Vertical force balance
A floating equilibrium requires enough displaced volume. A sealed overloaded hull cannot satisfy this balance.
M092 · Fluid mechanics
Move a ballast mass through a sealed box or flared prism. Compare exact displaced geometry, finite-heel restoring curves and initial stability; infer the initial metacentric height from acquired small-heel moments.
Physics tutorial
BackgroundA water experiment is meaningful when geometry, forces or conserved quantities and acquired data agree.
Why it mattersConnect a physical apparatus to a quantitative task, then test its domain and limitations.
Start with the essentials
A floating equilibrium requires enough displaced volume. A sealed overloaded hull cannot satisfy this balance.
Clip the rotated cross-section at the waterline; integrate its area and centroid.
For a floating hull, positive moment opposes clockwise heel. Negative arm assists it.
The waterplane second moment is about its centroid. This local height does not replace a finite-heel curve.
Angles are radians. Fit a free offset and cubic over four degrees, using raw moments and independently known mass.
Typical misconceptionA displayed reference is an observed measurement.
Better mental modelRecord sensor channels explicitly. Changing the configuration clears observations; no statistical certification follows from deterministic perturbations.
Compare Low ballast with High ballast, unstable.
What to observe: Both can float; their local restoring slopes differ in sign.Drag the gold heel selector through large angles.
What to observe: The geometry curve and local sine approximation diverge.Select Off-centre ballast and inspect zero heel.
What to observe: Positive initial stability can coexist with a nonzero upright moment.Acquire the small-heel sweep, add perturbations and export CSV.
What to observe: The slope estimate uses raw moments; clearing them removes the estimate.