centre of mass


Let ν be a Borel signed measure for some set En. The centre of mass of E (with respect to ν) is a vector in n defined by the following vector-valued integral:

𝝁(E;ν)=1ν(E)𝐫E𝐫𝑑ν,ν(E)0,±,

provided the integral exists. Intuitively, the integral is a weighted average of all the points of E.

Our abstract definition encompasses many situations. If E is a k-dimensional manifold, then we may take ν to be its absolute k-dimensional volume element (dν=dV). This would give the set E a unit mass density, and in this case the centre of mass of E is also called the centroid of E.

More generally, if we are given a measurable mass density ρ:E, then taking dν=ρdV, the definition defines the centre of mass for E with a mass density ρ. We do not restrict the density ρ (or the measureMathworldPlanetmath ν) to be non-negative; for this allows our definition to apply even to, for example, electrical charge densities.

If E is not a differentiable manifold, but is a rectifiable set, we can replace dV by the appropriate Hausdorff measureMathworldPlanetmath.

The measure ν could also be discrete. For example, E could be a finite setMathworldPlanetmath of points {xi}n with masses mi=ν(xi). In this case, the integral 𝝁(E;ν) reduces to a finite summation.

It is possible to economize the definition so that the set E does not have to be mentioned, although the result is somewhat unintuitive: the centre of mass of a finite signed Borel measure ν on n is defined by

𝝁(ν)=𝝁(n;ν)=1ν(n)𝐫n𝐫𝑑ν

(provided this exists). If νE is defined by νE(S)=ν(SE) for all measurable S and some fixed measurable E, then 𝝁(νE)=𝝁(E;ν).

The term centre of gravity is sometimes used loosely as a synonym for the centre of mass, but these are distinct concepts; the centre of gravity is supposed to be a single point on which the force of gravity can be considered to act upon. If E is three-dimensional and the force of gravity is uniform throughout E, then the centre of mass and the centre of gravity coincide.

As shown by the above examples, the centre of mass and its related concepts have applications in mechanics and other areas of physics.

Symmetry principle

If T:nn is an invertible linear mapMathworldPlanetmath, then by a straightforward change of variable in the integrand,

𝝁(TE;νT-1)=T(𝝁(E;ν)).

In particular, take T to be an isometry, and ν to be a k-dimensional volume measure for E. The corresponding k-dimensional volume measure for TE must be the same as νT-1, because T is an isometry. Then the above equation says that the centroid transforms as expected under isometries.

For example, it is intuitively obvious that the centre of mass of a disk D2 should be the centre of D. (Without loss of generality, assume that D is centered at the origin.) Using the property just mentioned, this is easy to prove rigorously too: if T is the isometry that reflects across the y-axis, and λ is the Lebesgue measureMathworldPlanetmath on 2, then

T(𝝁(D;λ)) =𝝁(TD;λT-1)
=𝝁(TD;λ) (λ is invariantMathworldPlanetmath under isometries)
=𝝁(D;λ), (TD=D by symmetryPlanetmathPlanetmath of the disk)

which means the x componentPlanetmathPlanetmath of 𝝁(D;λ) must be zero. Similarly, by considering reflections across the x-axis, we conclude that the y component of 𝝁(D;λ) must be zero.

Title centre of mass
Canonical name CentreOfMass
Date of creation 2013-03-22 15:28:09
Last modified on 2013-03-22 15:28:09
Owner stevecheng (10074)
Last modified by stevecheng (10074)
Numerical id 12
Author stevecheng (10074)
Entry type Definition
Classification msc 28A75
Classification msc 26B15
Synonym center of mass
Related topic PappussTheoremForSurfacesOfRevolution
Defines centre of gravity
Defines centroid
Defines center of gravity