introduction to complex systems...

61
Introduction to Complex Systems 複雜系統之簡介 梁鈞泰 中央研究院物理所 Kwan-tai Leung Institute of Physics, Academia Sinica, Taipei, 115, Taiwan http://www.sinica.edu.tw/~leungkt

Upload: others

Post on 13-Aug-2020

4 views

Category:

Documents


0 download

TRANSCRIPT

  • Introduction to Complex Systems複雜系統之簡介

    梁鈞泰中央研究院物理所

    Kwan-tai LeungInstitute of Physics, Academia Sinica,

    Taipei, 115, Taiwan

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

  • Outline of talk

    • What is complex system

    • Brownian motion and random walk

    • Power laws & self-similarity

    • Self-organized criticality

    • Earthquake and its modeling

    • Some current research topics - crack pattern formation- water striders- …..

  • What is a complex system (複雜系統)?

    複雜系統是一個由多個簡單單元所組成的結構。一般來講,複雜系統最有趣的地方在於所組成的單元經由非線性交互作用,會產生集体的行為。這些集体行為可在空間或時間中表現為圖形化、新層次之結構。

    這類系統往往受外界影響,而在熱力、噪音的作用下運作。要瞭解這些系統的行為,我們需要運用熱力學和統計力學的概念和方法。

  • Brownian motion & random walk布朗運動與隨機行走

    Let us start with a simple system:2 µm polysteryne spheres

    in waterdoing random walks

    布朗先生在顯微鏡下看到水中的花粉不斷進行

    不規則的運動

  • The random walker’s trajectory (軌跡)

    It does look random

  • The motion of a random walker is better described byan equation known as Langevin equation:

    ξµ += fdtdx

    dxdUf −=

    f 是外力,µ 是 mobility,而 ξ 則是噪音項

    假如流體中有不只一顆而是很多顆粒子,我們需要知道的不是每顆粒子的位移,而是粒子的密度場 。密度場遵守擴散方程式:

    ),( txρ.

    2

    2

    xD

    t ∂∂

    =∂∂ ρρ

  • 統計 規律

    tDx ≈2 D=diffusion constant~ 10-9 cm2/sec for 2µm particle in water

  • Power laws 指數定律When two physical variables are related, the simplest relationship is a power law. E.g.

    g Free fall22

    21 tgtx ∝=

    Constant speedtvtx ∝=

    Random walktDx ≈2

  • Self-similarity 自我相似性

    cut and blow up

    It looks random, butit also looks “self similar”

  • Self-similarity in fractal (碎形)

    Sierpinski gasket

    cut

    Blow up

  • A practical example of self-similarity

  • Self-similarity and power laws can be found in phase transitions

    Phase transitions 相變

    Common material’s 3 phases Magnetic material

  • Power laws in thermodynamic quantites at phase transition

    Magnetization 磁化率

    Specific heat 比熱

  • Lattice-gas model of phase transitions~ many random walkers with weak attraction

    T=Tc T=1.05 Tc T=2Tc

  • Scale invariance or self-similarity at Tc

    After the operation, the left pictureIs reduced into this box

  • A self-similar trajectory lacks characteristic length andtime scale. If you do a Fourier analysis, there is nocharacteristic frequency – the power spectrum is alsoa power law:

    αffP 1)( ≈ α=2

  • αffP 1)( ≈

    α=0White noise

    1/f noise

    Brownian noise

    α=1

    α=2

  • Self-Organized Criticality (SOC)自組臨界性

    對於任一時間序列,我們總可以計算它對應的功率譜。人們逐漸發現世界上有很多人為或自然產生的時間序列,它們對應的功率譜都沒有明顯的特徵頻率,而且經常具有這特性的現象有很多,包括河流的水位、恆星的亮度、地震的訊號、股票指數的起伏、甚至古典音樂的音量等。如何去合理解釋這普適性便成為理論物理學家的挑戰。

    於是,Per Bak等人在1987年提出即使在缺乏明顯可調控的參數下也能產生指數定律的機制,並稱之為「自組臨界性」(self-organized criticality)。他們更同時提出一個圖像化而直覺的「沙堆模型」(sandpile model)來闡釋該概念。

  • Bak & Chen, Sc. Am. 1991

    Sandpile as a paradigm of SOC

    • “Self-organized” means systems reaching critical states without tuning.• “Critical”: at critical slope (“angle of repose”), no characteristic avalanche

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

  • Open-boundary conditions 開放的邊界條件

    are important to ensure self-organized criticality

  • One major success of SOC is in earthquake modeling

  • Gutenberg-Richter law for earthquake magnitudeC

    umul

    ativ

    e di

    strib

    ut’n

    Earthquake magnitude m

    Slope 1.62 (compared to 1.8 of model)

    N(>m) per yrData from sesmicity catalog 1973-1997

  • self-organized critical earthquake model

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

    fault

  • Slip-size distribution in earthquake model

    P(S)~S -1.8Latest results: Lise & Paczuski PRE 2001

    One slip initiates an avalanche of ultimately S slips

    S

    P(S)

    S

  • Outline of talk

    • What is complex system

    • Brownian motion and random walk

    • Power laws & self-similarity

    • Self-organized criticality

    • Earthquake and its modeling

    • Some current research topics - crack pattern formation- water striders- …..

  • The scales of cracks

    50µm

    monolayer of microspheres

    20cmdried clay

    1m

    dried lake

    fissures in Black Rock Desert, Nevada

    100m

    earthquake faults

    100 km

  • monolayer of polystyrene spheres (µm size)

    Early stage

    Skjeltorp & Meakin

    0.5 mm

    0.05 mm

  • In presence of dissipation (e.g. friction), crack growthis subcritical, and speed of crack tip

  • What happens at crack tips?

    Tensile stress in a block

    0σσ >>yy

    Stress concentration at tip

  • Stress field Crack path

    xxσ

    0=yyσ

    A crack modifies the stress field around it, which in turn dictates its subsequent propagation.

    crack nucleated from boundary

    crack nucleated in bulk, thenpropagates toward boundary

  • Inexpensive experiments

    slipperysubstrate

    frictional substrate

    • coffee-water mixture Groisman & Kaplan, Europhys Lett. 1994

    Leung & Neda, Phys. Rev. Lett. 2000

    thick layerthin layer

    • starch-water mixture

  • with 120o joint

    without 120o joint

    thickness2

    fragment area

    Length scale

    fraction of 120o joint

    Groisman & Kaplan, Europhys Lett. 1994

    Morphology

    from coffee-water mixture expt

  • Approach: simplify the problem as much as possible—one step from being trivial. Try to capture the essentialphysics, then test the results against real, complex situations.

  • Simulating cracks: a spring-block model

    cracking

    0=τcrackF>τtension

    },{ ii yx

    kH

    slipi FF >force

    stick-slip

    0=iF localequilibrium

    slippings

    crackings

  • Some typical evolution of cracks by simulations

    Simulation using spring-block modelstrain=0.5 κ=1 thickness H=2

    Close-up of crack propagation and branching

  • Simulation using spring-block modelstrain=0.3 κ=0.5 thickness H=3

    Diffusive cracks

    real cracks on desiccatingpaint (Summer Palace, Beijing)

  • Simulation using spring-block modelstrain=0.5 κ=0.5 thickness H=3Connected (or percolating) cracks

  • Simulation using spring-block modelstrain=0.1 κ=0.5 thickness H=9

    Straight cracks, then diffusive

  • 生物物理 (Biology-Inspired Physics )

    生命體中有許多巨份子不斷在進行極為複雜的物理、生化相互作用。因此,從物理學的觀點看來,生命體無疑是最難被理解的物理系統。在探索生物的過程中會產生大量數據,物理學家希望能從中尋找一些基本原理。

    由於生物中的巨份子一直處於一個熱力環境中,統計物理自然是研究生物不可或缺的工具。在這個基礎上,物理學家可以研究: ‧生理訊號(如心跳)的數據分析, ‧生物巨分子(如DNA、RNA和蛋白質)的模擬﹔‧發展最佳化的數值方法在蛋白質結構的預測﹔‧份子馬達的物理機制﹔‧神經網絡的同步發火現象的實驗。

  • Current research reported in first-class scientific journalon a daily-life type of problem

    The water strider’s leg

  • Locomotion and the water-repellent legsof water striders

    Looks like a big mosquito, lives on surface of still water.Sensitive to surface vibrations—detects presence of preys.Eats living and dead insects on surface.No wing. Usually in group.Do not bite people.Body length L ~ 1 cmWeight w ~10 dyn ( m ~ 0.01 gm)

    1 cm

    水蠅@南港胡適公園

  • Excerpt fromMicrocosmos -- Claude Nuridsany and Marie Perennou, 1995

  • Focus on the legs

    Short front legs for grabbing prey, middle legs for rowing, and the rear legs steer and balance.Legs and lower body covered with tiny “hairs”to keep it from getting wet.Walking speed: 1m/sec ~ 100 body lengths/sec

    Main things to understand:

    1. How it stays afloat structure of its legs2. How it walks on water hydrodynamics

  • Two recent papers address those problems:

  • 1. Structure of legs

    The wax extracted from the leg of striders has a contact angle θ=105 ° . For length L=5mm, σ=70 dyn/cm:

    F= 2Lσ cosθ ~20 dyn.

  • Looking closelySEM scans reveal fine structures of leg:

    oriented setae (needle-shaped hair) of diameter hundreds nm to 3 µm,length 50µm, at angle 20 ° from axis

    Moreover, there are elaborate nanoscale grooves on a seta

    20 µm200 nm

    Trapping of air by setae and nanogrooves provides cushion for the leg from getting wet, and enables the insect to float.

  • Legs filled with air

  • 2. Mechanism of locomotion

    To move, one must push on something backward, something that carriesthe momentum. It's the ground (earth) that we push when we walk, and vortices in water when we swim. How about for water striders?

    Long believed to be surface waves (capillary waves).

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

    A strider must beat its legs faster than this speed.No problem for adults, but measurements show that infant striderscan’t beat that fast.

    Denny's paradox.

  • Hu et al videotaped striders at 500 fps, showing no substaintial surface waves, but there are vortices beneath the water surface. The vortex filament cannot start and end in bulk, it must be U-shaped.

    So, the legs stroke the water like the oars of a rowing-boat,sendingvortices backward to propel itself forward.

  • The balance of momenta

    For dipolar vortices at wake of stroke:Speed V=4 cm/s, radius R=4mm, Mass M=2 π R3/3, MV=1 g cm/s,

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

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

  • Robo-strider

    1 cm

  • What do we learn from the water strider?

    A common subject (such as water strider) may contain interesting, potentially important physics waiting for you to discover.

    In biophysics, to solve a problem one often needs to look very closely—as close as down to nanometer scale. This requires nano-technology, state-of-the-art imaging techniques, etc.

    Biophysics is more than proteins and DNA.

  • Conclusion

    Two main Ideas we want to get across:

    • We have shown that statistical physics methods are useful in understanding complex phenomena by means of simple models and rules.

    • Interesting problems are around you, as long as you keep an opened eye. And they can be inexpensive.

    Introduction to Complex Systems複雜系統之簡介