Abstract

We discuss the combined effects of overdamped motion in a quenched random potential and diffusion, in one dimension, in the limit where the diffusion coefficient is small. Our analysis considers the statistics of the mean first-passage time T(x) to reach position x, arising from different realisations of the random potential. Specifically, we contrast the median {bar{T}}(x), which is an informative description of the typical course of the motion, with the expectation value langle T(x)rangle , which is dominated by rare events where there is an exceptionally high barrier to diffusion. We show that at relatively short times the median {bar{T}}(x) is explained by a ‘flooding’ model, where T(x) is predominantly determined by the highest barriers which are encountered before reaching position x. These highest barriers are quantified using methods of extreme value statistics.

Highlights

  • There are many situations where particles move under the combined influence of thermal diffusion and a static random potential [1]

  • V (x) is a random potential, D is the diffusion coefficient, and η(t) is a white noise signal with statistics defined by η(t) = 0, η(t)η(t ) = δ(t − t )

  • We note that the central limit theorem is applicable to the quantity T (x) obtained by equation (9) in the limit as x → ∞, so that x2/2T (x) does approach a limit, which we identify as the effective diffusion coefficient

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Summary

Introduction

There are many situations where particles move under the combined influence of thermal diffusion and a static (or quenched) random potential [1]. Page 3 of 18 54 has been extended to consider a periodised random potential, so that the long-time dynamics is diffusive: in this case it is found [12] that the diffusion coefficient has a very broad probability distribution, and these studies have inspired other works on dispersion in the presence of traps, of which [13] is a recent example Another related problem is the motion of a quantum particle in a statistically homogeneous random potential which exhibits even slower spatial dispersion: it may be completely localised [14], and in one or two dimensions localisation is almost certain [15,16]: see [17] for a review. After a sufficiently long time, the dynamics becomes diffusive, with a diffusion coefficient given by (5)

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The Mean First Passage Time
Expression for Expectation Value of Mean First Passage Time
Summation Approximations
Statistics of Extreme-Weighted Sums
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Interpretation and Generalisation to TN
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Flooding Dynamics Model for Dispersion
Numerical Studies
Discrete Sums
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Conclusions
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Full Text
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