Example 1
ρ = 1000 kg/m³, h = 10 m, blank g → p ≈ 98 kPa.
Type density ρ and depth h. The calculator computes p = ρ g h. 1000 kg/m³ and 10 m of water is about 98 kPa. Empty g = 9.81.
Buoyancy of that fluid: F = ρ V g. Density: ρ = m/V.
Density ρ (kg/m³), Depth h (m) and g (m/s², optional). The result shows up here.
p = ρ g h grows with depth. Water 1000 kg/m³ and h = 10 m: p = 98,100 Pa, about 98 kPa. At 2 m that is 19,620 Pa ≈ 19.6 kPa. At 5 m about 49 kPa. At 30 m about 294 kPa. At 50 m about 491 kPa. Seawater 1025 kg/m³ and 100 m give about 1.01 MPa. Oil 900 kg/m³ and 3 m give about 26.5 kPa.
That is the fluid-column pressure, above atmosphere at the surface if you count the column alone. For absolute p, add about 101 kPa from outside. A barometer scale: ρ ≈ 13,550 kg/m³ and h = 0.76 m give about 101 kPa, the order of one atmosphere. The calculator does not add atmosphere on its own.
Fields: ρ in kg/m³, h in meters, empty g = 9.81. Result in pascals, 1 Pa = 1 N/m². A comma and a period are the same h: 2,5 and 2.5. Typed 0 in ρ or h gives p = 0. ρ and h both need a number before 98 kPa can appear.
Buoyancy F = ρ V g is on the neighbouring page: a force in newtons from volume, not pressure from depth. A liter of water is still 9.81 N of buoyancy, whether or not p at 10 m is 98 kPa. Mechanical p = F/S is on the force-and-area pressure page.
ρ = m/V is on the density page when the problem gives mass and volume of the fluid. Here ρ is an input. The model is hydrostatic, no flow and no waves.
Type 1000 and 10, click Calculate, and match about 98 kPa. Then 2 m and see 19.6 kPa. The header symbol does not dive.
p = ρ · g · h
Default g = 9.81 m/s2. Unit: Pa = N/m2.
Hydrostatic pressure here is p = ρ g h. Depth h from the free surface, not from the tank floor. 1000 kg/m³ at 1 m and 9.81 is 9810 Pa.
ρ = 1000 kg/m³, h = 10 m, blank g → p ≈ 98 kPa.
h = 2 m in water.
h = 30 m, water.
ρ ≈ 1025 kg/m³, h = 100 m.
h = 5 m, typed g.
ρ ≈ 13550 kg/m³, h = 0.76 m (barometer scale).
ρ = 900 kg/m³, h = 3 m.
h = 50 m at the base.
h = 0.4 m.
Same water, h = 10 m, g = 1.62.
p = 1000 × 9.81 × 10 = 98,100 Pa ≈ 98 kPa. At 2 m that is about 19.6 kPa.
Buoyancy is F = ρ V g in newtons. Here p is in pascals from depth. A liter of water is still 9.81 N.
ρ in kg/m³, h in meters, g in m/s². Result in Pa. 1000 Pa = 1 kPa.
Empty g = 9.81 m/s². Type g when the problem leaves Earth.
The calculator computes ρ g h, the column alone. For absolute p, add about 101 kPa from outside.
p ≈ 1.01 MPa. For oil 900 kg/m³ and 3 m, about 26.5 kPa.
p ≈ 101 kPa, the order of one atmosphere on a barometer scale.
Yes. 2,5 and 2.5 mean the same h [m]. Pressure is ρ g h at that depth.
On the pressure page from force and area. Here density and depth, not F and S.
On the density page. Here ρ is an input, then p = ρ g h.
The formula is the school one. Units follow SI; NIST SP 330 and BIPM define the measures, not your result.
Page updated in 2026.