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Sandbox Physics

M092 · Fluid mechanics

Buoyancy & Metacentric Stability

Can a floating hull still overturn? Yes. Floating only needs the weight to equal the buoyancy. Staying upright needs more: as the hull heels, buoyancy and weight must form a torque that pushes it back. Whether they do depends on the shape of the underwater volume and how high the ballast sits, and a hull that rights itself at small angles can have that torque reverse at large ones.

Move a ballast mass inside a sealed box hull or a flared prism hull. Compare the exact displaced geometry, the restoring curve at finite heel and the initial stability. Then infer the initial metacentric height from small-heel moments you record.

Interactive modelBuoyancy & Metacentric Stability
Total massReady\text{Ready}
Displaced volumeReady\text{Ready}
WeightReady\text{Ready}
Buoyant forceReady\text{Ready}
Signed righting armReady\text{Ready}
Signed restoring momentReady\text{Ready}
Initial metacentric heightReady\text{Ready}
Mass centre transverse positionReady\text{Ready}
Mass over fully submerged displacementReady\text{Ready}
Initial height from raw momentsReady\text{Ready}
Small-heel fit residualReady\text{Ready}
Recorded stationsReady\text{Ready}
Force or volume balance residualReady\text{Ready}
Model stateReady\text{Ready}

Physics tutorial

Displacement, ballast and initial stability

BackgroundThis experiment tells you something only when the hull geometry, the forces on the hull and the recorded data agree.

Why it mattersYou link a floating hull to a quantitative task, finding its initial metacentric height, and then test where that approach works and where it fails.

Start with the essentials

Focus question
Does floating mean stable?
One-sentence intuition
Compare the full geometric model, its small-angle approximation and the separately recorded data.

Core mathematical model

Vertical force balance

ρg∇=mg\rho g\nabla=mg

To float in equilibrium, the hull must displace enough water. A sealed hull that is overloaded cannot reach this balance.

Centre of the displaced volume

∇=LAsrB=1As∫Asr dA\begin{aligned}\nabla&=LA_s\\\boldsymbol r_B&=\frac{1}{A_s}\int_{A_s}\boldsymbol r\,dA\end{aligned}

Cut the tilted cross-section at the waterline, then integrate the submerged area and its centroid.

Restoring moment at any heel angle

GZ=xB−xGMR=mg GZ\begin{aligned}GZ&=x_B-x_G\\M_R&=mg\,GZ\end{aligned}

For a floating hull, a positive moment resists a clockwise heel. A negative arm makes the heel worse.

Initial metacentric height

BM=Iwp∇GM=KB+BM−KG\begin{aligned}BM&=\frac{I_{\mathrm{wp}}}{\nabla}\\GM&=KB+BM-KG\end{aligned}

The second moment of the waterplane is taken about its centroid. This height describes only small angles and does not replace the curve for finite heel.

Initial slope measured from raw data

Mimg≃c+aθi+bθi2+dθi3GM^=a\begin{aligned}\frac{M_i}{mg}&\simeq c+a\theta_i+b\theta_i^2+d\theta_i^3\\\widehat{GM}&=a\end{aligned}

Angles are in radians. Fit a cubic with a free offset over four degrees, using the raw moments and the separately known mass.

Common difficulties

A reference curve is not a measurement

Typical misconceptionThe reference curve on screen is a measured result.

Better mental modelOnly the sensor channels you record count as observations, and changing the setup clears them. The perturbations are deterministic, so they give no statistical certification.

Run the experiment

  1. 01

    Move weight down

    Compare Low ballast with High ballast, unstable.

    What to observe: Both hulls float, but near upright their restoring curves slope in opposite directions.
  2. 02

    Look beyond the initial slope

    Drag the gold heel selector out to large angles.

    What to observe: The curve from the full geometry moves away from the small-angle sine approximation.
  3. 03

    Move the ballast sideways

    Select Off-centre ballast and look at zero heel.

    What to observe: The initial stability can be positive while the upright hull still feels a nonzero moment.
  4. 04

    Measure first, then infer

    Acquire the small-heel sweep, add perturbations and export the CSV.

    What to observe: The slope estimate comes from the raw moments. Clear them and the estimate disappears.
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