assumes steady, incompressible, inviscid flow.
Worked examples
Garden hose nozzle
**Scenario:** Water in a hose at 300 kPa flows at 2 m/s through a wider section, then accelerates to 10 m/s through a narrower nozzle. Same elevation. **Calculation:** Δ(½ρv²) = 0.5 × 1000 × (100 − 4) = 48,000 Pa. P₂ = 300,000 − 48,000 = 252,000 Pa. **Result:** Pressure drops by 48 kPa as water speeds up. This is why fluid speeds up exiting a nozzle — pressure energy converts to kinetic energy. The pressure at the nozzle tip is still 152% of atmospheric, then drops to atmospheric as the jet leaves.
Airplane wing (qualitative)
**Scenario:** Air flows over a wing at 100 m/s on top, 80 m/s on bottom. Air density 1.0 kg/m³ at altitude. **Calculation:** ΔP = ½ρ(v_bottom² − v_top²) = 0.5 × 1.0 × (6400 − 10000) = −1,800 Pa. **Result:** Pressure on the wing's top is 1,800 Pa lower than on the bottom. For a wing area of 30 m², that's ~54,000 N of lift — roughly 5.5 tonnes. (Real aerodynamics involves circulation theory and viscous effects, but Bernoulli gives the intuition.)
Water tank drain
**Scenario:** Tank with water level 4 m above a small drain hole. How fast does water exit? **Calculation:** Torricelli's law: v = √(2gh) = √(2 × 9.81 × 4) = √78.48 ≈ 8.86 m/s. **Result:** Water exits at ≈8.86 m/s (≈20 mph). Same speed as if dropped from 4 m. Real-world losses (sharp edges, viscous effects) reduce this by ~15% — actual flow ≈7.5 m/s.
When to use this calculator
**Use Bernoulli's equation for:**
- **Pipe flow problems**: pressure-velocity-height relationships. - **Aerodynamics**: wing lift (qualitatively), airflow over surfaces. - **Flow measurement**: Venturi meters, pitot tubes, orifice plates. - **Tank drainage**: Torricelli's law for outflow speed. - **Spray systems**: atomizers, carburetors, paint sprayers. - **Chimney draft**: hot rising air pressure relationships. - **Stream/river hydraulics**: velocity-depth-pressure trade-offs.
**Critical assumptions and when they fail:**
- **Steady flow**: variables don't change with time. Pulsating systems (heart, reciprocating pumps) violate this. - **Incompressible**: density constant. Air at Mach < 0.3 OK; supersonic flow needs gas dynamics. - **Inviscid**: no friction. Long pipes need Darcy-Weisbach friction correction. - **Along a streamline**: holds for each streamline individually; vortices break this. - **Irrotational**: no swirling; turbulent flow violates this.
**Real-world corrections:**
**Extended Bernoulli (engineering form):**
P₁/ρg + v₁²/(2g) + h₁ = P₂/ρg + v₂²/(2g) + h₂ + h_L
Where h_L = head loss from friction, fittings, etc. Use Darcy-Weisbach or empirical loss coefficients.
**Common applications:**
- **HVAC design**: duct sizing and pressure drops. - **Plumbing**: water pressure at different elevations. - **Aircraft**: pitot-static system measures airspeed and altitude. - **Oil & gas**: pipeline pressure drops. - **Hydroelectric**: head difference drives turbines. - **Sports**: curveball physics, golf ball dimples (modified by viscous effects).
**Software:**
- **CFD (ANSYS Fluent, OpenFOAM)**: full Navier-Stokes for real flows. - **EPANET**: water distribution network analysis. - **Spreadsheets**: Bernoulli + Darcy-Weisbach for design calcs.
**Common pitfalls:**
- **Applying across pumps or turbines**: Bernoulli doesn't account for energy added/removed; use energy equation. - **Forgetting elevation changes**: in tall buildings, ρgh dominates. - **Mixing absolute and gauge pressures**: be consistent. - **Using on viscous flow**: long pipe = significant head loss. - **Compressibility**: high-speed gas needs gas dynamics equations. - **Across streamlines**: stagnation pressure ≠ static pressure in rotational flow.
**Bernoulli for gases (low speed):**
Works for air at Mach < 0.3 (about 100 m/s at sea level). Above that, compressibility matters and you need compressible Bernoulli or full gas dynamics.
**Beyond Bernoulli:**
- **Navier-Stokes equations**: full fluid dynamics with viscosity. - **Euler equations**: inviscid compressible flow. - **Reynolds-averaged Navier-Stokes (RANS)**: turbulent flow modeling. - **Direct numerical simulation (DNS)**: research-level accuracy.
Common mistakes to avoid
- Applying Bernoulli across streamlines where rotational flow exists.
- Forgetting that the equation requires steady, incompressible, inviscid flow.
- Mixing gauge and absolute pressures.
- Using on compressible flow at high Mach number (M > 0.3).
- Ignoring head losses in long pipes (use extended Bernoulli with friction).
- Applying across a pump or turbine (energy is added/removed there).
- Forgetting unit consistency (mixing Pa with kPa, or m with cm).
- Treating dynamic pressure as static pressure.