centrifuge physical modeling & scaling laws.pdf

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Centrifuge Physical Modeling & Scaling Laws Tarek Abdoun RPI/UCD NEES Centrifuge Research and Training Workshop 2011

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Page 1: Centrifuge Physical Modeling & Scaling Laws.pdf

Centrifuge Physical Modeling &

Scaling Laws

Tarek Abdoun

RPI/UCD NEES Centrifuge Research and Training

Workshop 2011

Page 2: Centrifuge Physical Modeling & Scaling Laws.pdf

Geotechnical Centrifuge

Ng

Page 3: Centrifuge Physical Modeling & Scaling Laws.pdf

Ground Centrifuge Modeling

Concept

Page 4: Centrifuge Physical Modeling & Scaling Laws.pdf

Radial g-field

• At which radius do you calculate g = w2r?

• Pick a point in the model where you are most concerned about accurately modeling the effective stress. Set g accordingly.

– For level ground: s = r (gavg overburden)(d)

• Document the RPM and the radius to a reference point on the model container

• Might need to account for g variation in deep models

Page 5: Centrifuge Physical Modeling & Scaling Laws.pdf

Why Physical Model Tests?

• Complex, nonlinear stress-strain behavior

of soil (made of interacting particles, air,

water)

• Difficulty of numerical simulation of soil

and soil-structure systems at large strains

and failure

• Validate and calibrate numerical methods

Page 6: Centrifuge Physical Modeling & Scaling Laws.pdf

Why Centrifuge Model Tests?

• Small-scale models are cost-effective

• Soil properties are highly stress-dependent

• Centrifuge produces equal confining stresses

in model and prototype, therefore same soil

properties

• Then, reasonable assumption that strains and

deformations are also equal in model and

prototype

Page 7: Centrifuge Physical Modeling & Scaling Laws.pdf

Application Domain: Systems

• Natural or artificial soil deposits, different

soil types, different geometries, earth

dams and dykes

• Soil-foundation and soil-structure systems:

– foundations of buildings, bridges

– buried pipes and tunnels, basements

– earth levees with sheetpiles

– etc.

Page 8: Centrifuge Physical Modeling & Scaling Laws.pdf

Application Domain : Loadings

• Static gravity loads

• Earthquake shaking

• Blasting

• Ground deformation

• Water waves

• Contaminant transport

Page 9: Centrifuge Physical Modeling & Scaling Laws.pdf

Centrifuge Modeling Limitations

• Useful only for systems containing

soil or other pressure-dependent

material

• Models allow limited detail

• Effect of model boundaries

• Time scale and strain-rate issues

Page 10: Centrifuge Physical Modeling & Scaling Laws.pdf

Scaling Laws (N = number of g’s)

• Stress & Pressure σ * = 1

• Density ρ * = 1

• Length 1/N

• Velocity 1

• Acceleration N

• Volume 1/N3

• Mass 1/N3

• Force 1/N2

• Time (dynamic) 1/N

• Time (diffusion) 1/N2

Scaling Laws

Page 11: Centrifuge Physical Modeling & Scaling Laws.pdf

Catalogue of scaling laws and

similitude questions in

centrifuge modelling

• Technical Committee TC2 –Physical

Modelling in Geotechnics 2007

• Covers: dynamics, fluid flow in soils, heat

transfer and ice, particle size effects, rate

effects

• About 60 references

Page 12: Centrifuge Physical Modeling & Scaling Laws.pdf

Concerns regarding scale

effects and scaling laws

• Unsaturated soil, Turbulent flow,

Erosion, Shear bands

• Effect of transducer or model container

on the experiment

• Range of scaling laws applicability (50g,

100g, 150g, etc.)

Page 13: Centrifuge Physical Modeling & Scaling Laws.pdf

Modeling Structural Elements

• Very challenging task:

– D & t (N)

– Area (N2)

– Inertia (N4)

– E (1) for same material

• Usually very difficult to maintain the same scale

for all parameters or to use same material in

both model and prototype (easier if no specific

prototype)

• Need to prioritize (EA, EI, t/D, etc.)

– EI for flexure or bending

– EA for axial loading

Page 14: Centrifuge Physical Modeling & Scaling Laws.pdf

NEES-Pipelines “Evaluation of Ground Rupture Effects on Critical Lifelines”

Numerical

Modeling

Centrifuge

Modeling Full scale

Testing

Page 15: Centrifuge Physical Modeling & Scaling Laws.pdf

EA vs. EI for Structural Elements

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0 0.02 0.04 0.06 0.08 0.1 0.12

tm/D

m

tp/Dp

EA curve

EI curve

Em/Ep= 0.6

Page 16: Centrifuge Physical Modeling & Scaling Laws.pdf

EA vs. EI for Structural Elements

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0 0.02 0.04 0.06 0.08 0.1 0.12

tm/D

m

tp/Dp

EA curve

EI curve

Em/Ep= 0.6

Page 17: Centrifuge Physical Modeling & Scaling Laws.pdf

EA vs. EI for Structural Elements

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0 0.02 0.04 0.06 0.08 0.1 0.12

tm/D

m

tp/Dp

EA curve

EI curve

Em/Ep= 0.6

tm/Dm = 2 tp/Dp

Page 18: Centrifuge Physical Modeling & Scaling Laws.pdf

Other Factors: Strain Rate

0 1 2 3 4

Axial Strain (%)

0

5

10

15

20

25

Axia

l S

tres

s (

MP

a)

HDPE Material Stress-Strain Behavior

0.1%/min

1%/min10%/min

1%/min

0.16%/min

130%/min

300%/min

Hypobolic Fit (Merry & Bray, 1997)

RPI Uniaxial Tension Test

100%/min

300%/min

Page 19: Centrifuge Physical Modeling & Scaling Laws.pdf
Page 20: Centrifuge Physical Modeling & Scaling Laws.pdf

Comparison with Full Scale Test

Results (-63.5o Tension Test)

-6 -4 -2 0 2 4 6

Distance from Fault (m)

0

2

4

6

8

10S

pri

ng

lin

e S

train

(%

)Full Scale, f = 1.06 m

Full Scale, f = 0.49 m

Centrifuge, f = 1.06 m

Centrifuge, f = 0.49 m

Springline Strain Comparison

Page 21: Centrifuge Physical Modeling & Scaling Laws.pdf

-63.5o Strike-Slip (Tension)

Page 23: Centrifuge Physical Modeling & Scaling Laws.pdf

Time Scaling Conflict

• Dynamic Time L = 0.5 a t2 L* = a* t*2 t* = sqrt(L*/a*)

t*dyn = sqrt(L*/(1/L*)) = L* or 1/N

• Diffusion Time, consider time factor, T For similarity, T* = 1 = cv* t* /L*2

t*dif = L*2 / cv*

If cv* = 1 (same soil in model and prototype) then:

t*dif = L*2 or 1/N2

• Conflict t*dif ≠ t*dyn

• Conflict Resolution – By increasing viscosity of the fluid (m* = 1/L* or N)

– Decreasing the particle size of the soil (k* = C (D10*)2 )

Page 24: Centrifuge Physical Modeling & Scaling Laws.pdf

Time Scaling Conflict

• Sometimes, conflict can be neglected without

changing cv

– both model and prototype are undrained during dynamic

event

– both model and prototype are drained during dynamic event

• we may want to systematically vary viscosity to cover

an interesting range. (Reviewers may have difficulty

with this concept)

• It takes time to saturate a large model with viscous

pore fluid. For practical purposes, we may knowingly

violate time scale factor similarity, and then account

for the different cv by analysis

Page 25: Centrifuge Physical Modeling & Scaling Laws.pdf

Modeling of Shear Bands

J. DeJong, U. Mass Amherst web page

The shear band thickness

depends on particle size, not

on L* (N)

Page 26: Centrifuge Physical Modeling & Scaling Laws.pdf

Modeling of Shear Bands

Page 27: Centrifuge Physical Modeling & Scaling Laws.pdf

Particle Size Reduction

0

10

20

30

40

50

60

70

80

90

100

0.001 0.01 0.1 1

Particle size, mm

% S

oil p

ass

ing

Scaled SandOttawa Sand F#55

Centrifuge

Modeling

Full Scale Testing

Page 28: Centrifuge Physical Modeling & Scaling Laws.pdf

Particle Size effect

• Most basic requirement is that there are a sufficient number of particles across the dimensions of a model so that we can model the soil as a continuum. – Required Dmodel/Dparticle depends on the problem.

– Footings: Dfooting/Dparticle > 30 (minimizes particle size effect)

• To model contact stress and capillary rise most accurately, need to use same particle size (pore size) and fluid. The Ability to model capillary rise is an advantage of centrifuge high g modeling.

Page 29: Centrifuge Physical Modeling & Scaling Laws.pdf

Explosions are Volumetric

• Explosions Scale as N3

• 1 gram of explosive tested at

100g is equivalent to one million

(106) grams of prototype

explosive, or one metric ton

(2200 lb)

• Scale effects also include

particle size effects and

differences in radial acceleration

Page 30: Centrifuge Physical Modeling & Scaling Laws.pdf

Application of High Speed

Camera to Blasting Tests

1.E-02

1.E-01

1.E+00

1.E+01

1.E-04 1.E-03 1.E-02 1.E-01 1.E+00 1.E+01 1.E+02 1.E+03 1.E+04 1.E+05 1.E+06

Scaled Charge Mass (kg)

Scale

d D

ep

th (

m)

S&H su-ho bu-ve su-ve Pow er (S&H)

Page 31: Centrifuge Physical Modeling & Scaling Laws.pdf

Blast Modeling

Page 32: Centrifuge Physical Modeling & Scaling Laws.pdf

• Time Scales as g2 – E.G., 24 Hour test @ 105g = 30 years prototype time

• Advection (Hydraulic flow) – No theoretical

problems

• Dispersivity (Diffusion, Dispersion) – more

complicated, but can be done

Groundwater/Contaminant

Transport

Page 33: Centrifuge Physical Modeling & Scaling Laws.pdf

• General: Single contaminant, conservative

contaminant – models acceptable

• The robot gives us a unique opportunity to

determine the transport and concentration with

time of multiple contaminants

Groundwater/Contaminant

Transport (cont.)

Page 34: Centrifuge Physical Modeling & Scaling Laws.pdf

Boundary/Container effects

• Flexible Containers

– Hinged plate, Laminar boxes

• Ideal for gently sloping

or level ground

– Complementary Shear issue

Page 35: Centrifuge Physical Modeling & Scaling Laws.pdf

Boundary/Container effects

• Rigid containers

– P-waves from

ends of the container

• Side friction

– Avoid narrow containers (width < height)

– Reduce sides friction

– Move structures e.g., away from boundaries

• Lateral stiffness (maintaining Ko)

Page 36: Centrifuge Physical Modeling & Scaling Laws.pdf

Ground motion selection

Page 37: Centrifuge Physical Modeling & Scaling Laws.pdf

Sine waves, step waves or realistic

ground motions?

• Small step waves – Useful to check that sensors are working

• Sine waves are easier to understand than real ground motions – Because they only reveal information about part of

the problem (one frequency from the possible spectrum)

• Sine sweeps – Useful because they cover all frequencies, but

amplitude is not random.

• Ground motion provides more realistic conditions but could be difficult to analyze

Page 38: Centrifuge Physical Modeling & Scaling Laws.pdf

Final Thoughts • Centrifuge Modeling is a tool that makes model tests more

accurate because it reproduces prototype stress levels in a small scale model but be mindful of it’s limitations

• Centrifuge Modeling is useful to:

– Test the validity of a numerical model

– Perform systematic parameter studies

– Discover mechanisms of behavior

• Model testing is valuable for problems where field data is insufficient – can obtain data that is impossible to obtain in other ways.

• Advanced instruments of NEES (robotics, shakers, instrumentation) enable more accurate and more detailed models than was possible in the past.

Page 39: Centrifuge Physical Modeling & Scaling Laws.pdf

NEES centrifuge research

• Complementary NEES Centrifuges

– UCD: larger container, V&H shaker, more sensors per test, multiple tests per container

– RPI: medium size, H&H shaker, more tests per month, Robot, split box.

Page 40: Centrifuge Physical Modeling & Scaling Laws.pdf

Thank You