Telegraph equation from the six-vertex model Vadim Gorin MIT - - PowerPoint PPT Presentation

telegraph equation from the six vertex model
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Telegraph equation from the six-vertex model Vadim Gorin MIT - - PowerPoint PPT Presentation

Telegraph equation from the six-vertex model Vadim Gorin MIT (Cambridge) and IITP (Moscow) July 2018 Telegraph equation Resistance R Inductance L Capacitance C Conductance G Wiki/Pixabay


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SLIDE 1

Telegraph equation from the six-vertex model

Vadim Gorin MIT (Cambridge) and IITP (Moscow)

July 2018

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SLIDE 2

Telegraph equation

Resistance R Inductance L Capacitance C Conductance G

  • Wiki/Pixabay

Voltage V Current I ∂V ∂x (x, t) = − L · ∂I ∂t (x, t) − R · I(x, t) ∂I ∂x (x, t) = − C · ∂V ∂t (x, t) − G · V(x, t)

  • r

Vxx − LC · Vtt − (RC + GL) · Vt − GR · V = 0

  • Wave equation
  • Effect of losses
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SLIDE 3

Six–vertex model

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H

Square grid with O in the vertices and H on the edges.

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SLIDE 4

Six–vertex model

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H

Square grid with O in the vertices and H on the edges. Finite/infinite domain.

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SLIDE 5

Six–vertex model

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H

Square grid with O in the vertices and H on the edges. Finite/infinite domain. Configurations: possible matchings

  • f all atoms inside domain into

H2O molecules. This is square ice model. Real-world ice has somewhat similar (although 3d) structure.

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SLIDE 6

Six–vertex model

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H

Square grid with O in the vertices and H on the edges. Finite/infinite domain. Configurations: possible matchings

  • f all atoms inside domain into

H2O molecules. This is square ice model. Real-world ice has somewhat similar (although 3d) structure. Also known as six vertex model.

O O O H H H H O O H O H H H H H H H

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SLIDE 7

Six–vertex model: Gibbs measures

O O O H H H H O O H O H H H H H H

a1 a2

H

b1 b2 c1 c2

Statistical mechanics starting from (Lieb–67):

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H

Assign Gibbs weights a#(a1)

1

a#(a2)

2

b#(b1)

1

b#(b2)

2

c#(c1)

1

c#(c2)

2

Z(a1, a2, b1, b2, c1, c2)

[ Depends only on b1b2

a1a2 and c1c2 a1a2 .]

Asymptotic properties of Gibbs measures?

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SLIDE 8

Six–vertex model: Gibbs measures

O O O H H H H O O H O H H H H H H

a1 a2

H

b1 b2 c1 c2

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H

Assign Gibbs weights a#(a1)

1

a#(a2)

2

b#(b1)

1

b#(b2)

2

c#(c1)

1

c#(c2)

2

Z(a1, a2, b1, b2, c1, c2)

[ Depends only on b1b2

a1a2 and c1c2 a1a2 .]

Asymptotic properties of Gibbs measures? Understanding is still very limited.

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SLIDE 9

Question for today

Telegraph equation Vxx − Vtt − αVt − βVx − γV = 0

  • Six–vertex model

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H a#(a1)

1

a#(a2)

2

b#(b1)

1

b#(b2)

2

c#(c1)

1

c#(c2)

2

Z(a1,a2,b1,b2,c1,c2)

What do they have in common?

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SLIDE 10

Stochastic six–vertex model

O O O H H H H O O H O H H H H H H H

a1 a2 b1 b2 c1 c2

An equivalent representation Collection of paths on the plane

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SLIDE 11

Stochastic six–vertex model

O O O H H H H O O H O H H H H H H H

1 1 b1 b2 1 − b1 1 − b2

Assumption: (Gwa–Spohn–92) a1 = a2 = 1, b1 + c1 = 1, b2 + c2 = 1

  • Implies

∆ = a1a2+b1b2−c1c2

2√a1a2b1b2

≥ 1

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SLIDE 12

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Take arbitrary boundary conditions in the quadrant

1 2 3 4 5 . . . 1 2 3

. . .

4 5

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SLIDE 13

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

b1 1 − b1 choice

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SLIDE 14

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

no choice

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SLIDE 15

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

no choice

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SLIDE 16

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

no choice

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SLIDE 17

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

choice b2 1 − b2

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SLIDE 18

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

no choice

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SLIDE 19

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

b1 1 − b1 choice

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SLIDE 20

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

choice b2 1 − b2

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SLIDE 21

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

choice b2 1 − b2

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SLIDE 22

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Proceed with sequential stochastic sampling

1 2 3 4 5 . . . 1 2 3

. . .

4 5

b1 1 − b1 choice

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SLIDE 23

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

Until the quadrant is filled

1 2 3 4 5 . . . 1 2 3

. . .

4 5

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SLIDE 24

Stochastic six–vertex model

1 1 b1 b2 1 − b1 1 − b2

The resulting paths are level lines of the height function

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

  • Height is 0 at

the origin,

  • increases up,
  • decreases to the

right.

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SLIDE 25

Domain–wall and fixed weights

1 2 3 4 5 . . . 1 2 3

. . .

4 1 2 3 4 1 1 1 1 1 1 2 2 2 2 1 3 5 4 3 2 2 5

b1 b2

s = 1 − b1 1 − b2 1 LH(Lx, Ly) → h(x, y) =          0,

x y > s−1,

(√sx − √y)2 1 − s , s ≤ x

y ≤ s−1

y − x,

x y < s.

  • Theorem. (Borodin–Corwin–Gorin-14) For domain–wall boundary

conditions and fixed 0 < b2 < b1 < 1, 1

LH(Lx, Ly) → h(x, y) with

fluctuations on L1/3 scale given by the Tracy–Widom distribution. TW = universal law for the largest eigenvalue of Hermitian matrices and for particle system in Kardar–Parisi–Zhang class

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SLIDE 26

Domain–wall and fixed weights

1 2 3 4 5 . . . 1 2 3

. . .

4 1 2 3 4 1 1 1 1 1 1 2 2 2 2 1 3 5 4 3 2 2 5

b1 b2

s = 1 − b1 1 − b2 1 LH(Lx, Ly) → h(x, y) =          0,

x y > s−1,

(√sx − √y)2 1 − s , s ≤ x

y ≤ s−1

y − x,

x y < s.

  • Theorem. (Borodin–Corwin–Gorin-14) For domain–wall boundary

conditions and fixed 0 < b2 < b1 < 1, 1

LH(Lx, Ly) → h(x, y) with

fluctuations on L1/3 scale given by the Tracy–Widom distribution. ρx · s + ρy · (s + (s − 1)ρ)2 = 0, ρ = hx.

1st–order non-linear PDE (Gwa–Spohn–92) (Reshetikhin–Sridhar–16)

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SLIDE 27

Domain–wall and fixed weights

1 2 3 4 5 . . . 1 2 3

. . .

4 1 2 3 4 1 1 1 1 1 1 2 2 2 2 1 3 5 4 3 2 2 5

b1 b2

s = 1 − b1 1 − b2 1 LH(Lx, Ly) → h(x, y) =          0,

x y > s−1,

(√sx − √y)2 1 − s , s ≤ x

y ≤ s−1

y − x,

x y < s.

ρx · s + ρy · (s + (s − 1)ρ)2 = 0, ρ = hx

  • Instead of b1, b2, only s. Where is the second parameter?
  • Where is the linear telegraph equation?
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SLIDE 28

Domain–wall and fixed weights

1 2 3 4 5 . . . 1 2 3

. . .

4 1 2 3 4 1 1 1 1 1 1 2 2 2 2 1 3 5 4 3 2 2 5

b1 b2

s = 1 − b1 1 − b2 1 LH(Lx, Ly) → h(x, y) =          0,

x y > s−1,

(√sx − √y)2 1 − s , s ≤ x

y ≤ s−1

y − x,

x y < s.

ρx · s + ρy · (s + (s − 1)ρ)2 = 0, ρ = hx

  • Instead of b1, b2, only s. Where is the second parameter?
  • Where is the linear telegraph equation?

(Borodin–Gorin–18): One needs to rescale weights b1, b2.

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SLIDE 29

Rescaled weights: Law of Large Numbers

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3 b1 b2 Low density of corners b1 = exp

  • − β1

L

  • b2 = exp
  • − β2

L

  • q =
  • b2

b1

L = eβ1−β2

  • Theorem. (Borodin–Gorin–18) For arbitrary boundary conditions and

rescaled weights, 1

LH(Lx, Ly) → h(x, y) with

∂2 ∂x∂y

  • qh(x,y)

+ β2 ∂ ∂x

  • qh(x,y)

+ β1 ∂ ∂y

  • qh(x,y)

= 0, qh(x,0) = χ(x), qh(0,y) = ψ(y).

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SLIDE 30

Rescaled weights: Law of Large Numbers

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3 b1 b2 Low density of corners b1 = exp

  • − β1

L

  • b2 = exp
  • − β2

L

  • q =
  • b2

b1

L = eβ1−β2

  • qh(x,y)

xy + β2

  • qh(x,y)

x + β1

  • qh(x,y)

y = 0

qh(x,0) = χ(x), qh(0,y) = ψ(y).

  • In t = x + y, z = x − y, a version of the Telegraph equation.
  • Characteristic Cauchy problem has a unique solution.
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SLIDE 31

Rescaled weights: Law of Large Numbers

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

b1 b2

Low density of corners b1 = exp

  • − β1

L

  • b2 = exp
  • − β2

L

  • q =
  • b2

b1

L = eβ1−β2

  • qh(x,y)

xy + β2

  • qh(x,y)

x + β1

  • qh(x,y)

y = 0

2nd order hyperbolic limit shape equation is strange:

  • Diffusions: parabolic equations (e.g. Brownian motion)
  • Interacting particle systems: 1st order equations (e.g. TASEP)
  • 2d statistical mechanics: 2nd order elliptic Euler–Lagrange equations

through variational principles (e.g. random tilings)

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SLIDE 32

Rescaled weights: Fluctuations

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

b1 b2

b1 = exp

  • −β1

L

  • b2 = exp
  • −β2

L

  • q = b2

b1 = q1/L 1 LH(Lx, Ly) → h(x, y). What about fluctuations H(Lx, Ly) − EH(Lx, Ly)?

  • Reminder. For fixed b1, b2, they were Tracy–Widom on L1/3 scale.
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SLIDE 33

Rescaled weights: Fluctuations

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

b1 b2

b1 = exp

  • −β1

L

  • b2 = exp
  • −β2

L

  • q = b2

b1 = q1/L

  • Claim. H(Lx, Ly) − EH(Lx, Ly) ≈ L1/2 × Gaussian.
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SLIDE 34

Rescaled weights: Fluctuations

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

b1 b2

b1 = exp

  • −β1

L

  • b2 = exp
  • −β2

L

  • q = b2

b1 = q1/L

  • Claim. H(Lx, Ly) − EH(Lx, Ly) ≈ L1/2 × Gaussian.
  • Theorem. (Borodin–Gorin–18, Shen–Tsai–18)

lim

L→∞

√ L

  • qH(Lx,Ly) − EqH(Lx,Ly)

solves Stochastic Telegraph φxy + β2φx + β1φy = ˙ W

  • V (x, y)

V (x, y) = (β1 + β2)qh

xqh y + (β2 − β1)β2qhqh x − (β2 − β1)β1qhqh y

R.H.S.=2d white noise × non-linear functional of the limit shape

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SLIDE 35

Six–vertex and Telegraph

  • 1

2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

Stochastic six–vertex model in the quadrant in low corner density asymptotic regime.

  • Deterministic limit (LLN) for

qH(x,y) is given by the homogeneous Telegraph equation.

  • Gaussian fluctuations (CLT)

are given by Stochastic Telegraph equation. Why?

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SLIDE 36

Feynman–Kac for Heat equation

For a second, switch to (parabolic) Heat equation. Ht = 1 2Hxx, t ≥ 0, H(0, x) = f (x). The Feynman–Kac formula expresses the solution: H(t, x) = Ef (Bt), where Bt is the Brownian motion started at B0 = x. Similar representation is possible for the Telegraph equation!

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SLIDE 37

Feynman–Kac for Telegraph

Persistent random walk.

intensity β1 intensity β2

Turns down/to the left at Poisson random times.

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SLIDE 38

Feynman–Kac for Telegraph

Persistent random walk.

intensity β1 intensity β2

Turns down/to the left at Poisson random times.

(X, Y )

ˆ x ˆ y

+ + −

  • Theorem. (Borodin–Gorin–18; following Goldstein–51, Kac–74)

φxy + β2φx + β1φy = u, x, y > 0; φ(x, 0) = χ(x), φ(0, y) = ψ(y). Then random characteristics solve the inhomogeneous Telegraph: φ(X, Y ) = Eχ(ˆ x) + Eψ(ˆ y) + E X Y I±

between(x, y)u(x, y)dxdy

  • .
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SLIDE 39

Six–vertex and persistent random walks

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

b1 b2

b1 = exp

  • −β1

L

  • b2 = exp
  • −β2

L

  • If paths are rare (low density limit), then each of them becomes a

persistent random walk. They are essentially independent.

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SLIDE 40

Six–vertex and persistent random walks

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

b1 b2

b1 = exp

  • −β1

L

  • b2 = exp
  • −β2

L

  • If paths are rare (low density limit), then each of them becomes a

persistent random walk. They are essentially independent.

  • Conclusion. LLN/CLT for the height at low density is the same as

LLN/CLT for a family of independent persistent random walks. Hence, connection to the Telegraph equation.

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SLIDE 41

Six–vertex and persistent random walks

1 2 3 4 5 . . . 1 2 3

. . .

4 5

−1 −1 −2 1 2 1 2 3

b1 b2

b1 = exp

  • −β1

L

  • b2 = exp
  • −β2

L

  • If paths are rare (low density limit), then each of them becomes a

persistent random walk. They are essentially independent.

  • Conclusion. LLN/CLT for the height at low density is the same as

LLN/CLT for a family of independent persistent random walks. Hence, connection to the Telegraph equation. How to explain the same connection at high densities and the appearance of qH(x,y)?

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SLIDE 42

Summary

O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H O O O O O H H H H H H H H H H H H H H H H H H H H H H H H

φxy + β2φx + β1φy = ˙ W √ V

1 2 3 4 5 . . . 1 2 3

. . .

4 5

b1 1 − b1 choice

  • Stochastic six–vertex model

in the rare corners regime unexpectedly connects to hyperbolic PDEs.

  • lim

L→∞ qH(Lx,Ly) solves

Telegraph equation.

  • q → 0: fixed weights 1st order

nonlinear PDE for LLN.

  • lim

L→∞

√ L(qH − EqH) — Stochastic Telegraph.

  • Links to persistent random

walks — Feynman–Kac formula for Telegraph.

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SLIDE 43

Main tool: four point relation

Proofs rely on exact discrete analogue of stochastic Telegraph.

1 1 b1 b2 1 − b1 1 − b2

H H H H H H H + 1 H − 1 H + 1 H H + 1 H H − 1 H H H − 1 H H − 1

  • Theorem. (Borodin–Gorin–18; with help of Wheeler) For the stochastic

six–vertex model in the quadrant with arbitrary boundary conditions, and each x, y = 1, 2, . . . , set for q = b2

b1 :

ξ(x, y) = qH(x,y) − b1qH(x−1,y) − b2qH(x,y−1) + (b1 + b2 − 1)qH(x−1,y−1). Then ξ is a martingale with explicit variance:

  • 1. E [ξ(x, y) | H(u, v), u < x or v < y] = 0.
  • 2. E
  • ξ2(x, y) | H(u, v), u < x or v < y
  • =
  • b1(1 − b1) + b1(1 − b2)
  • ∆x∆y + b1(1 − b2)(1 − q)qH(x,y)∆x − b1(1 − b1)(1 − q)qH(x,y)∆y,

with ∆x = qH(x,y−1) − qH(x−1,y−1), ∆y = qH(x−1,y) − qH(x−1,y−1)