Granular impact drag force and its material-dependent scaling - - PowerPoint PPT Presentation
Granular impact drag force and its material-dependent scaling - - PowerPoint PPT Presentation
Granular impact drag force and its material-dependent scaling Hiroaki Katsuragi & Douglas J. Durian Nagoya University University of Pennsylvania Impact! Fundamental process from planetary scale to our everyday Fundamental physics
- Fundamental process from planetary scale to our everyday
- Fundamental physics of granular matter
- Solid - fluid - solid transition
- Response to disturbance
Impact!
Contradictory previous works?
Uehara et al, PRL 2003, Ambroso et al, PRE 2004 de Bruyn et al, CJP 2004 Ciamarra et al, PRL 2004 Lohse et al, Nature 2004
F ∼ |z|α|v|
4−2α 3
F ∼ F0 + C|v| F ∼ |v0|
F ∼ |z|
d ∼ H1/3 d = α + cv0 tstop = const. d ∼ m (v0 = 0)
Experimental Apparatus
sand light line scan camera trigger electromagnet PC metal tip transparent stripe z sieve wind box ←N2
- Sand is fluidized
before each impact.
- Free fall is triggered
by an electromagnet holder.
- Dropping transparent
stripe is captured by a line-scan camera.
Raw data
z t
10 ms 1mm impact cessation z(t), v(t), a(t)
impact & stop time
- 80
- 60
- 40
- 20
v [cm/s]
0.06 0.04 0.02
t [s]
- 4
- 2
2 0.065 0.060
- 56
- 55
- 54
- 0.001
0.001
−g
vr 2vr
v = H(t−t0){v0+g(t−t0)}+H(t0−t){v0+(g−v2
0/d1)(t−t0)+([v3 0−2gd1v2 0]/d2 1)(t−t0)2}
- Low speed impact
takes longer time.
- Velocity is NOT
linear function of time.
- Acceleration shows
discontinuity at the stopping point.
a(t) = dv dt
Various drop heights :
(1” steel ball & glass beads)
- 8
- 6
- 4
- 2
2
z [cm]
- 400
- 300
- 200
- 100
v [cm/s]
h=83 cm h=50 h=30 h=15 h=7.0 h=3.8 h=2.2 h=1.6 h=1.1 h=0.52 h=0.28 h=0.18 h=0 101 102 103 104
a + g [cm/s2]
0.10 0.08 0.06 0.04 0.02 t [s]
z(t) = t v(t′)dt′ v(t)
Empirical laws & our new data
Constant stop time Coulomb friction
8 6 4 2
d [cm]
- 400
- 300
- 200
- 100
v0 [cm/s]
d = d0+|v0|
1 10
d [cm]
1 10 100
H [cm]
d= (d0
2H)1/3
d>H
0.10 0.08 0.06 0.04 0.02
tstop [s]
- 400
- 300
- 200
- 100
v0 [cm/s]
2.0x103 1.5 1.0 0.5
a + g [cm/s2]
- 2.0
- 1.5
- 1.0
- 0.5
z [cm]
v0 = 0
d/d0 = (H/d0)1/3 d = d0 + α|v0|
The data are completely consistent with empirical laws.
What is the stopping force?
Stopping force model
: independent of depth z : independent of velocity v
a+g v
f(zi)/m{
v2/d1
ΣF(= ma) = −mg + f(z) + mv2 d1 a + g = f(z) m + v2 d1 d1 f(z)
Inertial drag
a + g = (1/d1)v2 + f(zi)/m
zi = {0, −1, −2, −3, −4 [cm]}
20x103 15 10 5
a+g [cm/s2]
- 400
- 300
- 200
- 100
v [cm/s]
zi=-4 cm zi=-3 cm zi=-2 cm zi=-1 cm zi= 0 cm
20x103 15 10 5
a+g [cm/s2]
160x103 120 80 40
v2 [cm2/s2]
Friction force
8000 6000 4000 2000
- 2000
a + g - v2/d1 [cm/s2]
- 8
- 6
- 4
- 2
z [cm]
data g{1+[3(z/d0)2-1]exp(-2|z|/d1)} (k/m)|z|
f(z)/m = a + g − (1/d1)v2 f(z) m = k m|z|
Unified Force law
ΣF v z ΣF = −mg + k|z| + mv2 d1
gravitational force depth proportional frictional drag (velocity independent) velocity dependent inertial drag (depth independent)
- H. Katsuragi & D.J. Durian (2007)
Solving equation
Ke = 1 2mv2 dKe dz = −mg + 2 d1 Ke − k|z|
linearized!
v = −
- v2
0e− 2|z|
d1 − kd1|z|
m + (1 − e− 2|z|
d1 )
- gd1 + kd2
1
2m 1/2
dKe dz = mv dv dz = mdv dt
Clark & Behringer, EPL (2013) Katsuragi & Durian, PRE (2013)
v(z) & force model
- 400
- 300
- 200
- 100
v [cm/s]
- 8
- 6
- 4
- 2
z [cm] v = −
- v2
0e− 2|z|
d1 − kd1|z|
m + (1 − e− 2|z|
d1 )
- gd1 + kd2
1
2m 1/2
d1 = 8.7 cm k/m = 1040 s−2
Universality
For steel ball vs glass beads:
How can we predict these values for other material impacts?
Two parameters and determine the dynamics. d1 k/m d1 = 8.7 cm k/m = 1040 s−2
Expectation for inertial drag
ρp : density of projectile ρg : density of granular media Dp : diameter of projectile
(momentum transfer)
α = 3/2 (ball), 4/π (cylinder) A : impact area (ratio of area and volme factor)
m d1 v2 ∼ ρgAv2 d1 ∼ α−1 ρp ρg Dp
Expectation for friction force
(hydrostatic pressure + Coulomb friction)
ρp : density of projectile ρg : density of granular media µ = tan θr : friction coefficient Dp : diameter of projectile α = 3/2 (ball), 4/π (cylinder) A : impact area (ratio of area and volme factor)
k|z| ∼ µgρg|z|A k m ∼ αµg ρg ρp 1 Dp
Various projectiles and sand
glass beads beach sand rice sugar
1” Tungsten, steel,polymer, wood 2” - 1/8” steel 1/2” - 1/4” diameter 2” - 6” length aluminum
- 400
- 200
v [cm/s]
- 8
- 6
- 4
- 2
z [cm]
- 400
- 200
v [cm/s]
- 400
- 200
v [cm/s]
- 400
- 200
v [cm/s] (a) (b) (c) (d) Wood Delrin PTFE Steel
Limited fitting of v(z)
Good fitting for all impacts Bad fitting for all shallow impacts by fixed and
d1 k/m
v = −
- v2
0e− 2|z|
d1 − kd1|z|
m + (1 − e− 2|z|
d1 )
- gd1 + kd2
1
2m 1/2
Scaling of parameters
Inertial parameter: Friction parameter:
1 10
kDp'/mg
1 10 100
ρp [g/cm3]
- 1/2
- 1
0.1 1 10 100
d1/Dp' 1
(a) (b)
kDp mg ∼ ρp
1/2
d1 Dp
0 ∼ ρp
Dp
0 = 3π/8Dp for cylinder (shape factor)
Internal friction dependence
Inertial parameter Friction parameter
10
(kDp'/mg)(p/g)
1/2
1
µ 1
0.1 1
(d1/Dp')(g/p)
- 1
(a) (b)
kDp mg = 12µ ✓ρg ρp ◆1/2 d1 Dp
0 = 0.25
µ ρg ρp
d1 = 1/(1 + 2.2µ)
UNIFIED FORCE LAW
ΣF = −mg + k|z| + mv2 d1
final form of the drag force:
d1 Dp = 0.25 µ ρp ρg k m Dp g = 12µ ρp ρg 1/2
Scaling by material properties:
- H. Katsuragi & D.J. Durian, Phys. Rev. E 87, 052208 (2013)