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複雜系統 - 中研院物理研究所- Academia Sinica

複雜系統 - 中研院物理研究所- Academia Sinica

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Introduction to Complex Systems<br />

<br />

梁 <br />

理 <br />

Kwan-tai Leung<br />

Institute of Physics, <strong>Academia</strong> <strong>Sinica</strong>,<br />

Taipei, 115, Taiwan<br />

http://www.sinica.edu.tw/~leungkt


Outline of talk<br />

• What is complex system<br />

• Brownian motion and random walk<br />

• Power laws & self-similarity<br />

• Self-organized criticality<br />

• Earthquake and its modeling<br />

• Some current research topics<br />

- crack pattern formation<br />

- water striders<br />

-…..


What is a complex system ()?<br />

<br />

來 <br />

行 <br />

行 <br />

<br />

類 力 <br />

行 <br />

力 力 念


Brownian motion & random walk<br />

朗 行 <br />

Let us start with a simple system:<br />

朗 <br />

不 行<br />

不 <br />

2 µm polysteryne spheres<br />

in water<br />

doing random walks


The random walker’s trajectory ()<br />

It does look random


The motion of a random walker is better described by<br />

an equation known as Langevin equation:<br />

dx<br />

dt<br />

= µ f + ξ<br />

f<br />

=<br />

−<br />

dU<br />

dx<br />

力 µ mobility ξ <br />

<br />

流 不 粒 不<br />

粒 粒 度 ρ( x,<br />

t)<br />

度 <br />

:<br />

∂ρ<br />

= D<br />

∂t<br />

∂<br />

∂<br />

2<br />

ρ<br />

2<br />

x


律<br />

x ≈ Dt<br />

2 D=diffusion constant<br />

~ 10 -9 cm 2 /sec<br />

for 2µm particle in water


Power laws 數 律<br />

When two physical variables are related, the simplest<br />

relationship is a power law. E.g.<br />

x<br />

=<br />

1<br />

2<br />

gt<br />

2<br />

∝<br />

t<br />

2<br />

g<br />

Free fall<br />

x<br />

=<br />

vt<br />

∝t<br />

Constant speed<br />

2<br />

x ≈ Dt<br />

Random walk


Self-similarity <br />

cut and blow up<br />

It looks random, but<br />

it also looks “self similar”


Self-similarity in fractal ()<br />

cut<br />

Blow up<br />

Sierpinski gasket


A practical example of self-similarity


Phase transitions <br />

Self-similarity and power laws<br />

can be found in phase<br />

transitions<br />

Common material’s 3 phases<br />

Magnetic material


Power laws in thermodynamic<br />

quantites at phase transition<br />

Magnetization 率<br />

Specific heat


Lattice-gas model of phase transitions<br />

~ many random walkers with weak attraction<br />

T=T c<br />

T=1.05 T c T=2T c


Scale invariance or self-similarity at T c<br />

After the operation, the left picture<br />

Is reduced into this box


A self-similar trajectory lacks characteristic length and<br />

time scale. If you do a Fourier analysis, there is no<br />

characteristic frequency – the power spectrum is also<br />

a power law:<br />

1<br />

P( f ) ≈ α=2<br />

α<br />

f


P( f ) ≈<br />

1<br />

f<br />

α<br />

White noise<br />

α=0<br />

1/f noise<br />

α=1<br />

α=2<br />

Brownian noise


Self-Organized Criticality (SOC)<br />

臨 <br />

列 率 <br />

列 <br />

率 都 率 <br />

流 亮 度 <br />

數 樂 量 理 <br />

便 理 論 理 <br />

Per Bak1987 年 參<br />

數 數 律 臨 <br />

(self-organized criticality) 更 <br />

(sandpile model) 來 念


Sandpile as a paradigm of SOC<br />

Bak & Chen, Sc. Am. 1991<br />

• “Self-organized” means systems reaching critical states without tuning.<br />

• “Critical”: at critical slope (“angle of repose”), no characteristic avalanche<br />

size exists. It covers all possible values with power-law distribution P(s)~s -b .


Open-boundary conditions <br />

are important to ensure self-organized criticality


One major success of SOC is in earthquake modeling


Gutenberg-Richter law for earthquake magnitude<br />

N(>m) per yr<br />

Cumulative distribut’n<br />

Data from sesmicity catalog 1973-1997<br />

Slope 1.62<br />

(compared to 1.8 of model)<br />

Earthquake magnitude m


self-organized critical earthquake model<br />

fault<br />

Olami, Feder, and Christensen, Phys. Rev. Lett. 68, 1244 (1992)


Slip-size distribution in earthquake model<br />

S<br />

Latest results: Lise & Paczuski PRE 2001<br />

One slip initiates an avalanche of ultimately S slips<br />

P(S)~S -1.8<br />

P(S)<br />

S


Outline of talk<br />

• What is complex system<br />

• Brownian motion and random walk<br />

• Power laws & self-similarity<br />

• Self-organized criticality<br />

• Earthquake and its modeling<br />

• Some current research topics<br />

- crack pattern formation<br />

- water striders<br />

-…..


The scales of cracks<br />

monolayer of microspheres<br />

dried lake<br />

earthquake faults<br />

100 km<br />

50µm<br />

1m<br />

dried clay<br />

20cm<br />

100m<br />

fissures in Black Rock<br />

Desert, Nevada


monolayer of polystyrene spheres (µm size)<br />

Early stage<br />

0.5 mm<br />

0.05 mm<br />

Skjeltorp & Meakin


In presence of dissipation (e.g. friction), crack growth<br />

is subcritical, and speed of crack tip


What happens at crack tips?<br />

σ 0<br />

σ >> σ<br />

yy 0<br />

σ 0<br />

Tensile stress in a block<br />

Stress concentration at tip


σ xx<br />

Stress field Crack path<br />

A crack modifies the stress field around it, which<br />

in turn dictates its subsequent propagation.<br />

σ yy<br />

= 0<br />

crack nucleated<br />

from boundary<br />

crack nucleated in bulk, then<br />

propagates toward boundary


Inexpensive experiments<br />

• coffee-water mixture Groisman & Kaplan, Europhys Lett. 1994<br />

frictional<br />

substrate<br />

slippery<br />

substrate<br />

• starch-water mixture<br />

Leung & Neda, Phys. Rev. Lett. 2000<br />

thin layer<br />

thick layer


Length scale<br />

fragment<br />

area<br />

without 120 o joint<br />

with 120 o joint<br />

Morphology<br />

thickness 2<br />

fraction of<br />

120 o joint<br />

from coffee-water mixture expt<br />

Groisman & Kaplan, Europhys Lett. 1994


Approach: simplify the problem as much as possible—<br />

one step from being trivial. Try to capture the essential<br />

physics, then test the results against real, complex situations.


Simulating cracks: a spring-block model<br />

{<br />

i<br />

x i<br />

, y }<br />

stick-slip<br />

kH<br />

force<br />

F<br />

i<br />

> F slip<br />

Fi<br />

= 0<br />

local<br />

equilibrium<br />

cracking<br />

slippings<br />

tension<br />

τ ><br />

F crack<br />

crackings<br />

…<br />

τ = 0


Some typical evolution of cracks by simulations<br />

Simulation using spring-block model<br />

strain=0.5 κ=1 thickness H=2<br />

Close-up of crack propagation and branching


Simulation using spring-block model<br />

strain=0.3 κ=0.5 thickness H=3<br />

Diffusive cracks<br />

real cracks on desiccating<br />

paint (Summer Palace, Beijing)


Simulation using spring-block model<br />

strain=0.5 κ=0.5 thickness H=3<br />

Connected (or percolating) cracks


Simulation using spring-block model<br />

strain=0.1 κ=0.5 thickness H=9<br />

Straight cracks, then diffusive


理 (Biology-Inspired Physics )<br />

不 行 理 <br />

理 來 <br />

理 理 索 <br />

量 數 理 理 <br />

力 <br />

理 不 <br />

理 <br />

‧ 理 數 <br />

‧DNARNA<br />

‧ 數 <br />

‧ 理 <br />

‧ 神


Current research reported in first-class scientific journal<br />

on a daily-life type of problem<br />

The water strider’s leg


Locomotion and the water-repellent legs<br />

of water striders<br />

@<br />

• Looks like a big mosquito, lives on surface<br />

of still water.<br />

• Sensitive to surface vibrations—detects<br />

presence of preys.<br />

• Eats living and dead insects on surface.<br />

• No wing. Usually in group.<br />

• Do not bite people.<br />

• Body length L ~ 1 cm<br />

• Weight w ~10 dyn ( m ~ 0.01 gm)<br />

1 cm


Excerpt from<br />

Microcosmos -- Claude Nuridsany and Marie Perennou, 1995


Focus on the legs<br />

• Short front legs for grabbing prey, middle legs<br />

for rowing, and the rear legs steer and balance.<br />

• Legs and lower body covered with tiny “hairs”<br />

to keep it from getting wet.<br />

• Walking speed: 1m/sec ~ 100 body lengths/sec<br />

Main things to understand:<br />

1. How it stays afloat structure of its legs<br />

2. How it walks on water hydrodynamics


Two recent papers address those problems:


1. Structure of legs<br />

Water dropet on a leg θ=168<br />

152 dyn<br />

The wax extracted from the leg of striders has a contact angle θ=105 .<br />

For length L=5mm, σ=70 dyn/cm:<br />

F= 2Lσ cosθ ~20 dyn.


Looking closely<br />

•SEM scans reveal fine structures of leg:<br />

oriented setae (needle-shaped hair) of diameter hundreds nm to 3 µm,<br />

length 50µm, at angle 20 from axis<br />

•Moreover, there are elaborate nanoscale grooves on a seta<br />

20 µm<br />

Trapping of air by setae and nanogrooves provides cushion for the leg from<br />

getting wet, and enables the insect to float.<br />

200 nm


Legs filled with air


2. Mechanism of locomotion<br />

To move, one must push on something backward, something that carries<br />

the momentum. It's the ground (earth) that we push when we walk, and<br />

vortices in water when we swim. How about for water striders?<br />

Long believed to be surface waves (capillary waves).<br />

But surface wave speed = (4 g σ/ρ) ¼ = 23 cm/s for water.<br />

A strider must beat its legs faster than this speed.<br />

No problem for adults, but measurements show that infant striders<br />

can’t beat that fast.<br />

Denny's paradox.


Hu et al videotaped striders at 500 fps, showing no substaintial surface<br />

waves, but there are vortices beneath the water surface.<br />

The vortex filament cannot start and end in bulk, it must be U-shaped.<br />

So, the legs stroke the water like the oars of a rowing-boat,sending<br />

vortices backward to propel itself forward.


The balance of momenta<br />

For dipolar vortices at wake of stroke:<br />

Speed V=4 cm/s, radius R=4mm, Mass M=2 π R 3 /3, MV=1 g cm/s,<br />

For water Strider: v=100cm/s, m=0.01g, mv=1 g cm/s<br />

Estimation of capillary wave packet momentum gives 0.05 g cm/s


Robo-strider<br />

1 cm


What do we learn from the water strider?<br />

A common subject (such as water strider) may contain interesting,<br />

potentially important physics waiting for you to discover.<br />

In biophysics, to solve a problem one often needs to look very closely—<br />

as close as down to nanometer scale. This requires nano-technology,<br />

state-of-the-art imaging techniques, etc.<br />

Biophysics is more than proteins and DNA.


Conclusion<br />

Two main Ideas we want to get across:<br />

• We have shown that statistical physics methods are<br />

useful in understanding complex phenomena by means<br />

of simple models and rules.<br />

• Interesting problems are around you, as long as you<br />

keep an opened eye. And they can be inexpensive.

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