Mean field theory
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A many-body system with interactions is generally very difficult to solve exactly, except for extremely simple cases (Gaussian field theory, 1D Ising model.) The great difficulty (e.g. when computing the partition function of the system) is the treatment of combinatorics generated by the interaction terms in the Hamiltonian when summing over all states. The goal of mean field theory (MFT, also known as self-consistent field theory) is to resolve these combinatorial problems.
The main idea of MFT is to replace all interactions to any one body with an average or effective interaction. This reduces any multi-body problem into an effective one-body problem. The ease of solving MFT problems means that some insight into the behavior of the system can be obtained at a relatively low cost.
In field theory, the Hamiltonian may be expanded in terms of the magnitude of fluctuations around the mean of the field. In this context, MFT can be viewed as the "zeroth-order" expansion of the Hamiltonian in fluctuations. Physically, this means a MFT system has no fluctuations, but this coincides with the idea that one is replacing all interactions with a "mean field". Quite often, in the formalism of fluctuations, MFT provides a convenient launch-point to studying first or second order fluctuations.
In general, dimensionality plays a strong role in determining whether a mean-field approach will work for any particular problem. In MFT, many interactions are replaced by one effective interaction. Then it naturally follows that if the field or particle exhibits many interactions in the original system, MFT will be more accurate for such a system. This is true in cases of high dimensionality, or when the Hamiltonian includes long-range forces. The Ginzburg criterion is the formal expression of how fluctuations render MFT a poor approximation, depending upon the number of spatial dimensions in the system of interest.
While MFT arose primarily in the field of Statistical Mechanics, it has more recently been applied elsewhere, for example for doing Inference in Graphical Models theory in artificial intelligence.
Formal approach
The formal basis for mean field theory is the Bogoliubov inequality. This inequality states that the free energy of a system with Hamiltonian
- [\mathcal=\mathcal_+\Delta \mathcal]
- [F \leq F_ \equiv \langle \mathcal \rangle_ -T S_]
- [\mathcal_=\sum_^h_\left( \xi_\right)]
For the most common case that the target Hamiltonian contains only pairwise interactions, i.e.,
- [\mathcal=\sum_}V_\left( \xi_,\xi_\right)]
[F_ = \,\!] [_\mathcal(\xi_,\xi_,...,\xi_)P^_(\xi_,\xi_,...,\xi_)] [+kT \,_P^_(\xi_,\xi_,...,\xi_)\log P^_(\xi_,\xi_,...,\xi_)] where [P^_(\xi_,\xi_,...,\xi_)] is the probability to find the reference system in the state specified by the variables [(\xi_,\xi_,...,\xi_)]. This probability is given by the normalized Boltzmann weight
- [P^_(\xi_,\xi_,...,\xi_)=\frac_}e^_(\xi_,\xi_,...,\xi_)}=\prod_^\frac}e^\left( \xi_\right)}\equiv \prod_^ P^_(\xi_)].
- [F_=\sum_} _V_\left( \xi_,\xi_\right)P^_(\xi_)P^_(\xi_)+kT \sum_^ _ P^_(\xi_) \log P^_(\xi_).]
- [P^_(\xi_)=\frac}e^^(\xi_)}\qquad i=1,2,..,N]
- [h_^(\xi_)=\sum_\}}Tr_V_\left( \xi_,\xi_\right)P^_(\xi_)]
Example
Consider the Ising model on an N-dimensional cubic lattice. The Hamiltonian is given by
- [ H = -J \Sigma^ \mathbf \mathbf} ]
Let's transform our spin variable by introducing the fluctuation from its mean value [ \langle\mathbf\rangle ]. We may rewrite the Hamiltonian:
- [ H = -J \Sigma^ (\mathbf) (\mathbf)+ \langle s_\rangle}) ]
If fluctuations are small, we may neglect this last term. As per the above arguments, when the fluctuations are small, then MFT should work 'better', from an intuitive stand-point.
- [ H \approx -J \Sigma^ (\mathbf\rangle }) ]
- [ \mathbf\rangle} ]
- [ \mathbf\rangle} ]
We are still stuck with a double summation over neighboring spins, yet the summand involves only one site of each neighbor. Roughly speaking, we count 2d bonds (where d is the dimensionality of the cubic lattice) for each site. But since each bond participates in two spins, we would be overcounting by a factor of 2 if we gave each site a multiplicity of 2d. Therefore, the Hamiltonian becomes
- [ H = -2dJ\langle\mathbf\rangle \Sigma_i \mathbf ]
Substituting this Hamiltonian into the partition function, and solving the effective 1D problem, we obtain
- [ Z = (2 \cosh(\frac \langle \mathbf\rangle))^ ]
MFT is known under a great many names and guises. Similar techniques include Bragg-Williams approximation, Bethe approximation, Landau theory, and Flory-Huggins solution theory.
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