Calcylator
Fluid hydrostatic pressure

Fluid hydrostatic pressure:
formula and worked example

Pressure in a still liquid depends only on how deep you are, how dense the liquid is and the local gravity, not on the container's width.

Calcylator Editorial Team

Updated · 5 min read

What hydrostatic pressure is

Hydrostatic pressure is the pressure that a fluid at rest exerts because of its own weight. At any point, it equals the weight of the column of fluid above that point per unit area. That is why your ears feel it in a swimming pool, why dams are thicker at the base, and why water towers deliver pressure to taps through gravity alone.

The key feature is simplicity. The shape of the container, its width and the total volume of liquid do not matter. A narrow tube 4 m deep and a lake 4 m deep give the same value at the bottom.

Inputs, units and what gets left out

Fluid hydrostatic pressure =density × gravity × depth
density:
Density
gravity:
Gravity
depth:
Depth
Density in kg/m³, gravity in m/s² and depth in m give gauge pressure in pascals. Atmospheric pressure is not included.
  • Density: mass per cubic metre of the fluid. Fresh water is about 1,000 kg/m³, and denser liquids such as seawater are a little higher.
  • Gravity: 9.81 m/s² near Earth's surface, slightly different at other places.
  • Depth: the vertical distance below the free surface in metres, not the distance along a slope or pipe.

The result is in pascals, where one pascal is one newton per square metre. Multiplying kg/m³ by m/s² by m gives N/m², so no conversion is needed when you use SI units.

This is gauge pressure, the part caused by the fluid. The air above the surface adds roughly 101 kPa at sea level, and a sealed gauge that reads relative to the atmosphere will not show it.

Pressure at 4 m below the surface of water

  • Density

    1,000

  • Gravity

    9.81

  • Depth

    4

Fluid hydrostatic pressure

39,240 Pa

At 4 m depth in water of 1,000 kg/m³, the added pressure is 39,240 Pa, about 39.2 kPa. This is gauge pressure; add atmospheric pressure for absolute.

  1. Multiply density by gravity: 1,000 × 9.81 = 9,810 Pa per metre.
  2. Multiply by depth: 9,810 × 4 = 39,240 Pa.
  3. Express in kilopascals: 39,240 ÷ 1,000 = 39.24 kPa.
  4. Add atmospheric pressure of about 101,325 Pa if absolute pressure is needed, giving roughly 140,565 Pa.

Step one is a handy figure to remember: fresh water adds about 9.8 kPa for each metre of depth, so every 10 m adds close to 98 kPa, nearly one atmosphere.

Making sense of the pressure value

Pressure acts equally in all directions at a given depth, so it pushes sideways on a tank wall and upwards on a submerged object, not just downwards. Force on a surface is pressure times area, so 39,240 Pa on a hatch of 0.5 m² gives about 19,620 N.

  • Linear growth: double the depth, double the gauge pressure.
  • Fluid choice: a denser liquid gives proportionally higher pressure at the same depth.
  • Gauge or absolute: pumps and tyres usually quote gauge; gas laws need absolute.

The force on a sloping or vertical wall is not uniform. It rises with depth, so the load is greater near the bottom, and for dams and tank walls the average pressure, taken at mid-depth, is what you multiply by area.

What a heavier fluid does to the result

Effect of a denser fluid on hydrostatic pressure at 4 m depth
ScenarioDensityCalculated result
Original assumptions1,00039,240 Pa
Density increased by 10%1,10043,164 Pa

With density 10% higher, from 1,000 to 1,100 kg/m³, the pressure at 4 m rises from 39,240 to 43,164 Pa, an increase of exactly 10%. The dependence is linear in every input.

This is useful when comparing liquids in a tank design. A brine or syrup at 1,100 kg/m³ puts about 10% more load on the same wall than plain water at the same level.

Errors that creep into pressure calculations

  • Measuring depth along a slanted pipe instead of vertically from the free surface.
  • Using grams per cubic centimetre or litres without converting to kg/m³.
  • Adding or omitting atmospheric pressure inconsistently when comparing with a gauge reading.
  • Assuming a larger container means more pressure at the same depth.

A checklist for tanks, pools and dams

  1. Find the vertical depth from the free surface to the point of interest.
  2. Confirm the fluid and use its density at the working temperature.
  3. Decide whether the answer should be gauge or absolute.
  4. Multiply by the area, using mid-depth pressure for vertical walls, to get force.

Because pressure scales steadily with depth, a quick mental estimate of 10 kPa per metre for water is usually good enough to see if a design is in the right range before running the full numbers.

Common questions

Does the shape of the container affect hydrostatic pressure?

No. At a given depth the pressure depends only on fluid density, gravity and vertical depth. A narrow vessel and a large reservoir of the same depth produce the same pressure at the bottom.

What is the difference between gauge and absolute pressure?

Gauge pressure is measured relative to the surrounding atmosphere, while absolute pressure includes atmospheric pressure too. The formula here yields gauge pressure; add about 101 kPa at sea level to get the absolute value.

How much does pressure increase per metre of water?

Roughly 9.8 kPa per metre for fresh water, so about 98 kPa per 10 m. That is close to one extra atmosphere for every 10 m of depth.

Is gravity always 9.81 m/s²?

It is a standard value near the Earth's surface. It varies slightly with latitude and altitude, but for tank and pool work the difference is negligible. Use 9.81 unless you have a reason not to.

Why is the pressure the same in all directions at a given depth?

In a fluid at rest, molecules transmit pressure equally to every direction. This is why the same depth-based value pushes on side walls, on the base and on an object's top and bottom surfaces.

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