Sphericity

From HandWiki

Sphericity is a measure of how closely the shape of a physical object resembles that of a perfect sphere. For example, the sphericity of the balls inside a ball bearing determines the quality of the bearing, such as the load it can bear or the speed at which it can turn without failing. Sphericity is a specific example of a compactness measure of a shape.

Sphericity applies in three dimensions; its analogue in two dimensions, such as the cross sectional circles along a cylindrical object such as a shaft, is called roundness.

Definition

Defined by Wadell in 1935,[1] the sphericity, Ψ, of an object is the ratio of the surface area of a sphere with the same volume to the object's surface area:

Ψ=π13(6Vp)23Ap

where Vp is volume of the object and Ap is the surface area. The sphericity of a sphere is unity by definition and, by the isoperimetric inequality, any shape which is not a sphere will have sphericity less than 1.

Ellipsoidal objects

The sphericity, Ψ, of an oblate spheroid (similar to the shape of the planet Earth) is:

Ψ=π13(6Vp)23Ap=2ab23a+b2a2−b2ln⁡(a+a2−b2b),

where a and b are the semi-major and semi-minor axes respectively.

Derivation

Hakon Wadell defined sphericity as the surface area of a sphere of the same volume as the object divided by the actual surface area of the object.

First we need to write surface area of the sphere, As in terms of the volume of the object being measured, Vp

As3=(4πr2)3=43π3r6=4π(42π2r6)=4π⋅32(42π232r6)=36π(4π3r3)2=36πVp2

therefore

As=(36πVp2)13=3613π13Vp23=623π13Vp23=π13(6Vp)23

hence we define Ψ as:

Ψ=AsAp=π13(6Vp)23Ap

Sphericity of common objects

Name Picture Volume Surface area Sphericity
Sphere 50px 4π3r3 4πr2 1
Disdyakis triacontahedron 50px 900+720511s3 180179−24511s2 ((5+45)211π5)13179−245≈0.9857
Tricylinder 50px 16−82r3 48−242r2 36π+18π236≈0.9633
Rhombic triacontahedron 50px 45+25s3 125s2 455625π2+202500π25615≈0.9609
Icosahedron 50px 15+5512s3 53s2 2100π3+900π15330≈0.9393
Bicylinder 50px 163r3 16r2 2π32≈0.9226
Ideal bicone
(h=r2)
50px 2π3r2h=2π23r3 2πrr2+h2=2π3r2 43263≈0.9165
Dodecahedron 50px 15+54s3 325+105s2 ((15+75)2π12(25+105)32)13≈0.9105
Rhombic dodecahedron 50px 1639s3 82s2 2592π266≈0.9047
Ideal torus
(R=r)
50px 2π2Rr2=2π2r3 4π2Rr=4π2r2 18π232π≈0.8947
Ideal cylinder
(h=2r)
50px πr2h=2πr3 2πr(r+h)=6πr2 1833≈0.8736
Octahedron 50px 23s3 23s2 3π333≈0.8456
Hemisphere 50px 2π3r3 3πr2 2233≈0.8399
Cube 50px s3 6s2 36π36≈0.8060
Ideal cone
(h=2r2)
50px π3r2h=2π23r3 πr(r+r2+h2)=4πr2 432≈0.7937
Tetrahedron 50px 212s3 3s2 12π336≈0.6711

See also

References

  1. ↑ Wadell, Hakon (1935). "Volume, Shape, and Roundness of Quartz Particles". The Journal of Geology 43 (3): 250–280. doi:10.1086/624298. Bibcode: 1935JG.....43..250W.