The Prandtl-Tomlinson model of friction with stochastic driving
arXiv:1709.09604 · doi:10.1088/1742-5468/aa9db2
Abstract
We consider the classical Prandtl-Tomlinson model of a particle moving on a corrugated potential, pulled by a spring. In the usual situation in which pulling acts at constant velocity , the model displays an average friction force that relates to (for small as , where is a critical friction force. The possible values of are well known in terms of the analytical properties of the corrugated potential. We study here the situation in which the pulling has, in addition to the constant velocity term, a stochastic term of mechanical origin (i.e, the total driving is a function of ). We analytically show how this term modifies the force-velocity dependence close to the critical force, and give the value of in terms of the analytical properties of the corrugation potential and the scaling properties of the stochastic driving, encoded in the value of its Hurst exponent.
arXiv comment8 pages, 8 figures
References in corpus (5)
- Persistence and First-Passage Properties in Non-equilibrium Systems
- Collective Transport: From Superconductors to Earthquakes
- Nonequilibrium Dynamics of Interfaces and Lines
- Inertia and universality of avalanche statistics: The case of slowly deformed amorphous solids
- Different universality classes at the yielding transition of amorphous systems
Cited by in corpus (11)
- Criticality in elastoplastic models of amorphous solids with stress-dependent yielding rates
- Deformation and flow of amorphous solids: An updated review of mesoscale elastoplastic models
- On the critical exponents of the yielding transition of amorphous solids
- Two step micro-rheological behavior in a viscoelastic fluid
- The yielding of amorphous solids at finite temperatures
- Elastic interfaces on disordered substrates: From mean-field depinning to yielding
- Properties of the density of shear transformations in driven amorphous solids
- Adjoint-based calibration of nonlinear stochastic differential equations
- Discontinuous yielding transition of amorphous materials with low bulk modulus
- Soil creep facilitated by cyclic variations of environmental conditions
- Emergence of a random field at the yielding transition of a mean-field Elasto-Plastic model