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Entropy production and fluctuation phenomena in nonequilibrium - - PowerPoint PPT Presentation

Entropy production and fluctuation phenomena in nonequilibrium systems Haye Hinrichsen Faculty for Physics and Astronomy University of Wrzburg, Germany Workshop on Large Fluctuations in Non-Equilibrium Systems MPIPKS Dresden, July 2011 I n


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Entropy production and fluctuation phenomena in nonequilibrium systems

Haye Hinrichsen Faculty for Physics and Astronomy University of Würzburg, Germany Workshop on Large Fluctuations in Non-Equilibrium Systems MPIPKS Dresden, July 2011

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In collaboration with:

Andre Barato, ICTP, Trieste, Italy Urna Basu, SAHA Institute, Kolkata, India Raphael Chetrite, Lyon and CNRS Christian Gogolin, Potsdam Peter Janotta, Würzburg David Mukamel, Weizmann Insititute, Israel

Non-equilibrium Dynamics, Thermalization and Entropy Production

  • H. Hinrichsen, C. Gogolin, and P. Janotta
  • J. Phys.: Conf. Ser. 297 012011 (2011)

Entropy production and fluctuation relations for a KPZ interface

  • A. C. Barato, R. Chetrite, H. Hinrichsen, and D. Mukamel
  • J. Stat. Mech.: Theor. Exp. P10008 (2010)
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Outline 1) Introduction to entropy production 2) Fluctuation theorem revisited 3) Entropy production and renormalization

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Nonequilibrium systems Nonequilibrium systems

T1 T2 μ1 μ2

Flow of heat … typically driven systems Flow of particles

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Environment

Nonequilibrium systems Nonequilibrium systems

System

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Environment

Nonequilibrium systems Nonequilibrium systems

System

drive entropy

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Models of classical nonequilibrium systems Models of classical nonequilibrium systems

System

entropy Model

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Models of classical nonequilibrium systems Models of classical nonequilibrium systems

System

entropy

Set of configurations Ωsys (state space)

configurations c∈sys Model

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Models of classical nonequilibrium systems Models of classical nonequilibrium systems

System

entropy Model Irreversible dynamics by spontaneous transitions at rate

cc'

wcc'

Ωsys

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Configurational entropy Environmental entropy Total entropy

S syst = −ln Pc ,t S envt Stot(t)=Ssys(t)+Senv(t)

Environment

System

drive entropy

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Actual time evolution: Sequence of transitions (stochastic path) at times Our partial knowledge: Probability distribution P(c,t) evolving deterministically by the master equation.

c1c2c3...c N t1 ,t 2 ,t3 ,... ,t N

〈Ssys(t)〉 = −∑c∈Ωsys P(c,t)ln P(c,t)

Ssys(t) = −ln P(c(t),t) d dt P(c,t) = ∑

c '∈Ω

P(c' ,t)wc' c−P(c,t)wcc'

Configurational entropy Mean entropy

Entropy of the system Entropy of the system

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〈Ssys(t)〉 = − ∑

c∈Ωsys

P(c,t)ln P(c,t) Ssys(t) = −ln P(c(t),t)

Configurational entropy Mean entropy

Entropy of the system Entropy of the system

Change of conf. entropy

˙ Ssys(t) = − ˙ P(c(t),t) P(c(t),t)−∑

j

δ(t−t j)ln P(c j,t) P(c j−1,t)

〈 ˙

Ssys(t)〉 = − ∑

c,c'∈Ωsys

P(c,t)wc →c' ln P(c ,t) P(c' ,t)

Change of mean entropy

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Configurational entropy Environmental entropy Total entropy

S syst = −ln Pc ,t S envt Stot(t)=Ssys(t)+Senv(t)

Environment

System

drive entropy

? ?

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˙ Senv(t) = ∑

j

δ(t−t j)ln ωc j−1 →c j ωc j →c j−1

Andrieux and Gaspard, J. Chem. Phys. 2004

  • U. Seifert, PRL 2005

Commonly accepted formula for the Commonly accepted formula for the environmental entropy environmental entropy

Where does it come from?

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1976

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X 1 X 2 X N

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P(c ,t) [X i](t)

probability concentration

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Schnakenberg: The master equation is mapped to a fictitious chemical system evolving according to the law of mass action (= mean field equation)

Fictitious chemical system Fictitious chemical system d dt P(c ,t) = ∑

c'∈Ω

(P(c' ,t)wc' →c−P(c ,t)wc →c')

Isothermal / isochroric → minimize F.

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Extent of reaction Extent of reaction = average number of forward reactions c→c' minus backward reactions c'→c.

Brief summary of Schnakenbergs argument (1) Brief summary of Schnakenbergs argument (1)

Thermodynamic flux Thermodynamic flux Conjugate thermodynamic force Conjugate thermodynamic force Extent of reaction Extent of reaction ξ ξcc′

cc′

Chemical a nity ffi Chemical a nity ffi

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Compare with → Chemical affinity is chemical potential difference With and we arrive at:

Brief summary of Schnakenbergs argument (2) Brief summary of Schnakenbergs argument (2)

˙ F = ∑

cc'

Acc' ˙ ξcc' = −∑

cc'

Acc' ˙ N cc'

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Brief summary of Schnakenbergs argument (3) Brief summary of Schnakenbergs argument (3)

In the stationary state we have With . Hence turns into

˙ F=∑

cc '

Acc ' ˙ ξcc '

E,T constant

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Brief summary of Schnakenbergs argument (4) Brief summary of Schnakenbergs argument (4) ˙ S=−k B∑

c,c'

ξc ,c' ln [Xc ']wc' →c [Xc]wc →c ' ˙ S = −k B∑

c,c'

ξc ,c' ln [ X c'] [ X c] − k B∑

c,c'

ξc ,c' ln wc' →c wc →c'

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Brief summary of Schnakenbergs argument (4) Brief summary of Schnakenbergs argument (4)

〈 ˙

Ssys(t)〉 = − ∑

c,c'∈Ωsys

P(c,t)wc →c' ln P(c' ,t) P(c ,t)

〈 ˙ Stot〉 = 〈 ˙ Ssys〉 + 〈 ˙ Senv〉 ˙ S=−k B∑

c,c'

ξc ,c' ln [Xc ']wc' →c [Xc]wc →c ' ˙ S = −k B∑

c,c'

ξc ,c' ln [ X c'] [ X c] − k B∑

c,c'

ξc ,c' ln wc' →c wc →c'

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Brief summary of Schnakenbergs argument (4) Brief summary of Schnakenbergs argument (4) 〈 ˙ Stot〉 = 〈 ˙ Ssys〉 + 〈 ˙ Senv〉

〈 ˙

Senv(t)〉 =

c,c'∈Ωsys

P(c,t)wc →c 'ln wc →c ' wc ' →c

˙ S=−k B∑

c,c'

ξc ,c' ln [Xc ']wc' →c [Xc]wc →c ' ˙ S = −k B∑

c,c'

ξc ,c' ln [ X c'] [ X c] − k B∑

c,c'

ξc ,c' ln wc' →c wc →c'

〈 ˙

Ssys(t)〉 = − ∑

c,c'∈Ωsys

P(c,t)wc →c' ln P(c' ,t) P(c ,t)

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Environmental entropy production Environmental entropy production

〈 ˙

Senv(t)〉 =

c,c'∈Ωsys

P(c,t)wc, →c' ln wc →c' wc' →c ˙ Senv(t) = ∑

j

δ(t−t j)ln wc j−1 → c j wc j→c j−1

Important consequence: Irreversible transitions do not exist. In Nature, there are no „absorbing states“.

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tot

Total state space

sys

System state space

Environment

System

drive

Explaining entropy production Explaining entropy production in terms of microstates in terms of microstates

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Simplest example: Simplest example:

Stochastic clock in a stationary state

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Counting the number of cycles, we may think of a linear chain of transitions

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Each configuration corresponds to a certain number of configurations of the environment.

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Assume equal rates among all transitions

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Subsystem is driven by an entropic force.

wcc' wc' c = N c'  N c

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Environmental entropy production

wcc' wc' c = N envc'  N envc  S env = −ln N envc' ln N envc  S env = ln wcc' wc' c

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˙ Senv(t) = ∑

j

δ(t−t j)ln ωc j−1→c j ωc j →c j−1

Question Under which conditions is this formula correct?

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Answer: Answer:

  • The formula is correct if the environment

The formula is correct if the environment equilibrates instantaneously equilibrates instantaneously after each transition. after each transition.

  • In realistic systems this is not necessarily true.

In realistic systems this is not necessarily true.

  • The formula could provide an upper bound in the

The formula could provide an upper bound in the long-time limit (ongoing research) long-time limit (ongoing research)

˙ Senv(t) = ∑

j

δ(t−t j)ln ωc j−1→c j ωc j →c j−1

Question: Question: Under which conditions is Under which conditions is this formula correct? this formula correct?

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// Example: biased random walk const double p=0.3; int x=0; double S_env=0; ... if (rnd()<p) { x++; S_env += ln(p)/ln(1-p) } else { x--; S_env -= ln(p)/ln(1-p); }

Environmental entropy production is easily accessible in numerical simulations.

Whenever the configuration changes, simply add

ln wc→c' wc' →c

p 1-p

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˙ Ssys(t) = − ˙ P(c(t),t) P(c(t),t)−∑

j

δ(t−t j)ln P(c j,t) P(c j−1,t)

˙ Senv(t) = ∑

j

δ(t−t j)ln ωc j →c j+1 ωc j+1→c j

˙ Stot(t) = − ˙ P(c(t),t) P(c(t),t)−∑

j

δ(t−t j)ln P(c j,t)wc j−1→c j P(c j−1,t)wc j →c j−1

No entropy production in the stationary state Detailed balance ↔

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Two equivalent definitions of detailed balance: Two equivalent definitions of detailed balance:

Probability currents in the stationary state cancel pairwise:

∀ c ,c' ∈: Pcwcc' = Pc'wc' c

For each closed stochastic path the product of all rates along this path is equal to the product of the rates in reverse direction

wc1c2wc2c3...wcN −1cN wc N c1 = wcN cN −1wcN −1cN −2...wc2c1wc1cN

c1c2...cN c1

  • does not rely on P(c)
  • difficult to prove
  • easy to disprove
  • requires knowledge of P(c)
  • easy to prove
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  • 2. Fluctuation theorem revisited
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t

Stot(t)

t

ΔStot(t)

Second law: but it fluctuates - sometimes even in opposite direction 〈 S tot 〉 ≥0

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t

Stot(t)

t

ΔStot(t) P(ΔStot) ΔStot

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t

Stot(t)

t

ΔStot(t) P(ΔStot) ΔStot

P S tot P− S tot = e

 Stot

Fluctuation theorem:

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To prove the fluctuation theorem, 1) prove it for a single transition c↔c' 2) show that it will hold for any sequence

  • f transitions

YAP - yet another proof YAP - yet another proof

  • f the fluctuation relation
  • f the fluctuation relation

P(Δ Stot) P(−Δ Stot) = e

Δ Stot

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c c'

First step: Consider a single transition c↔c'

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P(ΔStot) ΔStot

First step: Consider a single transition c↔c'

c c'

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P(ΔStot) ΔStot

 S tot = ln Pcwcc' Pc' wc' c P S tot ∝ Pcwcc' P− S tot ∝ Pc'wc' c P S tot P− S tot = exp S tot

c c'

Fluctuation theorem holds trivially !

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Second step: Show that the FR holds for any sequence. Prove invariance under → convolution:

f x= f −xe

x

gx=g −xe

x

 f ∗gx = ∫ f ( y)g(x−y)dy

= ∫ f (−y)e

y g(−x+y)e x− y

= e

x∫ f (−y)g( y−x)dy

= e

x∫ f ( y)g(−y−x)dy = e x (f ∗g)(−x)

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Fluctuation relation

  • holds exactly for the total entropy
  • holds approximately for the environmental entropy

production in a non-equilibrium steady state in the long time limit

P(Δ Senv) P(−Δ Senv) ≈ exp(Δ Senv) P S tot P− S tot = exp S tot

Distribution itself is system-dependent

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  • 3. Entropy production and renormalization
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Arrow can be interpreted as ' time'

Contact process: A → 2A 2A → A A → 0 Example: Directed percolation (DP) Example: Directed percolation (DP)

Bonds openwith probability p Toy model for epidemic spreading

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Absorbing states Infinite entropy production ↔

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Renormalization scheme for DP by logical OR Renormalization scheme for DP by logical OR

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Let be the probability to find adjacent blocks of size m at time t in the bit pattern p. Example:

P101

(5)

000101001010000001011010110 1 1 0 1 1

Pp

(m)(t)

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Let be the probability to find adjacent blocks of size m at time t in the bit pattern p. Example: In a critical DP process increases with time while all other decrease with time. saturates as

P101

(5)

000101001010000001011010110 1 1 0 1 1

Pp

(m)(t)

P000

(m)(t)

S p

(m)(t) :=

P p

(m)(t)

1−P000

(m)(t)

t →∞

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Perform two limits: Perform two limits:

  • 1. Take time
  • 2. Take block size

Observation: These quantities are universal.

S p

(m) := lim t →∞ S p (m)(t) =

Pp

(m)(t)

1−P000

(m)(t)

t →∞ m→∞ S p

* := lim m→∞ S p (m)

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t →∞

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m→∞

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Useful for:

  • Verification whether a given model belongs to DP
  • Definition of a „clean“ contact process

Number of bits Number of univ. quantities 2 2 3 5 4 9 5 17

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space time

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space time

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space time

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space time

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space time

0 1 → 1 0 →

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space time

0 1 → 1 0 →

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space time

0 1 → 1 0 →

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space time

0 1 → 1 0 →

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space time

0 1 → 1 0 →

w100

w111

Effective transition rates wp in the coarse-grained dynamics

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There are

  • Reversible transitions

110 111 ↔

  • Irreversible transitions

010 000 ↔

  • Impossible transitions

000 010 → The allowed transitions are expected to decrease with increasing block size. Example: Effective 3-bit rates Example: Effective 3-bit rates

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Example: Effective 3-bit rates Example: Effective 3-bit rates

m=4 m=32

t →∞

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Example: Effective 3-bit rates Example: Effective 3-bit rates

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Example: Effective 3-bit rates Example: Effective 3-bit rates Observation:

  • 1. The irreversible rates decrease faster than

the reversible rates with increasing block size.

w p

rev∼m −2,

w p

irr∼m −2.6

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Example: Effective 3-bit Example: Effective 3-bit currents currents

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Example: Effective 3-bit Example: Effective 3-bit currents currents

m→∞

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Observation: Observation:

  • 1. The irreversible currents decrease faster than

the reversible currents with increasing block size.

  • 2. The reversible currents approach each other

as if they would satisfy detailed balance in the limit

J p

rev∼m −2,

J p

irr∼m −2.6

m→∞

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Summary

  • The commonly accepted formula for environmental

entropy production holds only if the environment equilibrates instantaneously.

  • The fluctuation theorem is a property that it is invariant

under convolution.

  • It is very difficult (although not impossible) to find other

physical quantities which obey the fluctuation theorem.

  • Directed percolation has infinite entropy production.

Under block renormalization, however, the currents of irreversible transitions vanish faster while reversible transitions seem to approach detailed balance.