Calculating Buoyant Force- Archimedes' Principle Explained

What Is Buoyant Force, Anyway?

Buoyant force is the upward push a fluid exerts on any object placed in it. It's why a steel boat floats despite steel being heavier than water. It's also why you feel lighter when you're submerged in a pool.

The concept is simple: fluids push back. Gravity pulls everything down, but the pressure difference between the top and bottom of an object creates an upward force. That force is buoyant force.

If you're trying to figure out whether something will float, you need to calculate this force. That's where Archimedes' Principle comes in.

Archimedes' Principle: The Core Idea

Archimedes' Principle states that the buoyant force on an object equals the weight of the fluid it displaces. Not the weight of the object itself—the weight of the displaced fluid.

This is the whole game right here. An object floats when the buoyant force equals its weight. It sinks when its weight exceeds the buoyant force. That's the entire mechanism.

Archimedes supposedly discovered this while taking a bath. The story goes he ran through the streets shouting "Eureka!" Whether that actually happened is debatable. What matters is the principle itself.

The Buoyant Force Formula

The equation is:

Fb = ρ × V × g

Where:

That's it. Three variables, one multiplication operation. You don't need calculus. You don't need a physics degree. Just plug in the numbers.

Density of Common Fluids

Fluid Density (kg/m³) Notes
Fresh Water 1,000 Standard reference
Salt Water 1,025 About 2.5% denser
Oil (typical) 800–950 Varies by type
Mercury 13,600 Extremely dense metal
Air 1.225 At sea level, 15°C

Step-by-Step: How to Calculate Buoyant Force

Step 1: Identify Your Fluid

What are you submerging the object in? Fresh water, salt water, oil, something else? The density of your fluid is your ρ value.

Step 2: Find the Volume Displaced

Measure the volume of the part of the object that's underwater. For a fully submerged object, this is just the object's total volume. For a floating object, it's the volume below the waterline.

Units matter here. Convert everything to before calculating. A common mistake is mixing units—centimeters and meters in the same problem.

Step 3: Plug Into the Formula

Multiply density × volume × gravity. That's your buoyant force in Newtons.

Step 4: Compare to the Object's Weight

Weight = mass × g. If the buoyant force is greater than the weight, the object rises. If the buoyant force is less, it sinks. If they're equal, the object stays suspended.

Practical Example

Let's say you have a 10 kg solid steel block with a volume of 0.00127 m³ (that's about 0.127 liters or roughly a 10cm cube).

Submerged in fresh water:

Fb = 1,000 × 0.00127 × 9.81 = 12.46 N

The block's weight:

W = 10 × 9.81 = 98.1 N

The buoyant force (12.46 N) is far less than the weight (98.1 N). This block sinks. No surprise there.

Now let's take a hollow steel cube of the same external dimensions but with air inside, so its effective density is much lower. If the mass is only 2 kg:

W = 2 × 9.81 = 19.62 N

The buoyant force is still 12.46 N. Now the object is lighter, but the buoyant force is still greater than the weight. It would rise. It would also float if shaped correctly to displace enough water.

Why Ships Float and Steel Balls Sink

People struggle with this. Steel is denser than water—every physics student knows this. So how does a steel ship float?

The ship isn't solid steel. It's a hollow shell with air inside. The overall density of the ship (steel + air + cargo + everything) is less than water. The ship floats because it displaces a volume of water that weighs more than the entire ship.

A solid steel sphere the size of a basketball? Sinks immediately. The same amount of steel shaped into a bowl? Floats. The difference is volume displaced.

This is why ships have draft markings. The deeper a ship sits in the water, the more weight it's carrying. Captains read the waterline to know when they're overloaded.

The Role of Fluid Density

The same object floats higher in salt water than fresh water. Salt water is denser—about 2.5% more dense than fresh water. That extra density means more buoyant force per unit volume displaced.

This is why you feel slightly lighter in the ocean than in a swimming pool. It's also why boats sitting in fresh water have a lower maximum load than the same boat in salt water.

The Dead Sea takes this further. Its salinity is around 340 g/kg, compared to the ocean's 35 g/kg. Objects float much higher there. Some people literally cannot sink in the Dead Sea.

Getting Started: Quick Calculation Checklist

Common Mistakes to Avoid

Using the object's density instead of the fluid's. Buoyant force depends on the fluid's density, not the object's. A hollow object with low average density floats even if its shell material is heavy.

Forgetting to convert units. If your volume is in cubic centimeters, convert to cubic meters first. Divide by 1,000,000.

Assuming partial submersion is complicated. It's not. Just use the volume that's actually underwater. The formula doesn't care if the object is halfway in.

Ignoring atmospheric pressure effects. For most practical purposes at normal scales, you ignore atmospheric pressure. But for very precise calculations or extreme altitudes, air has weight and affects the net buoyant force.

Real-World Applications

Archimedes' Principle shows up everywhere:

When Buoyant Force Calculations Get Complex

For simple shapes—spheres, cubes, cylinders—you can calculate displaced volume with basic geometry. For irregular objects, you need to measure displaced volume directly or use 3D modeling.

Compressible fluids add another layer. Gases change density significantly with pressure and temperature. Hot air balloons work because heated air expands, becoming less dense per unit volume. The buoyant force comes from the density difference between the inside and outside air.

Fluids in motion—rivers, ocean currents, wind—are a different problem entirely. Archimedes' Principle assumes static equilibrium. Moving fluids introduce drag, lift, and turbulence that basic buoyant force calculations don't account for.

The Bottom Line

Archimedes' Principle gives you a straightforward way to calculate upward fluid force. Fb = ρVg. Density, volume, gravity. Multiply them together.

The principle explains why some objects float and others sink, why steel ships work, and why you weigh less in a pool. It's one of the more practical concepts in physics—useful in engineering, navigation, and basic problem-solving.

You don't need to memorize the "Eureka" story. You need to remember the formula and understand that buoyant force equals the weight of displaced fluid, not the weight of the object itself. That's the part people consistently get wrong.