ConceptComplete

Integration on Manifolds - Core Definitions

Integration on manifolds extends the familiar notion of integration from calculus to curved spaces. Differential forms provide the natural objects to integrate, generalizing functions, vector fields, and volume elements.

DefinitionIntegration of n-Forms

Let MM be an oriented nn-manifold and ω\omega a compactly supported nn-form on MM. The integral of ω\omega over MM is defined by partitioning MM with charts (Uα,φα)(U_\alpha, \varphi_\alpha) and a subordinate partition of unity {ρα}\{\rho_\alpha\}:

Mω=αφα(Uα)(φα1)(ραω)\int_M \omega = \sum_\alpha \int_{\varphi_\alpha(U_\alpha)} (\varphi_\alpha^{-1})^*(\rho_\alpha \omega)

where the right side uses standard Lebesgue integration on Rn\mathbb{R}^n.

This definition is independent of the choice of charts and partition of unity, provided the orientation is respected. The key is that nn-forms transform by the Jacobian determinant under coordinate changes.

ExampleIntegration on $\mathbb{R}^n$

On Rn\mathbb{R}^n with standard coordinates and orientation, integrating ω=f(x)dx1dxn\omega = f(x) dx^1 \wedge \cdots \wedge dx^n gives

Rnω=Rnf(x)dx1dxn\int_{\mathbb{R}^n} \omega = \int_{\mathbb{R}^n} f(x) dx^1 \cdots dx^n

recovering the usual Riemann or Lebesgue integral.

DefinitionIntegration over Submanifolds

Let SMS \subset M be an oriented kk-dimensional submanifold and ω\omega a kk-form on MM. The integral of ω\omega over SS is

Sω=Siω\int_S \omega = \int_S i^*\omega

where i:SMi: S \hookrightarrow M is the inclusion map and iωi^*\omega is the pullback, which is a kk-form on the kk-manifold SS.

Remark

The crucial fact is that only top-degree forms can be integrated on oriented manifolds. A kk-form integrates over a kk-dimensional oriented submanifold, giving a real number.

ExampleLine Integrals

A line integral γω\int_\gamma \omega where γ:[a,b]M\gamma: [a,b] \to M is a curve and ω\omega is a 1-form can be written as

γω=abγω=abωγ(t)(γ(t))dt\int_\gamma \omega = \int_a^b \gamma^*\omega = \int_a^b \omega_{\gamma(t)}(\gamma'(t)) dt

This generalizes work integrals Fdr\int \mathbf{F} \cdot d\mathbf{r} from vector calculus.

DefinitionOrientation-Preserving Maps

A diffeomorphism f:MNf: M \to N between oriented manifolds is orientation-preserving if for every chart (U,φ)(U, \varphi) on MM and (V,ψ)(V, \psi) on NN in the oriented atlases, the Jacobian determinant of ψfφ1\psi \circ f \circ \varphi^{-1} is positive.

TheoremChange of Variables

If f:MNf: M \to N is an orientation-preserving diffeomorphism and ω\omega is a compactly supported nn-form on NN, then

Mfω=Nω\int_M f^*\omega = \int_N \omega

If ff reverses orientation, then Mfω=Nω\int_M f^*\omega = -\int_N \omega.

This is the manifold version of the change of variables formula from multivariable calculus, showing that integration respects the geometry encoded in differential forms.