An isotropic spin-polarized metal has a degenerate magnetization direction and a long-wavelength transverse magnon with quadratic dispersion. Nonzero spin density pairs the two transverse broken generators into one type-B Goldstone boson. Exchange-split Fermi surfaces also support fermionic low-energy excitations; the magnon is distinct from longitudinal amplitude motion and the spin-flip continuum.
Use dimensionless spin angular momentum operators, so their commutators have no additional . A fully polarized state is an exact ground state of the Heisenberg ferromagnet, with . On each bond the largest eigenvalue of is , obtained in the two-spin total-spin- sector. Hence the bondwise lower bound on the Hamiltonian is attained by this state.
The ferromagnetic ground-state multiplet has total spin . Applying the global lowering operator , , generates its magnetic states; their linear combinations are also ground states. Global spin rotations generate polarized ground states pointing in arbitrary directions and span the same multiplet. Uniform reorientation therefore costs no energy. Slowly varying orientations give gapless ferromagnetic magnons, with quadratic rather than linear long-wavelength dispersion. In the ordered thermodynamic ground state, the two broken spin generators are canonically paired because , producing one type-B Goldstone boson. For a finite chain the zero-wavevector motion remains inside the exact ground multiplet; nonzero wavevectors have a finite-size spacing that vanishes as . This is a ground-state statement, not a claim of finite-temperature long-range order in one dimension.
Use with , choosing distinct values modulo in the Brillouin zone. The lattice spacing is one; for spacing the dimensionless variable here would be . Orthogonality of the discrete Fourier modes diagonalizes the bilinear Hamiltonian:
This is the nearest-neighbour ferromagnetic magnon dispersion. The printed expression is missing a factor of four for the stated exchange Hamiltonian. If denotes a physical frequency, ; setting does not remove that factor. The printed coefficient would require an exchange constant in the original Hamiltonian.
An independent check uses one spin lowering at site . The exact one-magnon Hamiltonian relative to has diagonal element and off-diagonal elements at , giving the same Fourier eigenvalue. At small , , and the state belongs to the degenerate ground multiplet. The quadratic low-energy branch is the ferromagnetic type-B Goldstone boson.
The spin-independent term cancels in the signed sum. The linearized stationary equation becomes
The even powers vanish because the equation is odd under . Equivalently, the mean-field action has curvature
Thus the unpolarized stationary point becomes unstable when
At low temperature, the derivative of the Fermi distribution samples a narrow window around , so for a smooth density of states. Measuring energy from the Fermi level gives , the Stoner criterion in the spin-summed convention fixed above. This identifies local instability of the paramagnetic state; the detailed transition order also depends on higher terms in the action.
In the isotropic ordered phase of itinerant ferromagnetism, continuous spin-rotation symmetry leaves a degenerate direction of magnetization. Its transverse fluctuations produce one gapless, quadratically dispersing mean-field itinerant ferromagnetic Goldstone mode, . The two broken spin generators form a canonical pair, as for the type-B Goldstone boson of the localized ferromagnet. The system also remains metallic, with exchange-split Fermi surfaces and low-energy spin-conserving particle-hole excitations. Longitudinal-amplitude fluctuations and the spin-flip continuum are distinct from the long-wavelength magnon; their energy and damping scales depend on the band structure. Spin anisotropy, if added, could gap the transverse mode, but it is absent from the stated Hamiltonian.