Abstract

We consider a particle moving with equation of motion x˙=f(t)\dot x=f(t), where f(t)f(t) is a random function with statistics which are independent of xx and tt, with a finite drift velocity v=⟨f⟩v=\langle f\rangle and in the presence of a reflecting wall. Far away from the wall, translational invariance implies that the stationary probability distribution is P(x)∼exp⁡(αx)P(x)\sim \exp(αx). A classical example of a problem of this type is sedimentation equilibrium, where αα is determined by temperature. In this work we do not introduce a thermal reservoir and αα is determined from the equation of motion. We consider a general approach to determining αα which is not always in agreement with Einstein's relation between the mean velocity and the diffusion coefficient. We illustrate our results with a model inspired by the Boltzmann equation.

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