Sphericity
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Sphericity is a measure of how spherical an object is. Defined by Wadell in 1932, the sphericity, Ψ, of a particle is the ratio of the surface area of a sphere (with the same volume as the given particle) to the surface area of the particle:
where Vp is volume of the particle and Ap is the surface area of the particle
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[edit] Ellipsoidal Objects
- See also: Earth radius
The sphericity, Ψ, of an oblate spheroid (similar to the shape of the planet Earth or a Reese's Pieces candy) is defined as such:
(where a, b are the semi-major, semi-minor axes, respectively.
[edit] Derivation
Wadell (1932) defined Sphericity, Ψ, as the surface area of a sphere of the same volume as the particle divided by the actual surface area of the particle.
First we need to write surface area of the sphere, As in terms of the volume of the particle, Vp
therefore
hence we define Ψ as:
[edit] Sphericity of common objects
Name | Picture | Volume | Area | Sphericity |
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Platonic Solids | ||||
tetrahedron | ||||
cube (hexahedron) | ||||
octahedron | ||||
dodecahedron | ||||
icosahedron | ||||
Round Shapes | ||||
ideal cone |
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hemisphere (half sphere) |
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ideal cylinder |
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ideal torus (R = r) |
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sphere |