Classical Heisenberg model
- Classical Heisenberg model
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The Classical Heisenberg model is the n = 3 case of the n-vector model, one of the models used in statistical physics to model ferromagnetism, and other phenomena.
Definition
It can be formulated as follows: take a d-dimensional lattice, and a set of spins of the unit length
- ,
each one placed on a lattice node.
The model is defined through the following Hamiltonian:
with
a coupling between spins.
Properties
- Polyakov has conjectured that, in dimension 2, as opposed to the classical XY model, there is no dipole phase for any T > 0; i.e. at non-zero temperature the correlations cluster exponentially fast.[1]
- The general mathematical formalism used to describe and solve the Heisenberg model and certain generalizations is developed in the article on the Potts model.
- In the continuum limit the Heisenberg model (2) gives the following equation of motion
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- This equation is called the continuous classical Heisenberg ferromagnet equation or shortly Heisenberg model and is integrable in the soliton sense. It admits several integrable and nonintegrable generalizations like Landau-Lifshitz equation, Ishimori equation and so on.
See also
References
External links
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