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Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics Experiments and Computer Simulations Identical particles, collisional regime, ‘ergodic’ uniform energy injection Outline: • Describe apparatus and simulation • Phase transitions in the absence of shear • Shear profiles: effect of friction • Wall slip instability at high shear? • Conclusions and Acknowledgements

Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

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Page 1: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ.

Investigations of granular thermodynamics and hydrodynamicsExperiments and Computer Simulations

Identical particles, collisional regime, ‘ergodic’ uniform energy injection

Outline:• Describe apparatus and simulation• Phase transitions in the absence of shear• Shear profiles: effect of friction• Wall slip instability at high shear?• Conclusions and Acknowledgements

Page 2: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Apparatus

A sin(t)

Camera

h ~1.7 ball diameters

shaker

Light source

Accelerometer

~10,000 1.6 mm diameter stainless steel spheres 0.5% uniformity

• Shake hard no gravitational settling, collisional regime, ‘ergodic’

MD simulation 3 parameters: Elastic restoring force, Dissipative normal force, tangential friction(X. Nie, et al., EPL ‘00; A. Prevost, et al, PRL ‘02)

Page 3: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Crystal-liquid coexistence

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Experiment MD SimulationRed: Sphere in top half of cellBlue: Bottom half

Page 4: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Square or hexagonal symmetry?

When close-packed, 2 square layers are 1.6 high hexagonal are 1.8

Page 5: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Different Phases at different gap spacings (simulations)

A) H=1.3, 1 hexagonal B) H=1.5, buckledC) H=1.7, 2 squareD) H=1.9, 2 hexagonal

Red: Sphere in top half of cellBlue: Bottom half

Observed phases represent efficient packings

Page 6: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Same Phases O`bserved in ColloidsParticles suspended in fluid in equilibrium

ColloidsSchmidt & Lowen, PRE ‘97 (MD, Analytic)

Equilibrium transition driven by entropy maximization

Granular MDJPCM 17, S2689 (2005)

See also J.S Olafsen, JSU, PRL (2005) and P. M. Reis, R.A. Ingale, and M.D. Shattuck, PRL (2006).

Page 7: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Granular Temperature

SOLID

LIQUID

Experiment Simulation

Granular temperature does not obey ‘zeroth law’Increased dissipation in solid -> higher density

-> larger coexistence region

Mean square fluctuating horizontal velocities

Page 8: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Shaking and shearing

Page 9: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Shaking and Shearing• Test granular hydrodynamics with independent control of shear rate and collision rate• Couette geometry - known velocity profile for simple fluids• Use ‘rough walls’ to minimize slipping

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Page 10: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Angular velocity profiles• Varying shear (Δ: 100 rpm,▲: a=175 rpm,■: a=250 rpm).

• Varying shaking amplitude Varying Material

• (Δ: =1.267 g,▲: =2.373 g,■: =4.055 g). (Δ: chrome steel,▲: stainless,■: copper ).

Approximately exponential velocity profile, large slip, only weakly dependent on granular temperature

Page 11: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Field Profiles

Temperature Density

Page 12: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Momentum BalanceCouette flow: assume steady state, variation only in x direction

∂∂x

[ν∂Vy∂x

] = 0

Include linear friction with top and bottom plates:

∂∂x

[ν∂Vy∂x

] =αVy

Linear shear profile if is constant

Vy ~ e−y / yo yo = ν /αconstant

(Similar to simple fluid in thin Couette cell)

Page 13: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

MD Simulation, parameters matching experiment

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Vary :

yo ~ 1/ α

Exp. Profile,Large slip

Page 14: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Remove Friction

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Linear Profile,Don’t observeexpected deviations

Page 15: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Higher wall velocity

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Page 16: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics
Page 17: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics
Page 18: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Evolution of mean velocity

Time (oscillation periods)

Page 19: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Bulk shear rate vs. wall velocity

Page 20: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

Dependence on shaking

• Critical v ~ sqrt(T)

Page 21: Shaking and shearing in a vibrated granular layer Jeff Urbach, Dept. of Physics, Georgetown Univ. Investigations of granular thermodynamics and hydrodynamics

CONCLUSIONS • Complex phase diagram similar to colloids, with modifications due to non-eq. effects.• Exponential velocity profiles due to friction with plate and lid.• Approximately constant apparent viscosity.• Slip instability in simulations in the absence of wall friction.Acknowledgements:Paul Melby (now at Mitre Corp)Francisco Vega Reyes (now in Badajoz, Spain)Alexis Prevost (now at CNRS - Paris)

Nick Malaya, J. Cameron Booth, Pramukta KumarProf. David Egolf