Let , , and . Applied forces and couples below are forces and torques on the solid; by force balance their values are also the strengths exerted by that solid on the fluid. This fixes the signs in Faxén's first law and Faxén's rotational law. To hold the passive sphere fixed, set its translation and angular velocity to zero in those laws. The incident two-mode tensorial squirmer flow gives
Only the stresslet part has vorticity:
Consequently, for fixed as ,
The leading force is the radial stresslet force. Its next correction, , comes from the incident potential dipole. The next correction, , contains both the swimmer's field and the Laplacian term in Faxén's first law. If the relevant coefficient vanishes, these next terms must be retained instead of calling the vanished term a nonzero leading approximation. Further exchanges in the method of reflections for Stokes flow are smaller still.
The passive sphere reflects primarily a Stokeslet with strength . At the swimmer, its velocity is . The unchanged surface slip velocity adds the free swimming velocity to the incident-flow contribution in Faxén's first law. Thus
The leading change is ; its next correction is the displayed term. Finite-radius Faxén's first law corrections, the passive sphere's reflected stresslet, and its rotlet contribute at order to translation.
For a Stokeslet at the origin,
The curl of the first term is ; that of the second is also , before multiplying by . Hence . At the swimmer use displacement . The leading force is parallel to , so its Stokeslet has zero vorticity there. This eliminates the putative rotation. The potential dipole itself has no vorticity, but the holding force it induces is not radial. Applying Faxén's rotational law to its reflected Stokeslet yields
The passive sphere's rotlet and reflected stresslet can affect that last order, so they cannot restore the larger missing rotation. When , the boxed coefficient is zero and the higher-order terms determine any rotation.
Take and . Taking the divergence of the Stokes flow momentum equation gives ; applying the Laplacian to its vertical component then eliminates pressure and gives . The forced velocity and temperature are , so their advection product is and drops out at leading order. The steady heat equation reduces to .
Consequently the boundary value problem for the forced profiles is
Its six boundary conditions are
The horizontal velocity field is , which directly verifies the incompressible flow and stress-free boundary condition. In the detuning used subsequently, may be replaced by in this leading problem, since its correction enters at order . The vertical profiles depend linearly on .
For reference, the unforced free-slip convection neutral curve is , with and . At the neutral curve has , so the forced second horizontal harmonic is noncritical at , and the stated linear problem has no critical-mode resonance.
Take the layer depth as the length unit, its thermal diffusion time as the time unit, and its imposed temperature difference as the temperature unit. Then is the velocity field, the pressure after the conductive hydrostatic pressure has been subtracted, the departure from the conductive temperature , the upward unit vector, and the Rayleigh number. Here is the dimensional depth, the kinematic viscosity, the thermal diffusivity and the thermal expansion coefficient. The gradient, divergence and Laplacian act on the dimensionless coordinates. The term in the heat equation is advection of the background gradient, since . Mass density variations enter only the buoyancy term under the Boussinesq approximation; the incompressible flow constraint is .
For fixed, impermeable, stress-free plates, the no-penetration boundary condition, stress-free boundary condition and perfectly conducting thermal boundary condition are
For a nonzero horizontal Fourier mode, incompressibility gives , so the velocity conditions are equivalently on both plates. A uniform horizontal velocity is not fixed by these boundary conditions; take its mean to be zero when discussing the stationary forced pattern.
The printed small-Prandtl-number label does not generally justify these equations. In thermal-time units the full momentum equation contains , where the Prandtl number is . Dropping that term gives infinite-Prandtl-number convection or another explicitly justified Stokes flow approximation. It is not the general limit. For example the horizontal shear , , satisfies the full linear momentum equation and the plate conditions, and persists at fixed as . The printed inertia-free equation would instead require this shear to vanish. The following parts solve the equations actually displayed; applying them at small Prandtl number needs an additional slaving or creeping-flow ordering.
For Darcy-Bénard convection, the dimensionless Darcy law is , with incompressibility and a heat equation about . Here is a Darcy thermal-time Rayleigh number, with permeability replacing the squared-depth dependence in the fluid-layer Rayleigh number. The stated stream function convention gives , so . The vertical-plane curl of Darcy law gives ; omitting the quadratic perturbation advection from the heat equation gives .
On the impermeable connected square boundary, zero normal velocity makes constant along the boundary; choose that constant as zero. The prescribed conductive boundary temperature fixes on all four sides. Thus the perfect-conductor wording is interpreted through the supplied homogeneous perturbation data: the side temperatures retain the background vertical profile, rather than imposing a different isothermal side state.
At marginal stability put and . The two coupled equations imply
The gauge transformation for conducting-square Darcy onset removes the first derivative:
The square's Dirichlet Laplacian eigenfunctions are , with eigenvalues of equal to , . The first marginal value is therefore
It is genuinely the first instability threshold, not just an isolated neutral value. Eliminating gives the temperature linear operator , where is the Dirichlet realization of an elliptic operator for the Laplacian. Integration by parts shows the second term is self-adjoint and nonnegative, since its quadratic form is . Thus the spectrum is real, starts negative at , and its leading eigenvalue cannot cross into growth without a zero eigenvalue. The smallest zero value is the one found above.
Let , and . Multiplying the lowest real by independent real and imaginary constants gives two real physical eigenfunctions:
The subscripts indicate even and odd parity about . Because is even in , the first has even and odd , while the second reverses those parities. They are linearly independent and satisfy all four Dirichlet boundary conditions. The lowest complex eigenfunction is simple over the complex numbers, but its arbitrary complex multiplier supplies two independent real pairs; this explains the physical degeneracy.
Figure 1.
Neutral and oscillatory modes in porous convection
. Details.
The conclusion holds in dimension two. Shift and change sign to obtain a nonnegative harmonic function . Its circular mean satisfies
Here the angular second derivative in the polar-coordinate Laplacian integrates to zero. Thus ; nonnegativity for every forces . For , the mean value property for harmonic functions and nonnegativity give
The removable singularity for a bounded harmonic function fills in the origin, and the harmonic Liouville theorem makes the extension constant.
The conclusion fails for : is positive and nonconstant, and its radial Laplacian vanishes away from zero. For , is a nonconstant function bounded below whose second derivative vanishes on both components of the punctured line.
Let , so has zero Dirichlet boundary condition. Using the supplied form of the minimal surface equation for a graph, set
For and , the difference bound implies
and
The shifted arguments stay in the permitted radius-two ball, and . The Laplacian with zero Dirichlet boundary condition has trivial null space by the maximum principle for harmonic functions. Choose small enough that and , for the constants in part (c) with . Its small-data existence for a nonlinear elliptic Dirichlet problem supplies , and solves the minimal surface equation for a graph with the required boundary values.
Put and write the Riemannian metric as a conformal rescaling of a Riemannian metric:
The base metric is flat, so its Ricci scalar is zero and its Laplacian is . The formula for scalar curvature under conformal rescaling simplifies in dimension two to
Differentiate explicitly:
Since , the required Ricci scalar is
The same polytrope of index one interior equation is . A positive separated solution with zero density on all six cube faces is the cubic polytropic interior
Its Laplacian is , so the required side length is
With and , it satisfies the interior hydrostatic equilibrium and Poisson equation for Newtonian gravity. Integrating each sine factor yields
This formal interior solution is not an isolated physical cubic star. The cubic polytrope fails isolated gravitational matching: at a vertex, the product of sines has , so the interior potential predicts zero gravitational acceleration. At the vertex , however, the field generated by its own positive mass is
and each component is strictly positive. There can be no continuous matching to the isolated external field without additional forces or mass sources. Thus solving the interior density equation and imposing zero face values is insufficient. Fluid stars also have no rigid structure to maintain sharp cubic faces, and observed stellar shapes are approximately spherical or rotationally flattened rather than cubic.
The zero streamfunction gives zero velocity. The temperature obeys both prescribed temperature values, has no horizontal gradient, and has zero Laplacian. Thus it satisfies both equations with :
This is the conductive state of Darcy-Bénard convection.
Put . The noises required by a joint trajectory are and . Their independent Gaussian white noise weights give the joint path probability of an order parameter and its flux:
For the physically reversed path, is time-even and the transport flux is time-odd. Therefore , , and
The common factor includes the two noise normalizations and the midpoint Jacobian determinant. Its calculation must include both relaxation channels. On a finite spatial grid, let and represent the divergence and gradient, with the discrete Laplacian, and let be the Hessian matrix of at the midpoint of time step . Differentiating the two required noises with respect to the next configuration and the interval flux gives the Jacobian matrix
Using the Schur complement, its Jacobian determinant, apart from the path-independent power of , is
Reversal visits the same midpoint configurations in reverse order, so the product of these factors is unchanged. The joint time-reversal invariance of a path Jacobian therefore involves the complete relaxation operator .
Taking the action difference gives
Repeated component indices are summed. The second squared norm sums over both flux indices. This is mixed conserved and nonconserved order-parameter dynamics; reversing the order parameter history while leaving the flux unreversed would give the wrong probability ratio.
Applying the Laplacian to and using gives
For
one therefore has
Together with part (i), these are the Stokes equations, so the fields form the Unscaled Papkovich–Neuber representation.
Suppose are solutions and put . Then and satisfies the homogeneous Robin boundary condition
For , Green's first identity gives
The left side is nonnegative, so both sides vanish and . For , the Dirichlet boundary condition on and the same identity again imply . The solution is therefore unique for every .
For a regular spherically symmetric solution, the Laplacian equation is
Regularity at the origin gives , hence . Applying the boundary condition at yields
At the Neumann boundary condition would require , which is impossible for . Equivalently, its compatibility condition would require .
Computing the Laplacian gives
and
Thus Laplace's equation holds exactly when
For ,
so
One suitable analytic function is therefore
The magnetic field is . The magnetostatic Ampère-Maxwell equation is , so the curl of the curl identity gives
A gauge transformation does not change . We may therefore choose the Coulomb gauge by solving the Poisson equation . It follows component by component in a Cartesian coordinate system that
The free-space Green function of the Laplacian then gives
For a localized steady current density, conservation of electric charge gives ; integration by parts confirms directly that this integral has zero divergence and hence obeys the Coulomb gauge.
Let the displayed integrand be . Since it has no explicit dependence on or , the Euler-Lagrange equations for two fields are
Its derivatives are
Thus
Using the Laplacian, gradient, and divergence, these combine into the static Navier-Cauchy equation
On a relatively compact ball, mollification commutes with the Laplacian, so is a smooth harmonic function. Repeated interior derivative estimates, together with the Caccioppoli inequality, bound every derivative of on a smaller ball by the local norm of , uniformly as . The Arzelà-Ascoli theorem and a diagonal argument give a smooth local limit, while mollification gives in . Thus the limit equals almost everywhere. After choosing this smooth representative, is harmonic pointwise. This is the Weyl lemma for an weak solution.
For in two dimensions,
Thus the Laplacian satisfies , and the isotropic harmonic-oscillator operator gives
For Maxwell theory the group is Abelian, so write . The reduced equation loses its commutators and becomes
Since the Euclidean Laplacian is
the anti-self-dual Maxwell equations in this gauge are equivalent to
The multivariable chain rule first gives
Taking a second partial derivative in each variable, with the partial derivatives of evaluated at , gives
The mixed partial derivatives cancel even without using their equality. Hence the Laplacians satisfy
Away from the origin the factor is positive, so is a harmonic function if and only if is a harmonic function on the corresponding local coordinate patch. This is the Laplacian in planar parabolic coordinates.
If two solutions exist, their difference satisfies inside and on the boundary. Suppose has a positive value. Continuity on the closed ball gives a positive maximum at an interior point, where the Hessian matrix is negative semidefinite and hence . But the equation gives , a contradiction. A negative minimum similarly contradicts .
Thus , proving uniqueness by the maximum principle for the modified Helmholtz equation. Here a classical solution is understood to be inside and continuous up to the boundary; mere first differentiability would not define the displayed Laplacian classically. With enough boundary regularity, the alternative Green's first identity proof is .