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.