Abstract
We consider a particle moving with equation of motion , where is a random function with statistics which are independent of and , with a finite drift velocity and in the presence of a reflecting wall. Far away from the wall, translational invariance implies that the stationary probability distribution is . A classical example of a problem of this type is sedimentation equilibrium, where is determined by temperature. In this work we do not introduce a thermal reservoir and is determined from the equation of motion. We consider a general approach to determining 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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