Vary each field component independently and integrate the gradient term by parts, taking fixed boundary values or vanishing surface variations. With , the Euler-Lagrange equations for the free-energy saddle are
The anisotropy shifts the first two inverse susceptibilities in opposite directions. The derivative of is , which fixes the factor needed for both the magnetization and the free energies in c. Under natural free-boundary conditions the integration by parts instead supplies at the surface.

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