Calculate buoyant force, apparent weight, and whether an object floats or sinks using Archimedes' principle. Compare behavior across fluids.
Archimedes' principle states that an object submerged in a fluid experiences an upward buoyant force equal to the weight of the fluid it displaces. This fundamental principle governs whether objects float or sink and is the basis for ship design, submarine ballast systems, and density measurement techniques.
This calculator computes the buoyant force, apparent weight, and submersion fraction for any object-fluid combination. Enter the object and fluid densities along with the object volume, and the tool instantly determines whether the object floats or sinks, how much of it is submerged, and the net force acting on it.
A comparison table shows how the same object behaves across eight common fluids — from gasoline to mercury — providing an intuitive understanding of density-dependent buoyancy. Preset buttons let you explore classic scenarios like ice floating on water, steel sinking in water, or steel floating on mercury. Check the example with realistic values before reporting.
Understanding buoyancy is essential in naval architecture, offshore engineering, materials science, and even cooking (testing egg freshness). This calculator makes it easy to predict float/sink behavior and quantify the forces involved without manual computation.
The multi-fluid comparison table is especially useful for engineers selecting materials for underwater applications or students learning about density and fluid mechanics.
Buoyant force F_b = ρ_fluid × V_displaced × g. For floating objects, V_displaced = V_object × (ρ_object / ρ_fluid). Apparent weight = W_object − F_b. Object floats when ρ_object < ρ_fluid.
Result: Floats, 91.9% submerged, buoyant force = 1.123 N
Ice (917 kg/m³) in water (998 kg/m³): fraction submerged = 917/998 = 91.9%, which is why icebergs show about 8% above the waterline.
Legend says Archimedes discovered this principle while taking a bath, noticing the water level rose as he entered. He reportedly ran through the streets shouting "Eureka!" (I found it!). He used this insight to determine whether King Hiero II's crown was pure gold — by comparing its water displacement to that of an equal mass of gold.
Archimedes' principle is fundamental to ship design (hull displacement calculations), submarine operations (ballast tank engineering), hot air balloons (air buoyancy), hydrometers (measuring fluid density), and geological surveys (isostasy — how continents "float" on the mantle). Mining engineers use heavy liquids to separate minerals by density, directly applying Archimedes' principle.
A frequent misconception is that "heavy things sink." In reality, it is density (mass per unit volume) that determines buoyancy, not total mass. A massive aircraft carrier floats because its average density — including all the air inside — is less than seawater. Conversely, a tiny steel ball sinks because solid steel is denser than water.
It states that the upward buoyant force on an object submerged in a fluid equals the weight of the fluid displaced by the object. This explains why objects with lower density than the fluid float.
Ice has a density of about 917 kg/m³, less than water's 998 kg/m³. So ice displaces its own weight of water while only being about 92% submerged, leaving 8% above the surface.
Yes — steel (7,800 kg/m³) floats on mercury (13,546 kg/m³) because mercury is denser. A solid steel ball would float with about 58% submerged in mercury.
Apparent weight is the measured weight of an object while submerged in a fluid. It equals the true weight minus the buoyant force. This is why objects feel lighter in water.
Submarines adjust their average density by flooding or emptying ballast tanks with water. When the average density exceeds seawater density, it sinks; when less, it rises.
When object density exactly equals fluid density, buoyant force equals weight, and the object neither sinks nor rises. This is the principle behind SCUBA neutral buoyancy and fish swim bladders.