Floatation

A massive steel ship floats, yet a small steel nail dropped in a bucket sinks straight to the bottom — same material, opposite fates. The difference has nothing to do with how heavy the object is and everything to do with how its mass is spread through space. Floatation is the special case of Archimedes' principle that governs bodies which are lighter, on average, than the liquid they sit in: instead of sinking, such a body settles with only part of its volume submerged, pushed up until the upthrust from that submerged part exactly balances its weight. This article builds the floatation relation from Archimedes' principle, applies it to ships, submarines, icebergs and balloons, and works through the numbers so you can calculate immersed fractions and unknown densities directly.

The core insight

A body floats with a fraction V1/V2V_1/V_2 of its volume submerged that exactly equals the ratio of its own density to the liquid's density, ρ1/ρ2\rho_1/\rho_2, because floating equilibrium requires the upthrust on the immersed part to balance the body's full weight.

The core idea

Why some bodies float instead of sinking. A body floats in a liquid when its average density is less than the density of the liquid. Such a body cannot remain fully submerged: if it were pushed entirely under, the upthrust on its whole volume would exceed its weight, and the net force would shove it back up. It keeps rising until only part of it stays below the surface — just enough that the upthrust from that immersed part alone matches the weight. This balance is floating equilibrium:

FB=WF_B = W

where: FBF_B is the upthrust (buoyant force) on the immersed part of the body, and WW is the total weight of the body.

Turning the balance into a density ratio. Let ρ1\rho_1 be the body's density, V2V_2 its total volume, ρ2\rho_2 the liquid's density, and V1V_1 the volume of the body that is submerged. The weight is ρ1V2g\rho_1 V_2 g, and the upthrust equals the weight of liquid displaced by the immersed part, ρ2V1g\rho_2 V_1 g. This ratio is worked out in full below as the node's main derivation.

Reading the ratio. The relation says the fraction of the body submerged equals the ratio of its density to the liquid's density — nothing more, nothing less. A body with density close to the liquid's floats almost fully submerged, riding low with only a sliver above the surface. A body much lighter than the liquid floats high, with most of its bulk poking out. Because the body is in equilibrium, FB=WF_B = W means its apparent weight is zero — a floating object placed on a hypothetical spring balance dipped in the liquid would read zero, since the liquid's upthrust already carries its entire weight.

Figure
A block floats in a liquid with part of its volume above the surface and part below, upthrust arrow pointing up and weight arrow pointing down of equal length
A floating block — upthrust equals weight liquid surface V2 − V1 above V1 immersed F_B (upthrust) W (weight) Equilibrium: F_B = W, so only part of the body needs to be submerged

Everyday applications. A ship is hollow, enclosing a large volume of air; its average density (steel plus cargo plus enclosed air, divided by the total outer volume) is less than water's, even though solid steel itself sinks. A submarine adjusts its average density with ballast tanks — filling them with water increases average density to submerge, emptying them lowers it to rise. An iceberg floats mostly submerged because ice is only slightly less dense than seawater, so a large fraction of its volume must stay underwater to displace enough water to balance its weight. A balloon filled with a gas lighter than air floats in air by the same density-ratio logic, treating air itself as the surrounding fluid.

Derivation AThe floatation relation, from Archimedes' principle

The goal is to show, starting only from the floating-equilibrium condition FB=WF_B = W and the definition of density, that the fraction of a floating body's volume that stays submerged equals the ratio of the body's density to the liquid's density — the single relation this whole topic rests on, needed for every floatation numerical.

Step 1. Write the weight of the body using its density. If the body has density ρ1\rho_1 and total volume V2V_2, its mass is ρ1V2\rho_1 V_2 and its weight is W=ρ1V2gW = \rho_1 V_2 g, where gg is the acceleration due to gravity.

Step 2. Write the upthrust using only the immersed part. By Archimedes' principle, the upthrust equals the weight of liquid displaced, and a floating body displaces liquid only with the part of it that is actually underwater. If V1V_1 is the immersed volume and ρ2\rho_2 the liquid's density, FB=ρ2V1gF_B = \rho_2 V_1 g.

Step 3. Apply the floating condition FB=WF_B = W. Substituting the two expressions gives ρ2V1g=ρ1V2g\rho_2 V_1 g = \rho_1 V_2 g. The gg on both sides cancels, leaving ρ2V1=ρ1V2\rho_2 V_1 = \rho_1 V_2.

Step 4. Rearrange into the density-ratio form. Dividing both sides by ρ2V2\rho_2 V_2 gives

ρ1ρ2=V1V2\frac{\rho_1}{\rho_2} = \frac{V_1}{V_2}

This is the floatation relation: the ratio of the body's density to the liquid's density equals the ratio of immersed volume to total volume, so the submerged fraction is fixed the moment the two densities are known.

Worked example

A block of wood has density 600 kg/m3600\ \text{kg/m}^3 and floats in water of density 1000 kg/m31000\ \text{kg/m}^3. What fraction of the block is above the surface, and if the block has total volume 5×10−3 m35 \times 10^{-3}\ \text{m}^3, what volume of it is submerged?

Step 1. Apply the floatation relation to find the submerged fraction. ρ1ρ2=V1V2=6001000=0.6\dfrac{\rho_1}{\rho_2} = \dfrac{V_1}{V_2} = \dfrac{600}{1000} = 0.6. So 60%60\% of the block's volume stays submerged.

Step 2. Find the fraction above the surface. Since the whole volume is either above or below the surface, the fraction above is 1−0.6=0.41 - 0.6 = 0.4, i.e. 40%40\% of the block floats above the water.

Step 3. Convert the submerged fraction into an actual volume using the given total volume. V1=0.6×V2=0.6×5×10−3 m3=3×10−3 m3V_1 = 0.6 \times V_2 = 0.6 \times 5\times10^{-3}\ \text{m}^3 = 3\times10^{-3}\ \text{m}^3.

The block floats with 40% of its volume above water and 60%, or 3×10−3 m33\times10^{-3}\ \text{m}^3, submerged.

Competitive stretch

A solid of volume 2×10−4 m32\times10^{-4}\ \text{m}^3 floats in a liquid of density 1200 kg/m31200\ \text{kg/m}^3 with 1.5×10−4 m31.5\times10^{-4}\ \text{m}^3 of its volume immersed. What is the density of the solid, and does that value make physical sense for a floating body?

Step 1. Substitute directly into the floatation relation rearranged for ρ1\rho_1: ρ1=ρ2×V1V2=1200×1.5×10−42×10−4=1200×0.75=900 kg/m3\rho_1 = \rho_2 \times \dfrac{V_1}{V_2} = 1200 \times \dfrac{1.5\times10^{-4}}{2\times10^{-4}} = 1200 \times 0.75 = 900\ \text{kg/m}^3.

Step 2. Check the answer against the physics. 900 kg/m3900\ \text{kg/m}^3 is less than the liquid's 1200 kg/m31200\ \text{kg/m}^3, which is exactly what floating requires — a density greater than 1200 kg/m31200\ \text{kg/m}^3 would sink the solid entirely, and the relation would have no valid answer with V1<V2V_1 < V_2.

The density of the solid is 900 kg/m3900\ \text{kg/m}^3, consistent with it floating rather than sinking.

Common traps

  • Thinking heavy objects always sink. It is average density, not total weight, that decides floating — a hollow steel ship floats while a small solid steel ball sinks.
  • Using the total volume as the displaced volume. Only the immersed volume V1V_1 displaces liquid and produces upthrust for a floating body — not the whole volume V2V_2, unlike a fully submerged body where V1=V2V_1 = V_2.
  • Believing the upthrust on a floating body exceeds its weight. At equilibrium FB=WF_B = W exactly; if upthrust were greater the body would keep rising indefinitely, which never happens.
  • Forgetting the apparent weight of a freely floating object is zero, since the liquid's upthrust already balances its entire weight.

Ask the tutor: Want to see how changing the liquid's density (say, floating the same block in oil instead of water) shifts the immersed fraction? Ask the AI tutor to walk through it with you.

Why does a submarine sometimes float and sometimes sink to a chosen depth?

A submarine changes its average density on purpose using ballast tanks. Filling the tanks with seawater adds mass without adding volume, raising the average density above the surrounding water's density so the submarine sinks. Pumping the water back out lowers the average density below the water's, so it rises and floats. By controlling how much water sits in the tanks, the crew can also hold the average density equal to the water's density and hover at a chosen depth, fully submerged but neither rising nor sinking.

If ice is less dense than water, why does an iceberg float so low, with most of it underwater?

The floatation relation ρ1/ρ2=V1/V2\rho_1/\rho_2 = V_1/V_2 says the submerged fraction depends on how close the two densities are, not just on which one is smaller. Ice has a density of about 920 kg/m3920\ \text{kg/m}^3 and seawater about 1025 kg/m31025\ \text{kg/m}^3 — the two are close, so the ratio ρ1/ρ2\rho_1/\rho_2 is close to 1, roughly 0.90.9. That means about 90%90\% of an iceberg's volume must stay submerged to displace enough water to balance its weight, leaving only a small visible tip above the surface.

Can I use the floatation relation for a body that sinks completely?

No, not in the form ρ1/ρ2=V1/V2\rho_1/\rho_2 = V_1/V_2 with V1V_1 less than V2V_2. That relation comes from the equilibrium condition FB=WF_B = W, which only holds for a body floating with part of it above the surface. If the body's density is greater than the liquid's, it sinks and stays fully submerged, so its upthrust never grows large enough to balance its weight — there the relevant idea is Archimedes' principle for a fully submerged body, with V1=V2V_1 = V_2 throughout, not the floatation relation.

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