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The first chip identifies the source of the statement or construction; the second identifies the source of its local proof or verification.
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Exterior potential sphere and zero ideal force
Statement
Let , , , and on define , , , and . Then are smooth in the exterior and up to , and uniformly in direction at infinity, and on . The pair solves , , the steady formal constant-density incompressible Euler system. Its boundary condition is impermeable slip/no-through: is generally nonzero tangent to the sphere, so this is not a no-slip solution. For the formal Euler stress and sphere normal pointing from the center into the exterior, the exact resultant is
The theorem concerns only this explicit inviscid mathematical model; it asserts neither a viscous zero-drag result nor an observed force. Under SI interpretation, are in metres, in metres per second, in kilograms per cubic metre, and in pascals.
Statement references
Iain W. Stewart, MIT 8.09/8.309, Chapter 6, §6.4
David Tong, Fluid Mechanics lecture notes, Chapter 1, §§2.3.2–2.3.3
Formal constant-density incompressible Euler system and pressure-stress definition: Formal constant-density incompressible Euler system.
Facts & Assumptions
Given: Use the constants, exterior domain, potential, velocity and pressure in the Statement. For the surface calculation, extend by the same displayed formulas to the open set , as time-independent fields on , and evaluate their spatial sections at a fixed time. All equations are formal pointwise model equations; the surface resultant uses the stated orientation.
Formal parameterized fluid systems and observables: and are Cartesian operators, and smooth scalar fields have commuting mixed partials.
Formal constant-density incompressible Euler system: the steady inviscid equations are , , and the formal stress is . On a compact oriented regular surface patch in the open spatial domain of the fields, its resultant is ; here the fields used for this integral are stationary spatial sections.
Barotropic Kelvin and Bernoulli with exact hypotheses: for every vector field, . This is the exact algebraic clause of that theorem used here; no barotropic Bernoulli conclusion is invoked.
The first fundamental form, Gram matrix, and area density of a surface patch: the surface density is the nonnegative square root of the determinant of the Gram matrix of the parameter tangents.
Surface area and scalar surface integrals on a regular patch: a continuous scalar field is integrated against that density on the parameter region; area is the integral of the density, and changing values on a content-zero parameter boundary does not change the integral. Vector integrals are evaluated componentwise.
Proof
For , and for , so . Since , commuting smooth derivatives gives . Also , so . Therefore and by equality of the mixed second partials of . Direct differentiation yields . This gives uniform at infinity. At , , which is tangent to the sphere and has zero normal component.
By [F3] and , . The pressure definition gives , so the steady momentum equation in [F2] holds; step 1.1 supplies its divergence condition. The explicit formula gives , hence and uniformly in direction.
The displayed formulas extend smoothly to since their denominators are powers of . Thus , and [F2] applies to these stationary spatial fields on this sphere; their restrictions there equal the exterior traces by continuity. On the sphere, with , so . Thus depends on only through and is unchanged by . For , , , direct differentiation gives tangent Gram coefficients , , , so [F4] gives density (also ). The chart is regular in the parameter interior, and its poles and seam lie on the content-zero parameter boundary allowed in [F5]; those boundary values do not affect the integral. The substitution has absolute Jacobian one on each half of the longitude interval, preserves the density because , and induces the antipodal map, which reverses , so the vector integrand has zero integral over the sphere. By the stress convention in [F2], .
Remarks
The diagram is a two-dimensional cross-section of the sphere. The radial arrow is the outward unit normal ; the tangent arrow indicates the direction of the boundary velocity . The drawing is schematic and is not used in the field-equation or resultant proof.
diagram failed to render:
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\draw[->] (2.0,0.0) -- (3.0,0.0) node[right] {$U$ at infinity};
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