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单词 AlternateCharacterizationOfCurl
释义

alternate characterization of curl


Let 𝐅 be a smooth vector fieldMathworldPlanetmath on (an open subset of) 3.

We show that curl𝐅 defined using the coordinate-free definition given on the parent entry (http://planetmath.org/curl)is the same as the curl definedby ×𝐅 in Cartesian coordinatesMathworldPlanetmath.

The case for spherical surfaces

This will be done by directly computing the limit 𝐋 of surfaceintegrals defining curl𝐅(𝐩),using spheres S2(r,𝐩) centered at 𝐩 of radius r. The formulaMathworldPlanetmathPlanetmath is:

curl𝐅(𝐩)=𝐋=limr034πr3S2(r,𝐩)𝐧×𝐅𝑑A
=limr03r24πr3S2𝐧×𝐅(r𝐧+𝐩)𝑑A,

where 𝐧 is the outward unit normal to the surface (at each point of the surface), andS2 is the unit sphereMathworldPlanetmath at the origin.

We simplify the last integral.Expanding 𝐅(r𝐧+𝐩)in a first-degree Taylor polynomial about 𝐩, we have

S2𝐧×𝐅(r𝐧+𝐩)𝑑A=S2𝐧×𝐅(𝐩)𝑑A
+S2𝐧×D𝐅(𝐩)r𝐧𝑑A+S2𝐧×o(r𝐧)𝑑A.

The integral S2𝐧×𝐅(𝐩)𝑑Avanishes by symmetryMathworldPlanetmathPlanetmath of the sphere,while

S2𝐧×o(r𝐧)𝑑AS2𝐧o(r)𝑑A=o(r).

Combining these facts, we obtain

𝐋=limr0[0+34πrS2𝐧×D𝐅(𝐩)r𝐧𝑑A+o(1)]
=34πS2𝐧×D𝐅(𝐩)𝐧𝑑A.

Notice that 𝐋 depends only on the derivativePlanetmathPlanetmath of 𝐅at 𝐩.

We want to evaluate the last integral in Cartesian coordinates.Let 𝐞k be an orthonormal basisMathworldPlanetmath of 3oriented positively, and let B be the matrix of the derivativeD𝐅(p) in this basis.Then the kth coordinateMathworldPlanetmathPlanetmath of 𝐋 with respect to thesame basisis

(S2𝐧×B𝐧𝑑A)𝐞k=S2(𝐧×B𝐧)𝐞k𝑑A

The kth coordinate of the integrand is

(𝐧×B𝐧)𝐞k=ni(B𝐧)jϵijk=niBljnlϵijk,

where to lessen the writing, we employthe Einstein summation convention, alongwith the Levi-Civita permutation symbol ϵijk, and Bljdenotes the entry at the jth row, lth column of B.

In the summation above, if a summmand has il,then the integral of that summand over the sphere is zero, by symmetry.This means that in the summation the index l may be set to i,and thus

(S2𝐧×B𝐧𝑑A)𝐞k=S2niBijniϵijk𝑑A=BijϵijkS2(ni)2𝑑A.

Now there is a formula for the evaluation of integralsof polynomials over Sm-1m, in terms of the gamma function;in our case (m=3) the formula reads:

S2(ni)2𝑑A=2Γ(32)Γ(12)Γ(12)Γ(32+12+12)=2Γ(32)ππ32Γ(32)=4π3.

(If you do not know this formula, the integral in our casecan be computed directly using spherical coordinatesMathworldPlanetmath.)Therefore the kth component of 𝐋 is

𝐋𝐞k=34πBijϵijkS2(ni)2𝑑A=Bijϵijk=Fjxi|𝐩ϵijk.

But this is just (×𝐅(𝐩))𝐞k.

The case for arbitrary surfaces

Although we have onlycomputed

𝐋=curl𝐅(𝐩)=limV01VS𝐧×𝐅𝑑A

only for spheres S=S2(r,𝐩),this formula holds for arbitrary closed surfaces S that shrink nicely to 𝐩.It is hardly obvious, especially since our computation before dependedon the symmetry of the sphere extensively.

To show the general result,consider the triple scalar product(𝐯×𝐅)𝐞k.This is a linear functionalMathworldPlanetmathPlanetmath in the vector 𝐯,so there existsa unique vector function 𝐠k such that(𝐯×𝐅)𝐞k=𝐠k𝐯 for all 𝐯3.We can find the components of this 𝐠k by evaluating the functionalMathworldPlanetmathPlanetmathat 𝐯=𝐞i:

gki=𝐠k𝐞i=(𝐞i×𝐅)𝐞k=det(𝐞i,𝐅,𝐞k)=Fjϵijk.

The reason for considering such expressions is that, putting 𝐯=𝐧, we have

S(𝐧×𝐅)𝐞k𝑑A=S𝐠k𝐧𝑑A=S𝐠k𝑑𝐀.

So we have converted the original integral into an ordinary surface integral.And this surface integral can be changed into a volume integral, by using the divergence theoremMathworldPlanetmathPlanetmath:

S𝐠k𝑑𝐀=Mdiv𝐠kdV=MFjxiϵijk𝑑V,

where M is the volume whose boundary is S.Hence

𝐋𝐞k=limV01VS(𝐧×𝐅)𝐞k𝑑A
=limV01VMFjxiϵijk𝑑V
=Fjxi|𝐩ϵijk=(×𝐅(𝐩))𝐞k.

Definition in terms of differential forms

We mention, in passing,a computational, yet coordinate-free, alternative to the definition of the curl,using differential formsMathworldPlanetmath.If ω is a 1-form on 3 such that ω(𝐯)=𝐅,𝐯,then the curl of 𝐅 is defined as the vector function 𝐠=gkek such that

dω(𝐮,𝐯)=𝐠,𝐮×𝐯.

In Cartesian coordinates, we have

ω=F1dx1+F2dx2+F3dx3
dω=g1dx2dx3+g2dx3dx1+g3dx1dx2,

If we take the exterior derivative of the first equation for ω, and then equate componentswith the second equation for dω,we find that gk = (×𝐅)𝐞k,so our new definition is equivalentMathworldPlanetmathPlanetmathPlanetmathPlanetmath to the others.

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更新时间:2025/5/4 15:49:16