Fokker Planck equation

23 October 2012

Description

The Fokker Planck equation has the form

tϱ(x,t)=(β1ϱ(x,t)+ϱ(x,t)H(x)),ϱ(x,0)=ϱ0(x), \partial_t \varrho(x,t) = \nabla \cdot \bigl(\beta^{-1} \nabla \varrho(x,t) + \varrho(x,t) \nabla H(x)\bigr) ,\qquad \varrho(x,0)=\varrho_0(x) ,

where H:RnRH:\R^n\to \R is a smooth function, β>0\beta>0 some parameter and ϱ0\varrho_0 a probability density on Rn\R^n . The partial differential equation is in divergence form and conserves mass. Hence, also ϱ(,t)\varrho(\cdot,t) is a probability density on Rn\R^n . In the case, where HH has some growth at \infty , the equilibrium solutions ϱ:RnR\varrho_\infty:\R^n \to \R are characterized by

βϱ+ϱH=0 \beta \nabla \varrho_\infty + \varrho_\infty \nabla H =0

leading to the solution

ϱ(x)=Z1eβH(x)withZ=eβH(x)  dx \varrho_\infty(x) = Z^{-1} e^{-\beta H(x)} \quad \text{with} \quad Z = \int e^{-\beta H(x)} \; \dx x


The density ϱ\varrho_\infty is called Gibbs distribution, which accounts to the fact, that it minimizes the (Gibbs) free energy

F(ϱ)=E(ϱ)+β1S(ϱ) F(\varrho) = E(\varrho) + \beta^{-1} S(\varrho)

where EE is the energy and SS the (Gibbs-Boltzmann) entropy

E(ϱ):=Hϱ  dxandS(ϱ):=ϱlogϱ  dx. E(\varrho) := \int H \varrho\;\dx x \quad\text{and}\quad S(\varrho) := \int \varrho \log \varrho \; \dx{x} .

By this formulation  β\beta plays the role of the inverse temperature. Note, that the Euler-Lagrange equation is given by

H(x)+β1(ϱ(x)+1)=0, H(x) + \beta^{-1} \bigl(\varrho(x) + 1\bigr) = 0 ,

which is solved by ϱ\varrho_\infty .

Pathwise formulation via stochastic differential equations

The stochastic process X(t)X(t) defined by

dX(t)=H(X(t))  dt+2β1  dW(t),X(t)=X0, \dx X(t) = - \nabla H(X(t))\;\dx t + \sqrt{2\beta^{-1}} \;\dx W(t) , \quad X(t) = X_0 ,

where W(t)W(t) is an nn -dimensional Brownian motion, is the pathwise formulation of the Fokker Planck equation. If distribution of the initial random vector X0X_0 is given by law  X0=ϱ0\mathrm{law}\; X_0 = \varrho_0 , then at later times the solution X(t)X(t) has distribution law  X(t)=ϱ(,t)\mathrm{law}\; X(t) = \varrho(\cdot,t) , where ϱ\varrho is solution of the Fokker Planck equation.

The dynamic of the pathwise formulation undergoing diffusion in the potential HH . The particle is solely described by its position X(t)RnX(t)\in \R^n , i.e. inertia is neglected. Then, the particle chooses the steepest descent with respect ot HH , which is perturbed by random fluctuation, which are assumed to be normal distributed. The coupling parameter β\beta describing the strength of the fluctuations plays again the role of inverse temperature. In particular, the limit β\beta\to \infty describes the behaviour of the system without fluctuations.

Ornstein-Uhlenbeck process

A prominent example, which can be explicitly solved, is the Ornstein-Uhlenbeck process, corresponding to the choice

H(x)=γ2x2. H(x) = \frac{\gamma}{2} | x |^2 .

The stationary distribution is given by the Gaussian

ϱ(x)=(2πγβ)n2exp(γβx22). \varrho_\infty(x) = \left( \frac{2\pi}{\gamma\beta} \right)^{-\frac{n}{2}} \exp\left(-\frac{\gamma \beta |x|^2}{2}\right) .

The underlying picture becomes particular simple in one dimension. There, the leading order behaviour of the process can be characterized by its mean m(t)m(t) and variance σ(t)\sigma(t) , which are given by

m(t):=xϱ(x,t)  dxandσ(t):=(xm(t))2ϱ(x,t)  dx=x2ϱ(x,t)  dxm(t)2. m(t) := \int x \varrho(x,t) \;\dx x \qquad\text{and}\qquad \sigma(t) := \int (x-m(t))^2 \varrho(x,t) \;\dx{x} = \int x^2 \varrho(x,t)\; \dx{x} - m(t)^2 .

Both, m(t)m(t) and σ(t)\sigma(t) , satisfy an ordinary differential equation not depending on ϱ\varrho

m˙(t)=γm(t)ands˙igma(t)=2β12γσ(t). \dot m(t) = -\gamma m(t) \qquad \text{and}\qquad \dot sigma(t) = 2\beta^{-1} - 2\gamma \sigma(t) .

Hence, the mean converges exponentially fast to 00 with rate γ\gamma and the variance converges exponentially fast from the initial variance σ(0)\sigma(0) to (βγ)1(\beta \gamma)^{-1} with rate 2γ2 \gamma

m(t)=m(0)  e2γtandσ(t)=σ(0)e2γt+1βγ(1e2γt). m(t) = m(0) \; e^{-2\gamma t} \qquad\text{and}\qquad \sigma(t) = \sigma(0) e^{-2\gamma t} + \frac{1}{\beta \gamma} \bigl(1-e^{-2\gamma t}\bigr) .

Numerical example

For general potentials HH explicit solutions of the Fokker Planck equation are not available. However, the pathwise formulation allows to do Monte-Carlo simulation of single realisations of the process X(t)X(t) . The case, where HH is not convex is especially interessting, because at low temperature, i.e. β1\beta \gg 1 , the process shows metastable behaviour.

Therefore, we consider the potential function H:R2RH:\R^2 \to \R looking like

The realization of the process X(t)X(t) for increasing values of β\beta :

Monte Carlo simulation for Fokker Planck equation β=2.5\beta=2.5

Monte Carlo simulation for Fokker Planck equation β=5\beta=5

Monte Carlo simulation for Fokker Planck equation β=10\beta=10

Monte Carlo simulation for Fokker Planck equation β=20\beta=20 (red β=\beta=\infty )

For increasing values of β\beta the particle goes quickly to the local minima and is trapped there longer and longer times. The transition to the global energy minimizing state happens along a path crossing the saddle. This behaviour is called metastable. For the limiting dynamic β=\beta=\infty without any fluctuation a transition is not possible and the particle is stuck in the local minima.

References

  1. R. Jordan, D. Kinderlehrer, and F. Otto, “The Variational Formulation of the Fokker-Planck Equation,” SIAM Journal on Mathematical Analysis, vol. 29, no. 1, 1998.