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Exterior potential sphere and zero ideal force

Statement

Let a,ρ0>0, p∞∈R, U∈R3, and on Ωa={x∈R3:r=∣x∣>a} define n=x/r, ϕ(x)=(U⋅x)(1+a3/(2r3)), u=∇ϕ, and p=p∞+ρ0(∣U∣2−∣u∣2)/2. Then u,p are smooth in the exterior and up to r=a, u→U and p→p∞ uniformly in direction at infinity, and u⋅n=0 on r=a. The pair solves (u⋅∇)u+ρ0−1∇p=0, div⁡u=0, the steady formal constant-density incompressible Euler system. Its boundary condition is impermeable slip/no-through: u is generally nonzero tangent to the sphere, so this is not a no-slip solution. For the formal Euler stress σE=−pI3 and sphere normal n=x/a pointing from the center into the exterior, the exact resultant is

∫∣x∣=aσEn dS=−∫∣x∣=apn dS=0.

The theorem concerns only this explicit inviscid mathematical model; it asserts neither a viscous zero-drag result nor an observed force. Under SI interpretation, a,r,x are in metres, U,u in metres per second, ρ0 in kilograms per cubic metre, and p,p∞ in pascals.

Facts & Assumptions

Given: Use the constants, exterior domain, potential, velocity and pressure in the Statement. For the surface calculation, extend ϕ,u,p by the same displayed formulas to the open set D={x∈R3:∣x∣>0}, as time-independent fields on R×D, and evaluate their spatial sections at a fixed time. All equations are formal pointwise model equations; the surface resultant uses the stated orientation.

[F1]

Formal parameterized fluid systems and observables: ∇ and Δ are Cartesian operators, and smooth scalar fields have commuting mixed partials.

[F2]

Formal constant-density incompressible Euler system: the steady inviscid equations are (u⋅∇)u+ρ0−1∇p=0, div⁡u=0, and the formal stress is σE=−pI3. On a compact oriented regular surface patch S⊂Ω in the open spatial domain of the fields, its resultant is ∫SσEnS dS; here the fields used for this integral are stationary spatial sections.

[F3]

Barotropic Kelvin and Bernoulli with exact hypotheses: for every C2 vector field, (u⋅∇)u=∇(∣u∣2/2)−u×curl⁡u. This is the exact algebraic clause of that theorem used here; no barotropic Bernoulli conclusion is invoked.

[F4]

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.

[F5]

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

1.1givenF1algebra

For r>0, ∂i(1/r)=−xi/r3 and ∂i2(1/r)=−1/r3+3xi2/r5 for i=1,2,3, so Δ(1/r)=−3/r3+3r2/r5=0. Since (U⋅x)/r3=−U⋅∇(1/r), commuting smooth derivatives gives Δ((U⋅x)/r3)=0. Also Δ(U⋅x)=0, so Δϕ=0. Therefore div⁡u=Δϕ=0 and curl⁡u=0 by equality of the mixed second partials of ϕ. Direct differentiation yields u=U+a32r3(U−3(U⋅n)n). This gives uniform u→U at infinity. At r=a, u=(3/2)(U−(U⋅n)n), which is tangent to the sphere and has zero normal component.

2.1givenF2F3step 1.1algebra

By [F3] and curl⁡u=0, (u⋅∇)u=∇(∣u∣2/2). The pressure definition gives ρ0−1∇p=−∇(∣u∣2/2), so the steady momentum equation in [F2] holds; step 1.1 supplies its divergence condition. The explicit formula gives u−U=O(r−1), hence ∣u∣2→∣U∣2 and p→p∞ uniformly in direction.

3.1givenF2F4F5step 1.1constructalgebra∎

The displayed formulas extend smoothly to D since their denominators are powers of r>0. Thus Sa={∣x∣=a}⊂D, and [F2] applies to these stationary spatial fields on this sphere; their restrictions there equal the exterior traces by continuity. On the sphere, u=(3/2)Ut with Ut=U−(U⋅n)n, so ∣u∣2=(9/4)(∣U∣2−(U⋅n)2). Thus p∣r=a depends on n only through (U⋅n)2 and is unchanged by n↦−n. For Φ(θ,φ)=a(sin⁡θcos⁡φ,sin⁡θsin⁡φ,cos⁡θ), 0≤θ≤π, 0≤φ≤2π, direct differentiation gives tangent Gram coefficients E=a2, F=0, G=a2sin⁡2θ, so [F4] gives density EG−F2=a2sin⁡θ (also ∣Φθ×Φφ∣). 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 (θ,φ)↦(π−θ,φ+π mod 2π) has absolute Jacobian one on each half of the longitude interval, preserves the density because sin⁡(π−θ)=sin⁡θ, and induces the antipodal map, which reverses n, so the vector integrand pn has zero integral over the sphere. By the stress convention in [F2], ∫∣x∣=aσEn dS=−∫∣x∣=apn dS=0.

Remarks

The diagram is a two-dimensional cross-section of the sphere. The radial arrow is the outward unit normal n; the tangent arrow indicates the direction of the boundary velocity u=(3/2)Ut. The drawing is schematic and is not used in the field-equation or resultant proof.

diagram failed to render:
\begin{tikzpicture}[scale=1.25]
  \draw[thick] (0,0) circle (1);
  \fill (0,0) circle (0.025);
  \node[below left] at (0,0) {center};
  \fill (0.5,0.866) circle (0.035);
  \draw[->] (0,0) -- (0.5,0.866) node[midway,left] {$n$};
  \draw[->,thick] (0.5,0.866) -- (1.15,0.49) node[right] {$u=\tfrac32U_t$};
  \node at (0.72,0.98) {$r=a$};
  \draw[->] (2.0,0.0) -- (3.0,0.0) node[right] {$U$ at infinity};
\end{tikzpicture}

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