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Hydrostatic Pressure Calculator (P = ρ·g·h)

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Hydrostatic pressure is the pressure exerted by a fluid at rest due to its weight: P = ρ · g · h, where ρ is the fluid density, g is gravitational acceleration, and h is the depth. Greater depth means greater pressure. It's essential in hydraulics, scuba diving, civil engineering, and meteorology.

Last reviewed: April 16, 2026 Verified by Hacé Cuentas Team Source: NIST — National Institute of Standards and Technology, Khan Academy — Science 100% private

When to use this calculator

  • Calculate water pressure at different depths.
  • Solve hydrostatics problems in physics.
  • Determine pressure in pipes and tanks.
  • Understand depth limits for scuba diving.
  • Calculate force on dams and retaining walls.

Real-world example: Pressure at the bottom of a 3 m swimming pool

  1. Given: depth = 3 m, fresh water density = 1,000 kg/m³, g = 9.81 m/s².
  2. Formula: P = ρ · g · h = 1,000 × 9.81 × 3.
  3. Result: P = 29,430 Pa = 0.29 bar ≈ 0.29 atm.
  4. Absolute pressure with atmosphere: 29,430 + 101,325 = 130,755 Pa ≈ 1.29 atm.
Result: At 3 m depth in a pool, gauge pressure is 0.29 atm (total ~1.29 atm with air).

How it works

1 min read

What Is Hydrostatic Pressure

Hydrostatic pressure is the pressure exerted by a fluid at rest due to its weight: P = ρ · g · h, where ρ is the fluid density (kg/m³), g is gravitational acceleration (9.81 m/s²), and h is the depth (m). Important: it does not depend on the shape of the container—only on depth.

Typical Fluid Densities

Fluidρ (kg/m³)
Air1,225
Vegetable Oil920
Fresh Water1,000
Seawater1,025
Milk1,030
Blood1,060
Honey1,420
Mercury13,600

Pressure vs. Depth Table (Fresh Water)

DepthPressure (Pa)BarAtm
1 m9,8100.0980.097
10 m98,1000.980.97
100 m981,0009.819.68
1,000 m9,810,00098.196.8

When to Use It and Common Mistakes

  • Absolute pressure = hydrostatic + atmospheric (101,325 Pa).

  • The hydrostatic paradox: a fish tank and a deep well with the same water height produce the same pressure at the bottom.

  • Does not apply to moving fluids: use Bernoulli's equation instead.

  • Key applications: submarines, dams, scuba diving. Every 10 m of water adds ~1 atm of pressure.
  • Frequently asked questions

    What is hydrostatic pressure?

    Hydrostatic pressure is the pressure exerted by a fluid at rest due to its weight. It increases linearly with depth: approximately every 10 meters of water adds 1 atmosphere of pressure.

    How deep can a diver safely go?

    Recreational scuba divers are typically limited to 40 meters (130 feet). At 30 meters (~4 atm), nitrogen narcosis becomes a serious concern, and decompression sickness becomes more likely.

    Why does pressure increase with depth in water?

    Water above you exerts weight, and that weight is distributed across the area below. The deeper you go, the more water is above you, creating greater cumulative pressure.

    Does the shape of a container affect water pressure at the bottom?

    No—this is the hydrostatic paradox. Pressure at the bottom depends only on depth and fluid density, not on the container's shape or total volume.

    What is 1 atmosphere in pascals?

    1 atm = 101,325 Pa = 1.01325 bar. This is standard air pressure at sea level.

    How much pressure is at 100 meters deep?

    At 100 meters in fresh water, the pressure is about 981,000 Pa or 9.68 atmospheres—far beyond safe recreational diving limits.

    What's the difference between gauge and absolute pressure?

    Gauge pressure is the pressure from the fluid alone (P = ρgh). Absolute pressure adds atmospheric pressure: P_absolute = P_gauge + 101,325 Pa.

    Can this formula work for gases?

    For short gas columns (like mercury in a barometer), yes. For tall columns, gas density changes with pressure, making calculations more complex.

    How much pressure is in the Mariana Trench?

    At about 11,000 meters deep, the Mariana Trench experiences roughly 1,100 atmospheres (~111 MPa)—more than 1,000 kg/cm².

    Sources and references