title: Stick-slip instabilities in sheared granular flow: The role of friction and acoustic vibrations.
abstract: We propose a theory of shear flow in dense granular materials. A key ingredient of the theory is an effective temperature that determines how the material responds to external driving forces such as shear stresses and vibrations. We show that, within our model, friction between grains produces stick-slip behavior at intermediate shear rates, even if the material is rate strengthening at larger rates. In addition, externally generated acoustic vibrations alter the stick-slip amplitude, or suppress stick-slip altogether, depending on the pressure and shear rate. We construct a phase diagram that indicates the parameter regimes for which stick-slip occurs in the presence and absence of acoustic vibrations of a fixed amplitude and frequency. These results connect the microscopic physics to macroscopic dynamics and thus produce useful information about a variety of granular phenomena, including rupture and slip along earthquake faults, the remote triggering of instabilities, and the control of friction in material processing.
authors.affiliation: Department of Physics, University of California, Santa Barbara, California 93106, USA.
authors.forename: Charles K C
authors.initials: CK
authors.lastname: Lieou
authors.affiliation: Department of Civil and Environmental Engineering, University of Illinois, Urbana-Champaign, Illinois 61801, USA.
authors.forename: Ahmed E
authors.initials: AE
authors.lastname: Elbanna
authors.affiliation: Department of Physics, University of California, Santa Barbara, California 93106, USA.
authors.forename: J S
authors.initials: JS
authors.lastname: Langer
authors.affiliation: Department of Physics, University of California, Santa Barbara, California 93106, USA.
authors.forename: J M
authors.initials: JM
authors.lastname: Carlson
mesh_terms: D000162:Acoustics; D017276:Friction; D008962:Models, Theoretical; D009038:Motion; D011312:Pressure; D013816:Thermodynamics; D014732:Vibration