centre of mass
Let ν be a Borel signed measure for some set E⊆ℝn. The centre of mass of E (with respect to ν) is a vector in ℝn defined by the following vector-valued integral:
𝝁(E;ν)=1ν(E)∫𝐫∈E𝐫𝑑ν,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→ℝ,
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 measure 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 measure.
The measure ν could also be discrete. For example, E could be a finite set of points {xi}⊂ℝn 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 ℝn is defined by
𝝁(ν)=𝝁(ℝn;ν)=1ν(ℝn)∫𝐫∈ℝn𝐫𝑑ν |
(provided this exists). If νE is defined by νE(S)=ν(S∩E) 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:ℝn→ℝn is an invertible linear map, then by a straightforward change of variable
in the integrand,
𝝁(TE;ν∘T-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 ν∘T-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 D⊂ℝ2 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 measure on ℝ2,
then
T(𝝁(D;λ)) | =𝝁(TD;λ∘T-1) | |||
=𝝁(TD;λ) | (λ is invariant![]() |
|||
=𝝁(D;λ), | (TD=D by symmetry |
which means the x component 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 |