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複雜系統之簡介(梁鈞泰) - 中研院物理研究所- Academia Sinica

複雜系統之簡介(梁鈞泰) - 中研院物理研究所- Academia Sinica

複雜系統之簡介(梁鈞泰) - 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 a complex system<br />

• Brownian motion and random walk<br />

• Dimensions, fractal, power laws & self-similarity<br />

• Self-organized criticality<br />

• Earthquake and its modeling<br />

• Some current research topics


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

<br />

來 說 <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 />

Robert Brown (1773–1858)<br />

朗 <br />

<br />

不 行 不 <br />

<br />

10 -6 <br />

2 µm polysteryne spheres<br />

in water<br />

doing random walks


Brownian motion random walk<br />

Its trajectory () does look random


Random walk of a drunkard ( )<br />

He moves one step at a time,<br />

equal chance to the left and right<br />

Let us label the steps of the drunkard by<br />

x 1 for the first step, x 2 for the second step,<br />

and so on. Each of them equals ∆x or –<br />

∆x.<br />

time t<br />

Let n=total number of steps<br />

∆t=time between steps (e.g. 1 sec)<br />

t=total time=n ∆t<br />

The total distance of the walk is<br />

X = x 1 + x 2 + x 3 +…+ x n<br />

∆x<br />

Note the averages: =0, =(∆x) 2


Let us do some statistics:<br />

Although each walk looks random, after<br />

many such walks, their averages are no<br />

longer random:<br />

∆x<br />

X = x 1 + x 2 + x 3 +…+ x n<br />

= n =0<br />

X 2 = (x 1 + x 2 + x 3 +…+ x n ) (x 1 + x 2 + x 3 +…+ x n )<br />

= x 1<br />

2<br />

+ x 2<br />

2<br />

+ x 3<br />

2<br />

+…+ x n<br />

2<br />

+ x 1 x 2 + x 1 x 3 +…+ x 1 x n<br />

+ x 2 x 1 + x 2 x 3 +…+ x 2 x n +…<br />

+ x n x 1 + x n x 2 +…+ x n x n-1<br />

= + + +…+ + 0<br />

= n = (∆x) 2 n<br />

= [ (∆x) 2 /∆t ] (n ∆t)<br />

= C t<br />

where C≣ (∆x) 2 /∆t is called the diffusion constant


律<br />

= 了 t 度<br />

X<br />

2<br />

≈ C t<br />

Still holds in 2, 3,… dimensions.<br />

C=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 in 力<br />

v=g t<br />

x<br />

=<br />

vt<br />

∝t<br />

v=constant<br />

2<br />

x ≈ C t<br />

Random walk<br />

v=??


Exercises:<br />

Can we talk about the speed of diffusion?<br />

What is it? [Hint: how do you define speed?]<br />

Related:<br />

how long does it take for a fly to know you are<br />

eating a candy?<br />

How long does it take to spread a rumour (or<br />

information, or disease) in a class?


Dimension D ( 度 )<br />

Two ways to define D:<br />

1. Mass ( 量 ) M~L D<br />

M~L D=1<br />

M~L 2 D=2 M~L3 D=3<br />

2. Stick length ( 度 ) l Coverage ( 數 ) N ~ 1/l D 數 律<br />

1<br />

2<br />

4<br />

l=1, N=64 l=2, N=16=64/2 2 l=4, N=4=64/4 2<br />

N ~ 64/l D


Fractal dimension 度<br />

fractal B. Mandelbrot <br />

(The fractal geometry of Nature, 1983) <br />

Stick length ( 度 ) l<br />

Coverage ( 數 ) N ~ 1/l D<br />

l=200 km l=100 km l=50 km<br />

1 < D < 2<br />

Most coastlines are fractal with dimension between 1 & 2


Sierpinski gasket is a fractal that you can make


Sierpinski gasket<br />

l is the stick length (=radius for applying “gaussian blur”<br />

to this picture in the program called Photoshop)<br />

l=1=2 0 l=1/2=2 -1 l=1/4=2 -2 l=1/8=2 -3<br />

N=3 N=9=3 2 N=27=3 3 N=81=3 4<br />

So l=(1/2) n =2 -n<br />

N=3 n


l = (1/2) n =2 -n<br />

N = 3 n<br />

we want to know how N changes with l.<br />

we must eliminate n. Log is the way to do it:<br />

log l = - n log 2<br />

n = - log l / log 2<br />

Basic formula of logarithm:<br />

For x=a y , we have<br />

N = 3 n = 3<br />

-log l /log 2<br />

y=log a<br />

x=log x / log a,<br />

= 3 -log 3 l /log 3 2<br />

= (3 log 3 l ) -1/log 3 2<br />

a log a x =a y =x<br />

= l -1 /log 3 2<br />

= l<br />

–log 3/log 2<br />

= (1/l) D D = log3/log2 =1.585<br />

log a<br />

x / log a<br />

y=log b<br />

x / log b<br />

y, for any a, b.


Exercise:<br />

What is the average density of fractal?<br />

What is the difference between that and the density<br />

of normal objects?<br />

Can you use it to tell whether an object is a fractal or not?


Koch curve ()<br />

Exercise:<br />

Can you show that the fractal dimension of the<br />

Koch curve is log4/log3 = 1.26?


Fractal dimension of a random walk<br />

L<br />

2<br />

=<br />

x<br />

2<br />

≈<br />

C t<br />

L<br />

Let each step carry a unit mass m.<br />

After t steps, total mass M is<br />

M=m t ≈ m L 2 /C ~ L 2<br />

D=2 in any dimension


Self-similarity <br />

切 <br />

<br />

Sierpinski gasket


切 <br />

It looks random, but<br />

it also looks “self similar”


: Now you’ve learnt self-similarity, let us apply it!


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

an equation known as Langevin equation ( 朗 ):<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 />

= C<br />

∂t<br />

∂<br />

∂<br />

2<br />

ρ<br />

2<br />

x<br />

ρ<br />

x


Steady diffusion<br />

Current through any surface at<br />

radius r must be constant:<br />

absorber<br />

density ρ=0<br />

R<br />

I = constant ~ C ρ 0 R<br />

by dimensional analysis ( 量 ).<br />

But I =J * area = J 4π r 2<br />

density ρ 0<br />

<br />

So J = I/4πr 2 = C ρ 0 R/r 2<br />

is the current per unit area.<br />

Important to see that I ∝ R , not R 2 , because the current density J<br />

decreases as 1/R.


Similar result for a disk absorber: I = 4 C ρ 0 R.<br />

absorber<br />

R<br />

These results can all be derived by solving the diffusion equation<br />

(a differential equation):<br />

∂ρ<br />

=<br />

∂t<br />

C<br />

∂<br />

∂<br />

ρ<br />

=<br />

2<br />

x<br />

2<br />

0<br />

subject to boundary conditions ρ(R)=0, ρ()=ρ 0


If some sea animal is fed by taking small creatures or algae that<br />

happen to diffuse into its mouth, the sea animal cannot grow too big:<br />

3<br />

Food consumption rate ∝ R<br />

Food intake rate<br />

∝<br />

R<br />

R


Diffusion Limited Aggregation (DLA) ~ crystal growth<br />

Start with a seed at center. Random particles released from boundary,<br />

doing random walk until it sticks to the center. The seed grows into a cluster


Phase transitions <br />

Critical temperature<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~0<br />

T=T c T=1.05 T c T=2T c<br />

Exercise: which pattern is more complex, contains more information?


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 ()<br />

is also 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


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


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<br />

Number of jobs thrown out of window obeys P(n)~n -b


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


One major success of SOC is in earthquake modeling<br />

(Note: not prediction)


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


Note that we have only talked about statistics,<br />

nothing about prediction.<br />

Sadly, nobody is able to predict when, where<br />

and how an earthquake happens.<br />

Earthquake remains a difficult problem.


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 />

-…..


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


How about other creatures?<br />

All rely on vortices, but different<br />

topology due to different<br />

boundary conditions.


Ancient “water striders”<br />

Excerpt from


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.


Conclusion<br />

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 />

• Random walk and its generalizations occupy an<br />

important role.<br />

• Interesting problems are around you, so you’d better<br />

be curious.

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