Use the interior for the Sobolev space notation; the closed shell in the PDF specifies its boundary. Put . A weak solution has zero boundary trace in the sense of the Sobolev trace theorem, equivalently , and satisfiesThe minus sign is necessary because the operator in the paper is positive divergence, not its negative. One can first test with functions and then use density in the zero-boundary Sobolev space. Smoothness of makes its restriction to the compact radial interval bounded, so both sides define continuous functionals on this space. Merely belonging to without the zero trace would omit the boundary condition.
Positivity and continuity of give and a finite maximum . Hence, for every in the shell and every ,This is the uniformly elliptic operator condition. Positivity at separate points without a compactness/continuity lower bound would not alone supply a common ellipticity constant.
Test the weak formulation with itself. Uniform ellipticity and the Cauchy-Schwarz inequality giveThe Poincaré inequality for the bounded shell with zero trace gives . If the gradient is nonzero, divide to obtain ; if it is zero the estimate is immediate and the zero trace forces . ThusThe constant depends on the shell and , not on or . Subtracting two solutions with the same forcing gives a zero-forcing solution and hence proves uniqueness. This is a coercive energy argument, not an appeal to real analytic Cauchy solvability.
A fixed smooth choice already gives a counterexample. Select nonzero smooth functions and with product support compactly contained in a small box inside the shell. LetThen has zero boundary trace and is a classical, hence weak, solution. The norms of are bounded independently of . On the other hand,The squared norm of tends to , by the oscillatory integral identity for . The other term has bounded norm, so grows at least proportionally to . ThereforeThis failure of a coercive Dirichlet estimate under degeneracy loses control in the third direction; it does not rely on varying with the sequence.
For the spherical coordinates in the question, the coordinate tangent vectors are mutually orthogonal, with lengths . Their metric tensor is therefore and the Jacobian determinant is . Applying the divergence formula to the gradient givesFor example, the formula follows directly from for this diagonal metric. These coordinates are valid away from the polar axis and angular seam; the Laplacian is a smooth geometric operator there as well, described by other charts. The coordinate volume form integrates over , , , with the usual periodic identification.
Here is a direct use of the spherical representation that also avoids estimating separate coordinate derivatives at the poles. Put , , and write for unit-sphere area. Then . Expanding its squared norm with the physical measure givesOn each boundary sphere , so every angular derivative, including and , is zero there. Radial and angular integration by parts consequently giveIndeed the term gives with boundary remainder , while the term is , its boundary remainder also being zero. Thuswhere the last step uses the preceding energy estimate and . All unmarked integrals in these two identities are with .
To control every angular second derivative, the spherical Hessian identity isIt follows by integrating the derivative-commutation identity and using on the unit sphere. There is no sphere boundary. Hence the preceding bound controls , , and in their appropriate weighted norms.
In an orthonormal polar frame the Cartesian Hessian matrix has componentsand . Since is bounded above and below, these bounds plus the first-order estimate proveThis is the direct spherical-shell H2 estimate. Intrinsic angular integration combines the suggested angular tests, with no spurious boundary at the polar coordinate singularities.
The coefficients in the spherical Laplacian are independent of , so . Also is tangent to both boundary spheres; differentiating the zero boundary trace gives another zero trace. Therefore satisfies and the same homogeneous Dirichlet boundary conditions.
In Cartesian coordinates , a globally smooth rotation field even where angular coordinates are singular. Permuting coordinate axes gives , and . For each, the rotational commutator for the Laplacian follows directly from ; antisymmetrizing cancels the extra terms. ThusIf is radial, all these right-hand sides vanish. Uniqueness from the energy estimate makes every zero. At each point of a sphere the rotation fields span its tangent plane, so all tangential derivatives of vanish. Each sphere is connected, giving . This proves radiality without assuming it as a separation-of-variables ansatz.
The Sobolev embedding theorem in dimension three, combined with the preceding estimate, givesOne direct justification of this embedding is a bounded Sobolev extension operator into , followed by Fourier inversion and the Cauchy-Schwarz inequality: bounds the inverse Fourier integral by the norm.
For radial forcing, the preceding part makes and . Set , and . The radial equation gives . Both zero boundary values implyMoreover . Since , this proves the radial Poisson gradient estimate:
For a nonradial counterexample choose in the shell and a nonconstant . For sufficiently small , set and . These are smooth with support away from the boundary. Scaling givesThus the failure of L2-to-Linfinity Poisson gradient bounds in three dimensions is explicit, despite the valid and value-supremum estimates.
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