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CorollaryStatement: AI-adaptedProof: AI-adaptedPipeline-generatedjudge pass (gpt-5.6-terra)audited 2026-09-07
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General Stokes agrees with both planar Green formulas

Statement

Assume ACω. For a compact smooth planar region D oriented by dx∧dy and smooth P,Q on a neighborhood, general Stokes gives ∫∂D(P dx+Q dy)=∫D(Qx−Py) dx dy, ∫∂D(P dy−Q dx)=∫D(Px+Qy) dx dy. When D also has the supplied finite elementary Green decomposition required by the classical results, these are exactly their circulation and outward-flux formulas. Outer boundary curves run counterclockwise and holes clockwise.

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]

Green's theorem is the curl statement for a planar field lifted to R3: Let D be a finite elementary Green region with its supplied decomposition, positively oriented, and let P,Q be C1 on an open U⊆R2 containing D. Define the lift F~(x,y,z):=(P(x,y), Q(x,y), 0)((x,y,z)∈U×R), a field on the open set U×R⊆R3. Then F~ is C1, its curl has first and second coordinates identically 0 and third coordinate ∂xQ−∂yP at every point, independent of z, and the circulation of the planar field around the positive boundary chain equals the integral of the third coordinate of the curl of the lift: ∫∂D(P,Q)⋅dr=∬D(curl⁡F~)z(x,y,0) dA.

[F3]

The planar divergence theorem: the flux form of Green's theorem: Let D be a finite elementary Green region with its supplied decomposition, positively oriented, and let F=(Fx,Fy) be C1 on an open U⊆R2 containing D. Then ∫∂D(−Fy) dx+Fx dy=∬D(∂xFx+∂yFy) dA, the right-hand integrand being the divergence of F as a field on an open subset of R2. Moreover, if σ:[α,β]→R2 is one of the arcs of the positive boundary chain and its derivative is nowhere zero on a piece with continuous derivative extension v, then on that piece ∫σ(−Fy) dx+Fx dy=∫σ⟨F,ν⟩ ds,ν:=(v2,−v1)∥v∥2, where ν is the unit vector obtained from the tangent v by a quarter turn clockwise.

[F4]

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.

Proof

Given: The objects and hypotheses in the statement above.

1.1F1algebra

The coordinate derivative gives d(Pdx+Qdy)=(Qx−Py)dx∧dy and d(Pdy−Qdx)=(Px+Qy)dx∧dy. Apply Stokes to these smooth one-forms on compact D.

2.1F3F4step 1.1

For a positive tangent v=(v1,v2), the outward normal is ν=(v2,−v1)/∥v∥, since (ν,v) has positive determinant. Thus the flux form evaluated on v is Pv2−Qv1=⟨(P,Q),ν⟩∥v∥. This yields counterclockwise outer curves and clockwise holes. Parametrization integration identifies these form integrals with the scalar Riemann and curve integrals.

3.1F2F3step 1.1step 2.1∎

On the common elementary smooth scope, the classical circulation result uses the lift (P,Q,0), whose third curl component is Qx−Py, and the flux result uses divergence Px+Qy. These match the two computed expressions exactly. Their supplied decomposition and neighborhood hypotheses are retained. Empty regions or zero fields give zero; no corners theorem is invoked.

Depends on

Used by

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Sources