The classical Heisenberg model assigns a three-component unit vector to each site and couples pairs by their dot product. Positive favors parallel alignment. With no applied magnetic field or anisotropy, simultaneous rotations of all vectors preserve the energy, so an ordered state chooses a direction and exhibits spontaneous symmetry breaking. The vector order parameter is the spatially averaged orientation. A quartic Landau free energy describes its mean-field onset near a continuous transition; fluctuations can change the critical exponents.[ref]
For unit three-component classical spins and energy on a lattice of coordination , mean-field decoupling gives . Integrating each spin over solid angle yields
The constant term corrects double counting. A normalized angular measure removes but does not change the self-consistency equation. The lattice dimension and spin-space dimension are different data.
The single-site average in molecular field is , where . Thus with . The small- slope gives . On a square lattice . This finite mean-field transition does not imply actual positive-temperature magnetization for the ideal two-dimensional short-range isotropic model, where the Mermin-Wagner theorem applies.

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The Classical Heisenberg model is a theoretical framework used to describe the magnetic properties of a system of spins (or magnetic moments) arranged on a lattice. It is based on the concepts of classical mechanics and statistical mechanics, and it provides insights into phenomena such as ferromagnetism and antiferromagnetism.