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单词 SecondFundamentalForm
释义

second fundamental form


In classical differential geometrythe second fundamental formMathworldPlanetmath is a symmetric bilinear formMathworldPlanetmathdefined on a differentiableMathworldPlanetmathPlanetmath surface M embedded in 3, which in some sensemeasures the curvatureMathworldPlanetmathPlanetmath of M in space.

To construct the second fundamental form requires a small digression.After the digression we will discuss how it relates to the curvature of M.

Construction of the second fundamental form

Consider the tangent planesMathworldPlanetmath TpM of the surface M for each point pM.There are two unit normalsMathworldPlanetmath to TpM.Assuming M is orientable, we can choose one of these unit normals (http://planetmath.org/MutualPositionsOfVectors), n(p),so that n(p) varies smoothly with p.

Since n(p) is a unit vectorMathworldPlanetmath in 3, it may be consideredas a point on the sphere S23. Then wehave a map n:MS2. It is called the normal mapor Gauss map.

The second fundamental form is the tensor field on M definedby

p(ξ,η)=-Dnp(ξ),η,ξ,ηTpM,(1)

where , is the dot productMathworldPlanetmath of 3,and we consider the tangent planes of surfaces in 3to be subspacesPlanetmathPlanetmathPlanetmath of 3.

The linear transformation Dnp is in reality the tangentMathworldPlanetmathPlanetmathPlanetmath mappingDnp:TpMTn(p)S2,but since Tn(p)S2=TpM by the definition of n,we prefer to think of Dnp as Dnp:TpMTpM.

The tangent map Dn, is often called the Weingarten map.

Proposition 1.

The second fundamental form is a symmetric form.

Proof.

This is a computation using a coordinate chart σ for M.Let u,v be the corresponding names for the coordinatesMathworldPlanetmathPlanetmath.From the equation

n,σv=0,

differentiating with respect to u using the product ruleMathworldPlanetmath gives

n,2σuv=-nu,σv=-Dn(σu),σv=(σu,σv).(2)

(The second equality follows from the definition of the tangent map Dn.)Reversing the roles of u,v and repeating the last derivation,we obtain also:

n,2σuv=n,2σvu=(σv,σu).(3)

Since σ/u and σ/vform a basis for TpM, combining(2) and (3) proves that is symmetricMathworldPlanetmathPlanetmathPlanetmathPlanetmath.∎

In view of PropositionPlanetmathPlanetmath 1,it is customary to regard the second fundamental formas a quadratic formMathworldPlanetmath,as it done with the first fundamental formMathworldPlanetmath.Thus, the second fundamental form is referred to with the following expression11Unfortunately the coefficient M here clashes with our use of the letter M forthe surface (manifold), but whenever we write M, the context should make clearwhich meaning is intended.The use of the symbols L,M,N for the coefficients of the second fundamental formis standard, but probably was established long beforeanyone thought about manifolds.:

Ldu2+2Mdudv+Ndv2.

Compare with the tensor notation

=Ldudu+Mdudv+Mdvdu+Ndvdv.

Or in matrix form (with respect to the coordinates u,v),

=(LMMN).

Curvature of curves on a surface

Let γ be a curve lying on the surface M, parameterized by arc-length.Recall that the curvature κ(s) of γ at sis γ′′(s). If we want to measure the curvature of the surface, it is naturalto consider the component of γ′′(s) in the normal n(γ(s)).Precisely, this quantity is

γ′′(s),n(γ(s)),

and is called the normal curvatureMathworldPlanetmathPlanetmathPlanetmath of γ on M.

So to study the curvature of M, we ignore the component of the curvature of γin the tangent plane of M.Also, physically speaking, the normal curvature is proportional to the accelerationrequired to keep a moving particle on the surface M.

We now come to the motivation for defining the second fundamental form:

Proposition 2.

Let γ be a curve on M, parameterized by arc-length,and γ(s)=p.Then

γ′′(s),n(p)=(γ(s),γ(s)).
Proof.

From the equation

n(γ(s)),γ(s)=0,

differentiate with respect to s:

n(γ(s)),γ′′(s)=-ddsn(γ(s)),γ(s)
=-Dn(γ(s)),γ(s)
=(γ(s),γ(s)).

It is now time to mention an important consequence of Proposition 1:the fact that is symmetric means that-Dn is self-adjointPlanetmathPlanetmath with respect to the inner product (the first fundamental form). So, if -Dn is expressedas a matrix with orthonormal coordinates (with respect to ),then the matrix is symmetric. (The minus sign in front of Dnis to make the formulasMathworldPlanetmathPlanetmath work out nicely.)

Certain theorems in linear algebra tell usthat, -Dnp being self-adjoint, it has an orthonormal basis ofeigenvectorsMathworldPlanetmathPlanetmathPlanetmath e1,e2 with corresponding eigenvaluesMathworldPlanetmathPlanetmathPlanetmathPlanetmath κ1κ2.These eigenvalues are called the principal curvaturesof M at p.The eigenvectors e1,e2 are the principal directions.The terminology is justified by the following theorem:

Theorem 1 (Euler’s Theorem).

The normal curvature of a curve γ has the form

γ′′(s),n(p)=κ1cos2θ+κ2sin2θ,p=γ(s).

It follows that the minimum possible normal curvature is κ1,and the maximum possible is κ2.

Proof.

Since e1,e2 form an orthonormal basis for TpM, we may write

γ(s)=cosθe1+sinθe2

for some angle θ.Then

γ′′(s),n(p)=(γ(s),γ(s))
=-Dnp(γ(s)),γ(s)
=κ1cosθe1+κ2sinθe2,cosθe1+sinθe2
=κ1cos2θ+κ2sin2θ.

Matrix representations of second fundamental form and Weingarten map

At this point, we should find the explicit prescriptionsfor calculating the second fundamental form and the Weingarten map.

Let σ be a coordinate chart for M,and u,v be the names of the coordinates.For a test vector ξTpM, we write ξu and ξvfor the u,v coordinates of ξ.

We compute the matrix W for -Dn in u,v-coordinates.We have

(ξuξv)(LMMN)(ξuξv)=(ξ,ξ)=-Dn(ξ),ξ
=(Q(ξuξv))TQW(ξuξv)
=(ξuξv)(QTQ)W(ξuξv),

where Q is the matrix that changes from u,v-coordinates to orthonormalcoordinates for TpM — this is necessary to compute the inner product.But

QTQ=(EFFG)=(the first fundamental form),

because Q is the matrixwith columns σ/u and σ/vexpressed in orthonormal coordinates.

(More to be written…)

References

  • 1 Michael Spivak. A Comprehensive Introduction to Differential GeometryMathworldPlanetmath, volumes I and II.Publish or Perish, 1979.
  • 2 Andrew Pressley. Elementary Differential Geometry. Springer-Verlag, 2003.
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