ProofComplete

Proof of Well-Definedness of Integration

The integral of a differential form on an oriented manifold must be shown to be independent of the choice of atlas and partition of unity. This fundamental result ensures that integration is a geometric invariant.


Statement

Theorem4.1Well-definedness of the integral

Let MM be an oriented smooth nn-manifold, ω\omega a compactly supported nn-form on MM, {(Uα,φα)}\{(U_\alpha, \varphi_\alpha)\} and {(Vβ,ψβ)}\{(V_\beta, \psi_\beta)\} two oriented atlases, and {ρα}\{\rho_\alpha\}, {σβ}\{\sigma_\beta\} subordinate partitions of unity. Then

αφα(Uα)(φα1)(ραω)=βψβ(Vβ)(ψβ1)(σβω).\sum_\alpha \int_{\varphi_\alpha(U_\alpha)} (\varphi_\alpha^{-1})^*(\rho_\alpha \omega) = \sum_\beta \int_{\psi_\beta(V_\beta)} (\psi_\beta^{-1})^*(\sigma_\beta \omega).

Proof

Proof

Step 1: Double partition. Since αρα=1\sum_\alpha \rho_\alpha = 1 and βσβ=1\sum_\beta \sigma_\beta = 1, we have

ραω=βρασβω,σβω=αρασβω.\rho_\alpha \omega = \sum_\beta \rho_\alpha \sigma_\beta \omega, \quad \sigma_\beta \omega = \sum_\alpha \rho_\alpha \sigma_\beta \omega.

Thus both sums equal α,βMρασβω\sum_{\alpha, \beta} \int_M \rho_\alpha \sigma_\beta \omega (with appropriate chart interpretation). It suffices to show that for a single term η=ρασβω\eta = \rho_\alpha \sigma_\beta \omega (compactly supported in UαVβU_\alpha \cap V_\beta), the two chart integrals agree.

Step 2: Change of variables. Let η\eta be an nn-form compactly supported in the overlap UαVβU_\alpha \cap V_\beta. In the chart φα\varphi_\alpha:

φα(UαVβ)(φα1)η.\int_{\varphi_\alpha(U_\alpha \cap V_\beta)} (\varphi_\alpha^{-1})^*\eta.

In the chart ψβ\psi_\beta:

ψβ(UαVβ)(ψβ1)η.\int_{\psi_\beta(U_\alpha \cap V_\beta)} (\psi_\beta^{-1})^*\eta.

The transition map τ=ψβφα1\tau = \psi_\beta \circ \varphi_\alpha^{-1} relates these. Write (φα1)η=f(x)dx1dxn(\varphi_\alpha^{-1})^*\eta = f(x) dx^1 \wedge \cdots \wedge dx^n in coordinates xx. Under the change of variables y=τ(x)y = \tau(x):

(ψβ1)η=f(τ1(y))det(Dτ1(y))dy1dyn.(\psi_\beta^{-1})^*\eta = f(\tau^{-1}(y)) \det(D\tau^{-1}(y)) \, dy^1 \wedge \cdots \wedge dy^n.

Step 3: Orientation consistency. Since both atlases are oriented-compatible, the transition map τ\tau is orientation-preserving, meaning det(Dτ)>0\det(D\tau) > 0 everywhere. By the standard change of variables formula for Lebesgue integrals:

f(x)dx1dxn=f(τ1(y))det(Dτ1(y))dy1dyn.\int f(x) dx^1 \cdots dx^n = \int f(\tau^{-1}(y)) |\det(D\tau^{-1}(y))| dy^1 \cdots dy^n.

Since det(Dτ1)>0\det(D\tau^{-1}) > 0, we have det(Dτ1)=det(Dτ1)|\det(D\tau^{-1})| = \det(D\tau^{-1}), so the two expressions agree. \blacksquare


Consequences

RemarkRole of orientation

If the transition maps could reverse orientation (negative Jacobian determinant), the absolute value in the change of variables formula would differ from the signed determinant, and the integral would depend on the atlas. This is precisely why orientability is necessary for integrating forms. On non-orientable manifolds, one integrates densities instead, which transform by detJ|\det J|.

ExampleFailure of well-definedness without orientation

Consider the Mobius band MM with a "top form" ω\omega defined on charts. Following ω\omega around the band, the form returns with opposite sign. Any global "volume form" would need to vanish somewhere, so MM has no consistent orientation. Attempting to define Mω\int_M \omega via charts gives contradictory signs in overlapping regions.

RemarkExtension to manifolds with boundary

The same proof shows well-definedness of integration on oriented manifolds with boundary, using half-space charts Hn\mathbb{H}^n near the boundary. The transition maps between half-space charts preserve orientation and respect the boundary, ensuring the integral remains well-defined.