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CorollaryStatement: AI-adaptedProof: AI-adaptedPipeline-generatedjudge pass (gpt-5.6-terra)audited 2026-09-07
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Agreement of general and classical surface Stokes

Statement

Assume ACω. Let S⊂R3 be a compact oriented smooth embedded surface with boundary, and let F be smooth on an open neighborhood of S. Set α=Fxdx+Fydy+Fzdz and μ=dx∧dy∧dz. Then dα=ιcurl⁡Fμ,∫∂Sα=∫Sιcurl⁡Fμ. On an oriented parametrization r(u,v) the latter integrand is (curl⁡F)(r)⋅(ru×rv) du∧dv; on a boundary curve it is F(r)⋅r′ dt. On the common smooth patch scope this is the published classical Stokes theorem, using the standard Euclidean metric identification.

Facts & Assumptions

[F1]

The general Stokes theorem: Assume ACω. Let M be an oriented smooth n-manifold with boundary, n≥1, and let η∈Ωcn−1(M). With j:∂M↪M and the outward-normal-first orientation, ∫Mdη=∫∂Mj∗η. An empty boundary contributes zero; in dimension one its integral is a finite signed sum of point values.

[F2]

Integration on an oriented embedded submanifold: Let j:S↪M be an oriented embedded smooth k-submanifold, with boundary allowed. For a smooth k-form ω on M such that j∗ω has compact support on S, define ∫Sω:=∫Sj∗ω. If F:T→S is an orientation-preserving diffeomorphism, this equals ∫T(jF)∗ω. Compact support is required on S itself.

[F3]

Computing form integrals by finite parametrizations: Let n≥1, let Mn be oriented, and let ω∈Ωcn(M). For 1≤i≤m let Di⊂Rn be bounded open Jordan domains and Fi:D‾i→M continuous and smooth up to the boundary in target coordinates: near each parameter point, a target coordinate representative extends smoothly to a Euclidean neighborhood. Suppose Fi∣Di is an orientation-preserving diffeomorphism onto an open Wi⊂M, the Wi are pairwise disjoint, and supp⁡ω⊂⋃iW‾i. Then ∫Mω=∑i=1m∫DiFi∗ω. An empty family is allowed when the support is empty. No nonsingularity of DFi on ∂Di, and no M-valued extension across a genuine target boundary, is assumed.

[F4]

The classical Stokes theorem for a C2 patch over a finite elementary Green region: Let (D,φ) be a C2 patch over a finite elementary Green region (def-the-induced-boundary-chain-of-a-c2-surface-patch), with positive boundary chain ∂D=(σ1,…,σm) and induced boundary chain φ(∂D), and let F be a C1 vector field on an open set U⊆R3 containing φ[D]. Then the circulation around the induced boundary chain equals the flux of the curl in the induced orientation: ∮φ(∂D)F⋅dr=∫D⟨(curl⁡F)∘φ, φu×φv⟩. The right-hand side is the flux of curl⁡F through the patch in the orientation induced by φ, in the sense of def-oriented-unit-normal-and-flux-of-a-surface-patch.

[F5]

Divergence and curl of a C1 vector field: Let n≥1, let U⊆Rn be open and let F=(F0,…,Fn−1):U→Rn be C1 in the componentwise Euclidean sense of def-ck-euclidean-maps-and-diffeomorphisms. Then the divergence of F is div⁡F:=∑i<n∂iFi, the function U→R whose value at p is ∑i<n∂iFi(p). The partial derivatives are those of def-directional-and-partial-derivatives, and the sum is the finite sum used throughout def-euclidean-inner-product. Since each ∂iFi is continuous on U, so is div⁡F. Now let n=3 and let F:U→R3 be C1 on an open U⊆R3. Following def-cross-product-in-r3, write the three coordinates of a point and of a vector as x,y,z rather than 0,1,2, so that F=(Fx,Fy,Fz) means F=(F0,F1,F2) and ∂x,∂y,∂z are ∂0,∂1,∂2. With that naming, the curl of F is curl⁡F:=(∂yFz−∂zFy, ∂zFx−∂xFz, ∂xFy−∂yFx), a map U→R3 each of whose coordinates is continuous on U. In this naming the divergence reads div⁡F=∂xFx+∂yFy+∂zFz. Both operators are defined pointwise from the first partial derivatives of the components, so no differentiability of F beyond C1 is used and no orientation or metric structure enters beyond the standard coordinates of def-jacobian-matrix-and-gradient. For a C1 scalar function f on U, the gradient ∇f=(∂0f,…,∂n−1f) is that of def-jacobian-matrix-and-gradient; in the three-coordinate naming, ∇f=(∂xf,∂yf,∂zf).

Proof

Given: The objects and hypotheses in the statement above.

1.1F5algebra

Expand dα. Its coefficients of dy∧dz,dz∧dx,dx∧dy are respectively ∂yFz−∂zFy,∂zFx−∂xFz,∂xFy−∂yFx, exactly the three curl components. Contraction with μ gives the same expansion.

2.1F1F2step 1.1

Pull back to the compact surface and apply general Stokes, obtaining the integral identity. Evaluating the contracted three-form on (ru,rv) gives det⁡(curl⁡F,ru,rv)=(curl⁡F)⋅(ru×rv). The boundary pullback of α is F(r)⋅r′dt directly.

3.1F3F4step 2.1∎

The finite-parametrization theorem turns these expressions into the scalar flux and circulation integrals. For a patch over a supplied finite elementary Green region with its induced boundary chain, the classical theorem has exactly these two integrals; smooth r,F meet its C2,C1 requirements. Reversing the surface orientation changes both signs; empty surface or zero field gives zero.

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