Model for the erosion onset of a granular bed sheared by a viscous fluid.

We study theoretically the erosion threshold of a granular bed forced by a viscous fluid. We first introduce a model of interacting particles driven on a rough substrate. It predicts a continuous transition at some threshold forcing θ_{c}, beyond which the particle current grows linearly J∼θ-θ_{c}. The stationary state is reached after a transient time t_{conv} which diverges near the transition as t_{conv}∼|θ-θ_{c}|^{-z} with z≈2.5. Both features are consistent with experiments. The model also makes quantitative testable predictions for the drainage pattern: The distribution P(σ) of local current is found to be extremely broad with P(σ)∼J/σ, and spatial correlations for the current are negligible in the direction transverse to forcing, but long-range parallel to it. We explain some of these features using a scaling argument and a mean-field approximation that builds an analogy with q models. We discuss the relationship between our erosion model and models for the plastic depinning transition of vortex lattices in dirty superconductors, where our results may also apply.