Buoyancy is the upward force that an object experiences when it is submerged in a fluid (liquid or gas). This force is the result of pressure differences within the fluid, which are caused by the weight of the fluid itself. The concept of buoyancy is primarily explained by Archimedes' Principle, which states that an object immersed in a fluid experiences a buoyant force equal to the weight of the fluid displaced by the object.

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Buoyancy by Codex 0 Created 2026-09-28 Updated 2026-10-13
Buoyancy is the resultant upward force exerted by a resting fluid on an immersed body in a downward gravitational field. The fluid pushes inward, perpendicular to each part of the body's surface. Because hydrostatic pressure increases with depth, the upward push from below exceeds the downward push from above. Opposite horizontal forces cancel; buoyancy is the remaining vertical force. A sinking body still receives this upward support. [ref]
More precisely, pressure on a small surface of area with outward unit normal vector exerts
The minus sign says the force points into the body. On a cube, the top force points down, the bottom force points up, and the side forces cancel in pairs because opposite sides have the same pressure at each depth. This is a surface traction; gravity on the body itself is a separate body force. [ref]
For a computed example, stipulate resting water with constant mass density and uniform gravitational acceleration . A fully immersed cube has side , top depth and bottom depth . Each horizontal face has area , and its volume is . Its top and bottom gauge pressures are
The corresponding forces relative to the common surface pressure are downward and upward. Therefore the net buoyancy is
Using absolute pressures adds the same to both face forces, leaving their difference unchanged. Zero gauge pressure at the surface does not mean zero absolute pressure. Increasing both depths by the same amount also leaves buoyancy unchanged in this constant-mass density model.
Figure 1.
How a hydrostatic pressure difference supports an immersed cube
. Left: a fully immersed cube of side has its top at depth and bottom at . The inward pressure forces on its sides cancel; its horizontal faces have area . The displayed face forces use gauge pressure, whose common surface offset cancels in the net upward buoyancy. Right: gauge pressure increases linearly with depth, marking at the top and at the bottom. Details.
Archimedes' principle turns this calculation into a rule for bodies of any shape. It explains floating equilibrium and lets us infer an immersed body's volume from the difference between its force from gravity and the force needed to support it. In particular, buoyancy depends on the displaced volume and the surrounding mass density, whereas the body's own mass density decides how its force from gravity compares with that support.