Pressure Calculator
Calculate pressure from force and area or find hydrostatic pressure from fluid density, depth, and gravity.
About pressure calculations
Pressure calculation examples
These examples compare concentrated force with pressure created by a static fluid column.
| Known values | Pressure | Explanation |
|---|---|---|
| 1000 N over 0.01 m² | 100000 Pa | Dividing force by area gives 100 kPa of average applied pressure. |
| Water at 10 m: ρ 1000 kg/m³, g 9.80665 m/s² | 98066.5 Pa | This is hydrostatic gauge pressure and excludes pressure at the surface. |
| Oil at 5 m: ρ 850 kg/m³, g 9.80665 m/s² | 41678.26 Pa | The lower-density liquid produces less pressure than water at the same depth. |
How to use the pressure calculator
- Choose Force and Area for applied pressure or Fluid Density and Depth for hydrostatic pressure.
- Convert each known quantity to the SI unit shown in its field label.
- Enter positive values and adjust gravitational acceleration when the fluid is not under standard Earth gravity.
- Select Calculate Pressure and interpret the result in pascals.
Pressure calculator FAQ
What is the difference between pressure and force?
Force is a push or pull measured in newtons, while pressure is force distributed over area. The same force creates different pressures when the contact area changes.
Does hydrostatic pressure include atmospheric pressure?
The ρgh result is pressure relative to the fluid surface, so it is gauge pressure. Add the pressure acting on the surface when absolute pressure is required.
Why does fluid pressure depend on vertical depth?
Hydrostatic pressure comes from the weight of fluid above the measurement point. Horizontal position and container shape do not change the ideal pressure at equal vertical depth.
Can this calculator output psi or bar?
The calculator reports pascals to keep inputs and output in a coherent SI system. Divide pascals by 6894.76 for psi or by 100000 for bar.
Can I use the fluid formula for air?
The formula can approximate small air columns when density is nearly constant. For large altitude changes, air compressibility makes density variable and a barometric model is more appropriate.