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
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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.