23
1 Granular Flows

Acoustic emission of sand - DAMTP

  • Upload
    others

  • View
    9

  • Download
    0

Embed Size (px)

Citation preview

Page 1: Acoustic emission of sand - DAMTP

1

Granular Flows

Page 2: Acoustic emission of sand - DAMTP

2

Lecture 2: Contact forces

Contact forces between individual grains follow the

solid constitutive relations.

– Are they applicable for large-scale flows?

Contact forces:

Normal elastic stresses due to weight

Electrostatic attraction

Hertzian normal forces (+ impulsive case + liquid bridges)

Coulomb friction (+ impulsive case)

Page 3: Acoustic emission of sand - DAMTP

3

Newton’s cradle (1)

History:

Christiaan Huygens (1703): discusses Newton’s first law &

collisions of suspended bodies

Demonstrates conservation of momentum and energy with

swinging spheres

Assumptions:

Conservation of kinetic energy before and after collision

Conservation of total momentum before and after collision

Let’s take a look!

Page 4: Acoustic emission of sand - DAMTP

4

Newton’s cradle (2)

Let’s scale it up!

Mythbusters episode “Newton’s crane cradle” (Oct. 2011)

http://dsc.discovery.com/tv-

shows/mythbusters/videos/newtons-cradle-

high-speed-1.htm

http://www.wired.com/wiredscience/2011/1

0/what-went-wrong-with-the-mythbusters-

newton-cradle/

Page 5: Acoustic emission of sand - DAMTP

5

Forces from elastic stresses

Normal elastic stress on a cube:

In z-direction: zz = g h = E = E w/h

Example:

Density = 2.5.103 kg/m3

Gravity g = 9.8 m/s2 zz = 24.5 N/m2

Size h = 1 mm

Young’s modulus for glass E = 7.1010 N/m2

displacement w = h = h zz /E = 3.5.10-13 m

Elastic stresses are small (picometers), compared to

stresses due to electrostatic forces!

Page 6: Acoustic emission of sand - DAMTP

6

Electrostatic forces

Very dry conditions creates solid-solid rubbing:

Friction creates triboelectric charging

Long-range interactions manifest as Coulomb repulsion

Charge per grain scales with surface area

smaller particles have more static electricity

Causes: agglomeration,

adhesion and segregation

In experiments:

Provide grounding

Use metal surface, not plastic

Keep an eye on the humidity

From: http://www.physik.uni-wuerzburg.de/~hinrichsen

Page 7: Acoustic emission of sand - DAMTP

7

Forces from Hertzian contacts

From Wikipedia: http://en.wikipedia.org/wiki/Contact_mechanics

Page 8: Acoustic emission of sand - DAMTP

8

Focus: Hertzian contact force

Assumptions:

Frictionless contacts

R1, R2 >> l

Non-conforming surface

Hertzian theory:

Geometrical relation:

Hertzian pressure distribution:

Radius of contact area:

Depth of indentation:

Page 9: Acoustic emission of sand - DAMTP

9

Focus: Hertzian contact force

Assumptions:

Frictionless contacts

R1, R2 >> l

Non-conforming surface

Hertzian theory:

Geometrical relation:

Hertzian pressure distribution:

Radius of contact area:

Depth of indentation:

Page 10: Acoustic emission of sand - DAMTP

10

Speed of sound

Sound speed:

Sphere-on-sphere geometry:

high confining pressures

Conical geometry:

low confining pressures

What happens on

the free surface?

From: Jia et al., Phys. Review Letters, 1999

Page 11: Acoustic emission of sand - DAMTP

11

Impulsive Hertzian forces (1)

Drop a ball with a velocity v1 against a stationary ball:

Conservation of kinetic energy: ½ m1 v12 = ½ m2 v2

2

Momentum conservation: m1 v1 = m1 vr + m2 v2 = Fn t

Coefficient of restitution: = (-vr + v2)/v1

assume vr = 0, v1 = v2 & = 1 (perfectly elastic, no losses)

Page 12: Acoustic emission of sand - DAMTP

12

Impulsive Hertzian forces (2)

Coefficient of restitution :

= 1: perfectly elastic, no energy loss

= 0: plastic, complete energy loss

0 < < 1: a proportion of the energy is lossed

Bouncing ball:

= (h1/h0)½

hk = 2k h0

Page 13: Acoustic emission of sand - DAMTP

13

Processes during contact:

As soon as collision occurs, compressive forces act &

velocities change

Time of collision >> period of lowest mode of vibration

Calculate collision time during contact:

Normal force:

Acceleration (Fn t = m1 v1):

Collision time:

Details in: Theory of elasticity, Timoshenko & Goodier

Impulsive Hertzian forces (3)

Page 14: Acoustic emission of sand - DAMTP

14

A practical example of the collision time:

R = 1 mm

v = 1 m/s

E = 50 GPa, = 0.3

= 2.5.103 kg/m3

… and the maximum penetration depth:

R = 1 mm

v = 1 m/s

E = 50 GPa, = 0.3

= 2.5.103 kg/m3

Applied strain: = /l = (/R)½ = 4.8.10-2

Impulsive Hertzian forces (4)

t = 6.8.10-6 s

= 2.3.10-6 m c3 = 2.3.10-3 (m/s)-4/5

c2 = 6.8.10-3 (m/s)-4/5

Page 15: Acoustic emission of sand - DAMTP

15

What happens in the idealized Newton’s cradle?

Just after contact, all balls are in contact with each other

Net impulses of balls must be zero, for balls that end up with

the same velocity (also for stationary balls)

Net impulses of ball 1 & N are not zero, as forces are not

balanced during contact!

The kinetic energy of ball N was stored as compressed energy

at the interfaces

Two released particles?

Ball 1: initially at V, impulse slows it to rest

Ball 2: zero net impulse, equal and opposite compression force

Ball 3: initially at rest, impulse speed it up to V

Newton’s cradle (1)

Page 16: Acoustic emission of sand - DAMTP

16

What can go wrong (Mythbuster experiment?):

Balls are not perfectly elastic: vr ≠ 0

Flansburg and Hudnut [1979]: three steel balls

Final velocity ideal case: 0, 0, and 1

Final velocity real case: -0.06, +0.09 and +0.97

Air gaps between balls, alignment incorrect

Mass or dimensions of balls are not perfectly the same

As always, scale is an issue!

Newton’s cradle (2)

Page 17: Acoustic emission of sand - DAMTP

17

Liquid bridges between spheres:

Same principles apply!

As spheres approach they:

Experience resistance due to lubrication

Attain a minimum separation

Experience resistance upon rebound (not enough fluid left)

Fluid resistance cannot be neglected

Outcome depends on Stokes number (= inertial-viscous forces)

& liquid thickness between ball 2 & 3

Stokes’s cradle

From: Donahue et al., PRL, 2010

Page 18: Acoustic emission of sand - DAMTP

18

Granular medium: microscopic and macroscopic friction

Microscopic: in contacts between grains

Macroscopic: friction angle (later lectures)

Use Coulomb (solid-solid) friction as a model:

Stick: Ff < s Fn

Slip: Ff = d Fn

with the static s and dynamic d

coefficient of friction,

typically: 0 < d < s < 1

Force is opposite of motion

Frictional forces (1)

Page 19: Acoustic emission of sand - DAMTP

19

Stick-slip motion:

Alternating behavior: move – stop – move - stop

Spring elongates, mass moves, spring jumps back

Frictional forces (2)

From: Les Milieux granulaires, O. Pouliquen

Page 20: Acoustic emission of sand - DAMTP

20

Indeterminacy:

4 unknown forces (Ff, Fn for each wall)

2 force balances

1 momentum balance

Indeterminacy, solve by knowing history!

For a pile of sand: how was it build?

Frictional forces (3)

Page 21: Acoustic emission of sand - DAMTP

21

Ball on a surface:

slips and decelerates by friction force

decrease in linear momentum increase angular momentum

starts rolling with rolling friction (empirical)

when ball rolls without slip rolling velocity: Vr = 5/7 V0

Rolling or slipping?

Page 22: Acoustic emission of sand - DAMTP

22

Bowling ball is thrown with backspin and velocity V0:

assume mass m, radius R, moment of inertia Icm = 2/5 m R2

furthermore, assume V0 > R 0

calculate speed Vf when it rolls without slipping

Example: Bowling ball (1)

Page 23: Acoustic emission of sand - DAMTP

23

Equate angular momentum:

Linitial = m V0 R – Icm 0

Lfinal = m Vf R + Icm f

Substitute: vf = f R vf = 5/7 (v0 – 2/5 R 0)

Example: Bowling ball (2)

Linitial = Lfinal