Abstract
Coarse-grained simulations are often employed to study the translocation of DNA through a nanopore. The majority of these studies investigate the translocation process in a relatively generic sense and do not endeavour to match any particular set of experimental conditions. In this manuscript, we use the concept of a Péclet number for translocation, , to compare the drift-diffusion balance in a typical experiment vs a typical simulation. We find that the standard coarse-grained approach over-estimates diffusion effects by anywhere from a factor of 5 to 50 compared to experimental conditions using dsDNA. By defining a coarse-graining parameter, , we are able to correct this and tune the simulations to replicate the experimental (for dsDNA and other scenarios). To show the effect that a particular can have on the dynamics of translocation, we perform simulations across a wide range of values for two different types of driving forces: a force applied in the pore and a pulling force applied to the end of the polymer. As brings the system from a diffusion dominated to a drift dominated regime, a variety of effects are observed including a non-monotonic dependence of the translocation time on and a steep rise in the probability of translocating. Comparing the two force cases illustrates the impact of the crowding effects that occur on the trans side: a non-monotonic dependence of the width of the distributions is obtained for the in-pore force but not for the pulling force.
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