
Problem Statement
A cone of base radius R and height H floats in water with its vertex downwards. If θ is the semi-vertex angle of the cone and h is the depth of immersion, show that for stable equilibrium:
The variables are defined as follows:
- D: Diameter of the cone
- d: Diameter of the cone at the water surface
- h: Depth of immersion
- H: Height of the cone
- 2θ: Apex angle
- R: Base radius of the cone
- r: Radius of the cone at the water surface
Solution
-
Express the radius at the water surface:
r = h · tan θ -
The centroid (center of gravity) of the cone is located at a distance from the vertex:
OG = (3/4) · H -
The centroid of the immersed part (center of buoyancy) is at:
OB = (3/4) · h -
The vertical distance between these two centroids is:
BG = 0.75 (H − h) -
The moment of buoyancy (MB) is determined by the ratio of the moment of inertia (I) to the immersed volume (V):
MB = I/V = (¼ πr4) / (⅓ πr2h) = (0.75r2) / hSubstituting r = h tan θ:
MB = 0.75h tan2θ -
The metacentric height (GM) is the difference between MB and BG:
GM = 0.75h tan2θ − 0.75(H − h) -
For stable equilibrium, the metacentric height must be positive (GM > 0):
0.75h tan2θ − 0.75(H − h) > 0Dividing through by 0.75 and rearranging:
h tan2θ > H − hAdding h to both sides:
h (1 + tan2θ) > HSince sec2θ = 1 + tan2θ, we arrive at the stability condition:
sec2θ > H/h
Explanation
This analysis relies on the balance of moments about the floating cone’s center of mass and center of buoyancy. By finding the positions of these points (using the centroid positions of the entire cone and the immersed portion) and calculating the corresponding moment of buoyancy, we determine the metacentric height (GM). A positive GM indicates that any small tilt will create a restoring moment.
Rewriting the stability criterion in terms of the cone’s geometry (through the semi-vertex angle θ) and the depth of immersion (h) leads to the condition sec2θ > H/h, which must be satisfied for the cone to remain stable in water.
Physical Meaning
The inequality sec2θ > H/h encapsulates the requirement that the metacenter (a point related to the distribution of buoyant forces) must lie above the center of gravity of the cone.
In practical terms, this means that if the cone’s semi-vertex angle is too large (making sec2θ small) or if the immersed depth h is too shallow relative to its height H, the restoring moments will be insufficient, and the cone may tip over. Meeting the inequality ensures that any slight tilt produces a restoring force, leading to stable equilibrium.



