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Quantum Gravity in Paris, Mar. 20, 2013 Generalized CDT as a scaling limit of planar maps Timothy Budd (collaboration with J. Ambjørn) Niels Bohr Institute, Copenhagen. [email protected] http://www.nbi.dk/ ~ budd/

Generalized CDT as a scaling limit of planar maps

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Page 1: Generalized CDT as a scaling limit of planar maps

Quantum Gravity in Paris,Mar. 20, 2013

Generalized CDT as ascaling limit of planar maps

Timothy Budd

(collaboration with J. Ambjørn)

Niels Bohr Institute, [email protected]

http://www.nbi.dk/~budd/

Page 2: Generalized CDT as a scaling limit of planar maps

Outline

I Introduction to (generalized) CDT in 2d

I Enumeration using labeled trees

I Continuum limit and two-point function

I Scaling limit of planar maps

I Loop identities

Page 3: Generalized CDT as a scaling limit of planar maps

Causal Dynamical Triangulations in 2d

I CDT in 2d is a statistical system with partition function

ZCDT =∑T

1

CTgN(T )

I ZCDT (g) is a generating function for the number of causaltriangulations T of S2 with N triangles.

I The triangulations have a foliatedstructure

I May as well view them as causalquadrangulations with a uniquelocal maximum of the distancefunction from the origin.

I What if we allow more than onelocal maximum?

t

Page 4: Generalized CDT as a scaling limit of planar maps

Causal Dynamical Triangulations in 2d

I CDT in 2d is a statistical system with partition function

ZCDT =∑T

1

CTgN(T )

I ZCDT (g) is a generating function for the number of causaltriangulations T of S2 with N triangles.

I The triangulations have a foliatedstructure

I May as well view them as causalquadrangulations with a uniquelocal maximum of the distancefunction from the origin.

I What if we allow more than onelocal maximum?

t

Page 5: Generalized CDT as a scaling limit of planar maps

Causal Dynamical Triangulations in 2d

I CDT in 2d is a statistical system with partition function

ZCDT =∑T

1

CTgN(T )

I ZCDT (g) is a generating function for the number of causaltriangulations T of S2 with N triangles.

I The triangulations have a foliatedstructure

I May as well view them as causalquadrangulations with a uniquelocal maximum of the distancefunction from the origin.

I What if we allow more than onelocal maximum?

t

Page 6: Generalized CDT as a scaling limit of planar maps

Causal Dynamical Triangulations in 2d

I CDT in 2d is a statistical system with partition function

ZCDT =∑T

1

CTgN(T )

I ZCDT (g) is a generating function for the number of causaltriangulations T of S2 with N triangles.

I The triangulations have a foliatedstructure

I May as well view them as causalquadrangulations with a uniquelocal maximum of the distancefunction from the origin.

I What if we allow more than onelocal maximum?

t

Page 7: Generalized CDT as a scaling limit of planar maps

Generalized CDTI Allow spatial topology to change in time.

Assign a coupling gs to each baby universe.

I The model was solved in the continuum bygluing together chunks of CDT. [Ambjørn,

Loll, Westra, Zohren ’07]

I Can we understand the geometry in moredetail by obtaining generalized CDT as ascaling limit of a discrete model?

I Generalized CDT partition function

Z (g , g) =∑Q

1

CQgNgNmax ,

sum over quadrangulations Q withN faces, a marked origin, and Nmax

local maxima of the distance to theorigin.

−→

Page 8: Generalized CDT as a scaling limit of planar maps

Generalized CDTI Allow spatial topology to change in time.

Assign a coupling gs to each baby universe.

I The model was solved in the continuum bygluing together chunks of CDT. [Ambjørn,

Loll, Westra, Zohren ’07]

I Can we understand the geometry in moredetail by obtaining generalized CDT as ascaling limit of a discrete model?

I Generalized CDT partition function

Z (g , g) =∑Q

1

CQgNgNmax ,

sum over quadrangulations Q withN faces, a marked origin, and Nmax

local maxima of the distance to theorigin.

−→

Page 9: Generalized CDT as a scaling limit of planar maps

Generalized CDTI Allow spatial topology to change in time.

Assign a coupling gs to each baby universe.

I The model was solved in the continuum bygluing together chunks of CDT. [Ambjørn,

Loll, Westra, Zohren ’07]

I Can we understand the geometry in moredetail by obtaining generalized CDT as ascaling limit of a discrete model?

I Generalized CDT partition function

Z (g , g) =∑Q

1

CQgNgNmax ,

sum over quadrangulations Q withN faces, a marked origin, and Nmax

local maxima of the distance to theorigin.

−→

Page 10: Generalized CDT as a scaling limit of planar maps

Generalized CDTI Allow spatial topology to change in time.

Assign a coupling gs to each baby universe.

I The model was solved in the continuum bygluing together chunks of CDT. [Ambjørn,

Loll, Westra, Zohren ’07]

I Can we understand the geometry in moredetail by obtaining generalized CDT as ascaling limit of a discrete model?

I Generalized CDT partition function

Z (g , g) =∑Q

1

CQgNgNmax ,

sum over quadrangulations Q withN faces, a marked origin, and Nmax

local maxima of the distance to theorigin.

−→

Page 11: Generalized CDT as a scaling limit of planar maps

Generalized CDTI Allow spatial topology to change in time.

Assign a coupling gs to each baby universe.

I The model was solved in the continuum bygluing together chunks of CDT. [Ambjørn,

Loll, Westra, Zohren ’07]

I Can we understand the geometry in moredetail by obtaining generalized CDT as ascaling limit of a discrete model?

I Generalized CDT partition function

Z (g , g) =∑Q

1

CQgNgNmax ,

sum over quadrangulations Q withN faces, a marked origin, and Nmax

local maxima of the distance to theorigin.

−→

Page 12: Generalized CDT as a scaling limit of planar maps

N = 2000, g = 0, Nmax = 1

Page 13: Generalized CDT as a scaling limit of planar maps

N = 5000, g = 0.00007, Nmax = 12

Page 14: Generalized CDT as a scaling limit of planar maps

N = 7000, g = 0.0002, Nmax = 38

Page 15: Generalized CDT as a scaling limit of planar maps

N = 7000, g = 0.004, Nmax = 221

Page 16: Generalized CDT as a scaling limit of planar maps

N = 4000, g = 0.02, Nmax = 362

Page 17: Generalized CDT as a scaling limit of planar maps

N = 2500, g = 1, Nmax = 1216

Page 18: Generalized CDT as a scaling limit of planar maps

Causal triangulations and trees

I Union of all left-most geodesicsrunning away from the origin.

I Simple enumeration of planar trees:

#

{ }N

= C (N), C (N) =1

N + 1

(2NN

)[Malyshev, Yambartsev, Zamyatin ’01]

[Krikun, Yambartsev ’08]

[Durhuus, Jonsson, Wheater ’09]

I Union of all left-most geodesicsrunning towards the origin.

I Both generalize to generalized CDTleading to different representations.

Page 19: Generalized CDT as a scaling limit of planar maps

Causal triangulations and treesI Union of all left-most geodesics

running away from the origin.

I Simple enumeration of planar trees:

#

{ }N

= C (N), C (N) =1

N + 1

(2NN

)[Malyshev, Yambartsev, Zamyatin ’01]

[Krikun, Yambartsev ’08]

[Durhuus, Jonsson, Wheater ’09]

I Union of all left-most geodesicsrunning towards the origin.

I Both generalize to generalized CDTleading to different representations.

Page 20: Generalized CDT as a scaling limit of planar maps

Causal triangulations and treesI Union of all left-most geodesics

running away from the origin.

I Simple enumeration of planar trees:

#

{ }N

= C (N), C (N) =1

N + 1

(2NN

)[Malyshev, Yambartsev, Zamyatin ’01]

[Krikun, Yambartsev ’08]

[Durhuus, Jonsson, Wheater ’09]

I Union of all left-most geodesicsrunning towards the origin.

I Both generalize to generalized CDTleading to different representations.

Page 21: Generalized CDT as a scaling limit of planar maps

Causal triangulations and treesI Union of all left-most geodesics

running away from the origin.

I Simple enumeration of planar trees:

#

{ }N

= C (N), C (N) =1

N + 1

(2NN

)[Malyshev, Yambartsev, Zamyatin ’01]

[Krikun, Yambartsev ’08]

[Durhuus, Jonsson, Wheater ’09]

I Union of all left-most geodesicsrunning towards the origin.

I Both generalize to generalized CDTleading to different representations.

Page 22: Generalized CDT as a scaling limit of planar maps

Causal triangulations and treesI Union of all left-most geodesics

running away from the origin.

I Simple enumeration of planar trees:

#

{ }N

= C (N), C (N) =1

N + 1

(2NN

)[Malyshev, Yambartsev, Zamyatin ’01]

[Krikun, Yambartsev ’08]

[Durhuus, Jonsson, Wheater ’09]

I Union of all left-most geodesicsrunning towards the origin.

I Both generalize to generalized CDTleading to different representations.

Page 23: Generalized CDT as a scaling limit of planar maps

Causal triangulations and trees

I Labeled planar trees: Schaeffer’s bijection.

I Unlabeled planar maps (one face per localmaximum).

Page 24: Generalized CDT as a scaling limit of planar maps

Causal triangulations and trees

I Labeled planar trees: Schaeffer’s bijection.

I Unlabeled planar maps (one face per localmaximum).

Page 25: Generalized CDT as a scaling limit of planar maps

Causal triangulations and trees

I Labeled planar trees: Schaeffer’s bijection.

I Unlabeled planar maps (one face per localmaximum).

Page 26: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

I Quadrangulation

→ mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 27: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

I Quadrangulation → mark a point

→ distance labeling → apply rules→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 28: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling

→ apply rules→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 29: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules

→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 30: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules

→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 31: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules

→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 32: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 33: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 34: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection

7

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4

6

5

[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree

→ add squares → identify corners → quadrangulation.

Page 35: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection

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5

[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree → add squares

→ identify corners → quadrangulation.

Page 36: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection

7

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57

6

6

4

6

4

6

5

[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree → add squares → identify corners

→ quadrangulation.

Page 37: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection

7

6

6

6

8

6

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8

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7

7

7

57

6

6

4

6

4

6

5

[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree → add squares → identify corners

→ quadrangulation.

Page 38: Generalized CDT as a scaling limit of planar maps

The Cori–Vauquelin–Schaeffer bijection[Cori, Vauquelin, ’81]

[Schaeffer, ’98]

t t

t + 1

t - 1

t t

t + 1

t + 1

I Quadrangulation → mark a point → distance labeling → apply rules→ labelled tree.

I Labelled tree → add squares → identify corners → quadrangulation.

Page 39: Generalized CDT as a scaling limit of planar maps

Rooting the tree [e.g. Chassaing, Schaeffer ’04]

I We will be using the bijection:{Quadrangulations with originand marked edge

}↔{

Rooted planar treeslabelled by +, 0,−

}

Page 40: Generalized CDT as a scaling limit of planar maps

Rooting the tree [e.g. Chassaing, Schaeffer ’04]

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4

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4

6

5

I We will be using the bijection:{Quadrangulations with originand marked edge

}↔{

Rooted planar treeslabelled by +, 0,−

}

Page 41: Generalized CDT as a scaling limit of planar maps

Rooting the tree [e.g. Chassaing, Schaeffer ’04]

7

6

6

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6

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6

6

4

6

4

6

5

I We will be using the bijection:{Quadrangulations with originand marked edge

}↔{

Rooted planar treeslabelled by +, 0,−

}

Page 42: Generalized CDT as a scaling limit of planar maps

Rooting the tree [e.g. Chassaing, Schaeffer ’04]

+-

-

-

0

-

-

-

0+

-

-

0

-+

-

-

0

-

-

0

-

-

-

0

0

-

-

-

-

-

-

0

0

-

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--

-

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-

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0

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0-

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7

57

6

6

4

6

4

6

5

I We will be using the bijection:{Quadrangulations with originand marked edge

}↔{

Rooted planar treeslabelled by +, 0,−

}

Page 43: Generalized CDT as a scaling limit of planar maps

Rooting the tree [e.g. Chassaing, Schaeffer ’04]

+-

-

-

0

-

-

-

0+

-

-

0

-+

-

-

0

-

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0

-

-

-

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0

-

-

-

-

-

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-

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-

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-

0-

-

-

-

-

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-

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-

-

-

I We will be using the bijection:{Quadrangulations with originand marked edge

}↔{

Rooted planar treeslabelled by +, 0,−

}

Page 44: Generalized CDT as a scaling limit of planar maps

Assigning couplings to local maxima

I Assign coupling g to the local maxima of thedistance function.

I In terms of labeled trees:

5 4

44

4

4 4

5

3

3

5

5

I Generating function z0(g , g) for number of rooted labeled trees withN edges and Nmax local maxima.

I Similarly z1(g , g) but local maximum at the root not counted.

I Satisfy recursion relations:

z1 =∞∑k=0

(z1 + z0 + z0)k gk = (1− gz1 − 2gz0)−1

z0 =∞∑k=0

(z1 + z0 + z0)k gk + (g− 1)∞∑k=0

(z1 + z0)k gk

= z1 + (g− 1) (1− gz1 − gz0)−1

Page 45: Generalized CDT as a scaling limit of planar maps

Assigning couplings to local maxima

I Assign coupling g to the local maxima of thedistance function.

I In terms of labeled trees:

5 4

44

4

4 4

5

3

3

5

5

I Generating function z0(g , g) for number of rooted labeled trees withN edges and Nmax local maxima.

I Similarly z1(g , g) but local maximum at the root not counted.

I Satisfy recursion relations:

z1 =∞∑k=0

(z1 + z0 + z0)k gk = (1− gz1 − 2gz0)−1

z0 =∞∑k=0

(z1 + z0 + z0)k gk + (g− 1)∞∑k=0

(z1 + z0)k gk

= z1 + (g− 1) (1− gz1 − gz0)−1

Page 46: Generalized CDT as a scaling limit of planar maps

Assigning couplings to local maxima

I Assign coupling g to the local maxima of thedistance function.

I In terms of labeled trees:

5 4

44

4

4 4

5

3

3

5

5

I Generating function z0(g , g) for number of rooted labeled trees withN edges and Nmax local maxima.

I Similarly z1(g , g) but local maximum at the root not counted.

I Satisfy recursion relations:

z1 =∞∑k=0

(z1 + z0 + z0)k gk = (1− gz1 − 2gz0)−1

z0 =∞∑k=0

(z1 + z0 + z0)k gk + (g− 1)∞∑k=0

(z1 + z0)k gk

= z1 + (g− 1) (1− gz1 − gz0)−1

Page 47: Generalized CDT as a scaling limit of planar maps

Assigning couplings to local maxima

I Assign coupling g to the local maxima of thedistance function.

I In terms of labeled trees:

5 4

4

5

5

5

I Generating function z0(g , g) for number of rooted labeled trees withN edges and Nmax local maxima.

I Similarly z1(g , g) but local maximum at the root not counted.

I Satisfy recursion relations:

z1 =∞∑k=0

(z1 + z0 + z0)k gk = (1− gz1 − 2gz0)−1

z0 =∞∑k=0

(z1 + z0 + z0)k gk + (g− 1)∞∑k=0

(z1 + z0)k gk

= z1 + (g− 1) (1− gz1 − gz0)−1

Page 48: Generalized CDT as a scaling limit of planar maps

Assigning couplings to local maxima

I Assign coupling g to the local maxima of thedistance function.

I In terms of labeled trees:

+�0

0�-

0�-

0�-

0�-

I Generating function z0(g , g) for number of rooted labeled trees withN edges and Nmax local maxima.

I Similarly z1(g , g) but local maximum at the root not counted.

I Satisfy recursion relations:

z1 =∞∑k=0

(z1 + z0 + z0)k gk = (1− gz1 − 2gz0)−1

z0 =∞∑k=0

(z1 + z0 + z0)k gk + (g− 1)∞∑k=0

(z1 + z0)k gk

= z1 + (g− 1) (1− gz1 − gz0)−1

Page 49: Generalized CDT as a scaling limit of planar maps

Assigning couplings to local maxima

I Assign coupling g to the local maxima of thedistance function.

I In terms of labeled trees:

+�0

0�-

0�-

0�-

0�-

I Generating function z0(g , g) for number of rooted labeled trees withN edges and Nmax local maxima.

I Similarly z1(g , g) but local maximum at the root not counted.

I Satisfy recursion relations:

z1 =∞∑k=0

(z1 + z0 + z0)k gk = (1− gz1 − 2gz0)−1

z0 =∞∑k=0

(z1 + z0 + z0)k gk + (g− 1)∞∑k=0

(z1 + z0)k gk

= z1 + (g− 1) (1− gz1 − gz0)−1

Page 50: Generalized CDT as a scaling limit of planar maps

Assigning couplings to local maxima

I Assign coupling g to the local maxima of thedistance function.

I In terms of labeled trees:

+�0

0�-

0�-

0�-

0�-

I Generating function z0(g , g) for number of rooted labeled trees withN edges and Nmax local maxima.

I Similarly z1(g , g) but local maximum at the root not counted.

I Satisfy recursion relations:

z1 =∞∑k=0

(z1 + z0 + z0)k gk = (1− gz1 − 2gz0)−1

z0 =∞∑k=0

(z1 + z0 + z0)k gk + (g− 1)∞∑k=0

(z1 + z0)k gk

= z1 + (g− 1) (1− gz1 − gz0)−1

Page 51: Generalized CDT as a scaling limit of planar maps

z1 = (1− gz1 − 2gz0)−1

z0 = z1 + (g− 1) (1− gz1 − gz0)−1

I Combine into one equation for z1(g , g):

3g2z41 − 4gz3

1 + (1 + 2g(1− 2g))z21 − 1 = 0

I Phase diagram for weighted labeled trees (constant g):

g = 0g = 1

Page 52: Generalized CDT as a scaling limit of planar maps

z1 = (1− gz1 − 2gz0)−1

z0 = z1 + (g− 1) (1− gz1 − gz0)−1

I Combine into one equation for z1(g , g):

3g2z41 − 4gz3

1 + (1 + 2g(1− 2g))z21 − 1 = 0

I Phase diagram for weighted labeled trees (constant g):

g = 0g = 1

Page 53: Generalized CDT as a scaling limit of planar maps

z1 = (1− gz1 − 2gz0)−1

z0 = z1 + (g− 1) (1− gz1 − gz0)−1

I Combine into one equation for z1(g , g):

3g2z41 − 4gz3

1 + (1 + 2g(1− 2g))z21 − 1 = 0

I Phase diagram for weighted labeled trees (constant g):

g = 0g = 1

Page 54: Generalized CDT as a scaling limit of planar maps

z1 = (1− gz1 − 2gz0)−1

z0 = z1 + (g− 1) (1− gz1 − gz0)−1

I Combine into one equation for z1(g , g):

3g2z41 − 4gz3

1 + (1 + 2g(1− 2g))z21 − 1 = 0

I Phase diagram for weighted labeled trees (constant g):

g = 0g = 1

Page 55: Generalized CDT as a scaling limit of planar maps

I The number of local maxima Nmax(g) scales with N at the criticalpoint,

〈Nmax(g)〉NN

= 2(g

2

)2/3

+O(g),〈Nmax(g = 1)〉N

N= 1/2

I Therefore, to obtain a finite continuum density of critical points oneshould scale g ∝ N−3/2, i.e. g = gsε

3 as observed in [ALWZ ’07].

I This is the only scaling leading to a continuum limit qualitativelydifferent from DT and CDT.

I Continuum limit g = gc(g)(1− Λε2),z1 = z1,c(1− Z1ε), g = gsε

3:

Z 31 −

(Λ + 3

(gs2

)2/3)Z1 − gs = 0

I Can compute:

Page 56: Generalized CDT as a scaling limit of planar maps

I The number of local maxima Nmax(g) scales with N at the criticalpoint,

〈Nmax(g)〉NN

= 2(g

2

)2/3

+O(g),〈Nmax(g = 1)〉N

N= 1/2

I Therefore, to obtain a finite continuum density of critical points oneshould scale g ∝ N−3/2, i.e. g = gsε

3 as observed in [ALWZ ’07].

I This is the only scaling leading to a continuum limit qualitativelydifferent from DT and CDT.

I Continuum limit g = gc(g)(1− Λε2),z1 = z1,c(1− Z1ε), g = gsε

3:

Z 31 −

(Λ + 3

(gs2

)2/3)Z1 − gs = 0

I Can compute:

Page 57: Generalized CDT as a scaling limit of planar maps

I The number of local maxima Nmax(g) scales with N at the criticalpoint,

〈Nmax(g)〉NN

= 2(g

2

)2/3

+O(g),〈Nmax(g = 1)〉N

N= 1/2

I Therefore, to obtain a finite continuum density of critical points oneshould scale g ∝ N−3/2, i.e. g = gsε

3 as observed in [ALWZ ’07].

I This is the only scaling leading to a continuum limit qualitativelydifferent from DT and CDT.

I Continuum limit g = gc(g)(1− Λε2),z1 = z1,c(1− Z1ε), g = gsε

3:

Z 31 −

(Λ + 3

(gs2

)2/3)Z1 − gs = 0

I Can compute:

Page 58: Generalized CDT as a scaling limit of planar maps

I The number of local maxima Nmax(g) scales with N at the criticalpoint,

〈Nmax(g)〉NN

= 2(g

2

)2/3

+O(g),〈Nmax(g = 1)〉N

N= 1/2

I Therefore, to obtain a finite continuum density of critical points oneshould scale g ∝ N−3/2, i.e. g = gsε

3 as observed in [ALWZ ’07].

I This is the only scaling leading to a continuum limit qualitativelydifferent from DT and CDT.

I Continuum limit g = gc(g)(1− Λε2),z1 = z1,c(1− Z1ε), g = gsε

3:

Z 31 −

(Λ + 3

(gs2

)2/3)Z1 − gs = 0

I Can compute:

Page 59: Generalized CDT as a scaling limit of planar maps

I The number of local maxima Nmax(g) scales with N at the criticalpoint,

〈Nmax(g)〉NN

= 2(g

2

)2/3

+O(g),〈Nmax(g = 1)〉N

N= 1/2

I Therefore, to obtain a finite continuum density of critical points oneshould scale g ∝ N−3/2, i.e. g = gsε

3 as observed in [ALWZ ’07].

I This is the only scaling leading to a continuum limit qualitativelydifferent from DT and CDT.

I Continuum limit g = gc(g)(1− Λε2),z1 = z1,c(1− Z1ε), g = gsε

3:

Z 31 −

(Λ + 3

(gs2

)2/3)Z1 − gs = 0

I Can compute:

Page 60: Generalized CDT as a scaling limit of planar maps

Two-point function

I Amplitude for having root atdistance T from origin.

I Given by T -derivative of Z0(T )and Z1(T ), which are thescaling limits of the generatingfunctions z0(t) and z1(t) oflabeled trees with label t on theroot.

I They satisfy

z1(t) =1

1− gz1(t − 1)− gz0(t)− gz0(t + 1)

z0(t) = z1(t) +g− 1

1− gz1(t − 1)− gz0(t)

Page 61: Generalized CDT as a scaling limit of planar maps

Two-point function

I Amplitude for having root atdistance T from origin.

I Given by T -derivative of Z0(T )and Z1(T ), which are thescaling limits of the generatingfunctions z0(t) and z1(t) oflabeled trees with label t on theroot.

I They satisfy

z1(t) =1

1− gz1(t − 1)− gz0(t)− gz0(t + 1)

z0(t) = z1(t) +g− 1

1− gz1(t − 1)− gz0(t)

Page 62: Generalized CDT as a scaling limit of planar maps

Two-point function

I Amplitude for having root atdistance T from origin.

I Given by T -derivative of Z0(T )and Z1(T ), which are thescaling limits of the generatingfunctions z0(t) and z1(t) oflabeled trees with label t on theroot.

I They satisfy

z1(t) =1

1− gz1(t − 1)− gz0(t)− gz0(t + 1)

z0(t) = z1(t) +g− 1

1− gz1(t − 1)− gz0(t)

Page 63: Generalized CDT as a scaling limit of planar maps

I Solution is (using methods of [Bouttier, Di Francesco, Guitter, ’03]):

z1(t) = z11− σt

1− σt+1

1− (1− β)σ − βσt+3

1− (1− β)σ − βσt+2,

z0(t) = z01− σt

1− (1− β)σ − βσt+1

(1− (1− β)σ)2 − β2σt+3

1− (1− β)σ − βσt+2,

with β = β(g , g) and σ = σ(g , g) fixed by

g(1 + σ)(1 + βσ)z1 − σ(1− 2g z0) = 0,

(1− β)σ − g(1 + σ)z1 + g(1− σ + 2βσ)z0 = 0.

I Continuum limit, g = gsε3, g = gc(1− Λε2), t = T/ε, gives

dZ0(T )

dT= Σ3 gs

α

Σ sinh ΣT + α cosh ΣT(Σ cosh ΣT + α sinh ΣT

)3

gs→∞−→ Λ3/4 cosh(Λ1/4T ′)

sinh3(Λ1/4T ′)T ′ = g1/6

s T

I DT two-point function appears as gs →∞! [Ambjørn, Watabiki, ’95]

Page 64: Generalized CDT as a scaling limit of planar maps

I Solution is (using methods of [Bouttier, Di Francesco, Guitter, ’03]):

z1(t) = z11− σt

1− σt+1

1− (1− β)σ − βσt+3

1− (1− β)σ − βσt+2,

z0(t) = z01− σt

1− (1− β)σ − βσt+1

(1− (1− β)σ)2 − β2σt+3

1− (1− β)σ − βσt+2,

with β = β(g , g) and σ = σ(g , g) fixed by

g(1 + σ)(1 + βσ)z1 − σ(1− 2g z0) = 0,

(1− β)σ − g(1 + σ)z1 + g(1− σ + 2βσ)z0 = 0.

I Continuum limit, g = gsε3, g = gc(1− Λε2), t = T/ε, gives

dZ0(T )

dT= Σ3 gs

α

Σ sinh ΣT + α cosh ΣT(Σ cosh ΣT + α sinh ΣT

)3

gs→∞−→ Λ3/4 cosh(Λ1/4T ′)

sinh3(Λ1/4T ′)T ′ = g1/6

s T

I DT two-point function appears as gs →∞! [Ambjørn, Watabiki, ’95]

Page 65: Generalized CDT as a scaling limit of planar maps

I Solution is (using methods of [Bouttier, Di Francesco, Guitter, ’03]):

z1(t) = z11− σt

1− σt+1

1− (1− β)σ − βσt+3

1− (1− β)σ − βσt+2,

z0(t) = z01− σt

1− (1− β)σ − βσt+1

(1− (1− β)σ)2 − β2σt+3

1− (1− β)σ − βσt+2,

with β = β(g , g) and σ = σ(g , g) fixed by

g(1 + σ)(1 + βσ)z1 − σ(1− 2g z0) = 0,

(1− β)σ − g(1 + σ)z1 + g(1− σ + 2βσ)z0 = 0.

I Continuum limit, g = gsε3, g = gc(1− Λε2), t = T/ε, gives

dZ0(T )

dT= Σ3 gs

α

Σ sinh ΣT + α cosh ΣT(Σ cosh ΣT + α sinh ΣT

)3

gs→∞−→ Λ3/4 cosh(Λ1/4T ′)

sinh3(Λ1/4T ′)T ′ = g1/6

s T

I DT two-point function appears as gs →∞! [Ambjørn, Watabiki, ’95]

Page 66: Generalized CDT as a scaling limit of planar maps

Planar maps

2

1

1

1

3

3

3

4

4

0

2

2

2

2

2

1

3

1

3

3

2

t t

t +1

t - 1

t t

t +1

t +1

I Bijection between quadrangulations with Nmax local maxima andplanar maps with Nmax faces!

Page 67: Generalized CDT as a scaling limit of planar maps

Planar maps

2

1

1

1

3

3

3

4

4

2

2

2

2

2

1

3

1

3

3

2

t t

t +1

t - 1

t t

t +1

t +1

I Bijection between quadrangulations with Nmax local maxima andplanar maps with Nmax faces!

Page 68: Generalized CDT as a scaling limit of planar maps

Planar maps

2

1

1

1

3

3

3

4

4

2

2

2

2

2

1

3

1

3

3

2

t t

t +1

t - 1

t t

t +1

t +1

2

1

1

1

3 3

3

4

4

0

2

2

2

2

2

1

3

1

332

t t

t +1

t - 1

t t

t +1

t +1

I Bijection between quadrangulations with Nmax local maxima andplanar maps with Nmax faces!

Page 69: Generalized CDT as a scaling limit of planar maps

Planar maps

2

1

1

1

3

3

3

4

4

2

2

2

2

2

1

3

1

3

3

2

t t

t +1

t - 1

t t

t +1

t +1

2

1

1

1

3 3

3

4

4

0

2

2

2

2

2

1

3

1

332

t t

t +1

t - 1

t t

t +1

t +1

I Bijection between quadrangulations with Nmax local maxima andplanar maps with Nmax faces!

Page 70: Generalized CDT as a scaling limit of planar maps

Planar maps

2

1

1

1

3

3

3

4

4

2

2

2

2

2

1

3

1

3

3

2

t t

t +1

t - 1

t t

t +1

t +1

t t

t +1

t - 1

t t

t +1

t +1

I Bijection between quadrangulations with Nmax local maxima andplanar maps with Nmax faces!

Page 71: Generalized CDT as a scaling limit of planar maps

Planar maps

t t

t +1

t - 1

t t

t +1

t +1

I Bijection between quadrangulations with Nmax local maxima andplanar maps with Nmax faces!

Page 72: Generalized CDT as a scaling limit of planar maps

Two-point function for planar maps

2

1

1

1

3 3

3

4

4

2

2

2

2

2

1

3

1

3

32

I We know generating functions for trees and therefore obtain anexplicit generating function

z0(t + 1)− z0(t) =∞∑

N=0

∞∑n=0

Nt(N, n)gNgn

for the number Nt(N, n) of planar maps with N edges, n faces, anda marked point at distance t from the root.

Page 73: Generalized CDT as a scaling limit of planar maps

Two loop identity in generalized CDT

I Consider surfaces with two boundaries separatedby a geodesic distance D.

I One can assign time T1, T2 to the boundaries(|T1 − T2| ≤ D) and study a “merging” process.

I For a given surface the foliation depends onT1 − T2, hence also Nmax and its weight.

I However, in [ALWZ ’07] it was shown that theamplitude is independent of T1 − T2.

I Refoliation symmetry at the quantum level in thepresence of topology change!

I Can we better understand this symmetry at thediscrete level?

I For simplicity set the boundarylengths to zero.Straightforward generalization to finite boundaries.

Page 74: Generalized CDT as a scaling limit of planar maps

Two loop identity in generalized CDT

I Consider surfaces with two boundaries separatedby a geodesic distance D.

I One can assign time T1, T2 to the boundaries(|T1 − T2| ≤ D) and study a “merging” process.

I For a given surface the foliation depends onT1 − T2, hence also Nmax and its weight.

I However, in [ALWZ ’07] it was shown that theamplitude is independent of T1 − T2.

I Refoliation symmetry at the quantum level in thepresence of topology change!

I Can we better understand this symmetry at thediscrete level?

I For simplicity set the boundarylengths to zero.Straightforward generalization to finite boundaries.

Page 75: Generalized CDT as a scaling limit of planar maps

Two loop identity in generalized CDT

I Consider surfaces with two boundaries separatedby a geodesic distance D.

I One can assign time T1, T2 to the boundaries(|T1 − T2| ≤ D) and study a “merging” process.

I For a given surface the foliation depends onT1 − T2, hence also Nmax and its weight.

I However, in [ALWZ ’07] it was shown that theamplitude is independent of T1 − T2.

I Refoliation symmetry at the quantum level in thepresence of topology change!

I Can we better understand this symmetry at thediscrete level?

I For simplicity set the boundarylengths to zero.Straightforward generalization to finite boundaries.

Page 76: Generalized CDT as a scaling limit of planar maps

Two loop identity in generalized CDT

I Consider surfaces with two boundaries separatedby a geodesic distance D.

I One can assign time T1, T2 to the boundaries(|T1 − T2| ≤ D) and study a “merging” process.

I For a given surface the foliation depends onT1 − T2, hence also Nmax and its weight.

I However, in [ALWZ ’07] it was shown that theamplitude is independent of T1 − T2.

I Refoliation symmetry at the quantum level in thepresence of topology change!

I Can we better understand this symmetry at thediscrete level?

I For simplicity set the boundarylengths to zero.Straightforward generalization to finite boundaries.

Page 77: Generalized CDT as a scaling limit of planar maps

Two loop identity in generalized CDT

I Consider surfaces with two boundaries separatedby a geodesic distance D.

I One can assign time T1, T2 to the boundaries(|T1 − T2| ≤ D) and study a “merging” process.

I For a given surface the foliation depends onT1 − T2, hence also Nmax and its weight.

I However, in [ALWZ ’07] it was shown that theamplitude is independent of T1 − T2.

I Refoliation symmetry at the quantum level in thepresence of topology change!

I Can we better understand this symmetry at thediscrete level?

I For simplicity set the boundarylengths to zero.Straightforward generalization to finite boundaries.

Page 78: Generalized CDT as a scaling limit of planar maps

Two loop identity in generalized CDT

I Consider surfaces with two boundaries separatedby a geodesic distance D.

I One can assign time T1, T2 to the boundaries(|T1 − T2| ≤ D) and study a “merging” process.

I For a given surface the foliation depends onT1 − T2, hence also Nmax and its weight.

I However, in [ALWZ ’07] it was shown that theamplitude is independent of T1 − T2.

I Refoliation symmetry at the quantum level in thepresence of topology change!

I Can we better understand this symmetry at thediscrete level?

I For simplicity set the boundarylengths to zero.Straightforward generalization to finite boundaries.

Page 79: Generalized CDT as a scaling limit of planar maps

Two loop identity in generalized CDT

I Consider surfaces with two boundaries separatedby a geodesic distance D.

I One can assign time T1, T2 to the boundaries(|T1 − T2| ≤ D) and study a “merging” process.

I For a given surface the foliation depends onT1 − T2, hence also Nmax and its weight.

I However, in [ALWZ ’07] it was shown that theamplitude is independent of T1 − T2.

I Refoliation symmetry at the quantum level in thepresence of topology change!

I Can we better understand this symmetry at thediscrete level?

I For simplicity set the boundarylengths to zero.Straightforward generalization to finite boundaries.

Page 80: Generalized CDT as a scaling limit of planar maps

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 0D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 81: Generalized CDT as a scaling limit of planar maps

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 0D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 82: Generalized CDT as a scaling limit of planar maps

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 0D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 83: Generalized CDT as a scaling limit of planar maps

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 0D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 84: Generalized CDT as a scaling limit of planar maps

8

7

7

7

7

7

6

8

68

6

6

6

6

8

5

5

7

55

7

5

7

7

5

7

5

5

75

7

5

7

6

6

6

4

6

4

44

46

4

4

4

6

4 4

6

4

6

6

6

3

5

3

55

5

5

5

3

3

5

3

5

5

5

3

3

5

3

5

3

3

4

2

2

2

44

22

4

2

4

2

44

44 4

4

2

1

1

33

5

5

3

3

3

1

3

3

3

3

5

53

3

3

4

0

2

24

2

2

2

4

4

4

2

2

2

2

3

3

3

1

3

1

1

3

1

3

3

0

2

2

2

2

2

2

1

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 0D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 85: Generalized CDT as a scaling limit of planar maps

0

0

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 0D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 86: Generalized CDT as a scaling limit of planar maps

0

2

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 2D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 87: Generalized CDT as a scaling limit of planar maps

8

7

7

7

7

7

6

9

69

6

6

6

6

8

5

5

7

55

8

5

8

9

5

7

5

5

75

8

5

9

7

8

8

4

6

4

44

48

4

4

4

8

4 4

7

4

8

8

8

3

7

3

77

7

7

7

3

3

7

3

5

6

7

3

3

7

3

7

3

3

6

2

2

2

66

22

4

2

6

2

66

66 6

6

2

1

1

55

7

5

5

3

4

1

5

5

5

4

6

75

5

3

4

0

2

46

4

2

3

5

6

6

4

2

4

2

5

5

3

3

3

3

3

5

1

5

4

2

4

4

2

4

4

4

3

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 2D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 88: Generalized CDT as a scaling limit of planar maps

8

7

7

7

7

7

6

9

69

6

6

6

6

8

5

5

7

55

8

5

8

9

5

7

5

5

75

8

5

9

7

8

8

4

6

4

44

48

4

4

4

8

4 4

7

4

8

8

8

3

7

3

77

7

7

7

3

3

7

3

5

6

7

3

3

7

3

7

3

3

6

2

2

2

66

22

4

2

6

2

66

66 6

6

2

1

1

55

7

5

5

3

4

1

5

5

5

4

6

75

5

3

4

0

2

46

4

2

3

5

6

6

4

2

4

2

5

5

3

3

3

3

3

5

1

5

4

2

4

4

2

4

4

4

3

t t

t + 1

t - 1

t t

t + 1

t + 1

T1 = 0T2 = 2D = 4

I Only need to keep the labels of the marked points!

I There exists a bijection preserving the number of local maxima:{ }T1,T2

←→

{0

0

}T1,T2

←→

{0

2

}T ′

1 ,T′2

←→

{ }T ′

1 ,T′2

Page 89: Generalized CDT as a scaling limit of planar maps

Conclusions & Outlook

I ConlusionsI The Cori–Vauquelin–Schaeffer bijection is ideal for studying

“proper-time foliations” of random surfaces.I Generalized CDT appears naturally as the scaling limit of random

planar maps with a fixed finite number of faces.I Continuum DT (Brownian map?) seems to be recovered by taking

gs → ∞.I The relation to planar maps explains the mysterious loop-loop

identities in the continuum.

I OutlookI Is there a convergence towards a random measure on metric spaces,

i.e. analogue of the Brownian map? Should first try to understand2d geometry of random causal triangulations.

I What is the structure of the symmetries mentioned above?I Various stochastic processes involved in generalized CDT. How are

they related?

Further reading: arXiv:1302.1763

These slides and more: http://www.nbi.dk/~budd/

Questions?

Page 90: Generalized CDT as a scaling limit of planar maps

Conclusions & Outlook

I ConlusionsI The Cori–Vauquelin–Schaeffer bijection is ideal for studying

“proper-time foliations” of random surfaces.I Generalized CDT appears naturally as the scaling limit of random

planar maps with a fixed finite number of faces.I Continuum DT (Brownian map?) seems to be recovered by taking

gs → ∞.I The relation to planar maps explains the mysterious loop-loop

identities in the continuum.

I OutlookI Is there a convergence towards a random measure on metric spaces,

i.e. analogue of the Brownian map? Should first try to understand2d geometry of random causal triangulations.

I What is the structure of the symmetries mentioned above?I Various stochastic processes involved in generalized CDT. How are

they related?

Further reading: arXiv:1302.1763

These slides and more: http://www.nbi.dk/~budd/

Questions?

Page 91: Generalized CDT as a scaling limit of planar maps

Conclusions & Outlook

I ConlusionsI The Cori–Vauquelin–Schaeffer bijection is ideal for studying

“proper-time foliations” of random surfaces.I Generalized CDT appears naturally as the scaling limit of random

planar maps with a fixed finite number of faces.I Continuum DT (Brownian map?) seems to be recovered by taking

gs → ∞.I The relation to planar maps explains the mysterious loop-loop

identities in the continuum.

I OutlookI Is there a convergence towards a random measure on metric spaces,

i.e. analogue of the Brownian map? Should first try to understand2d geometry of random causal triangulations.

I What is the structure of the symmetries mentioned above?I Various stochastic processes involved in generalized CDT. How are

they related?

Further reading: arXiv:1302.1763

These slides and more: http://www.nbi.dk/~budd/

Questions?

Page 92: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

0

2

Page 93: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

1

11

0

1

2

Page 94: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

2

2

2

22

2

2

2

1

11

0

2

2

2

21

2

2

Page 95: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

3

3

3

3

3

3

3

3

3

3

2

2

2

22

2

2

2

1

1

3

1

3

0

2

2

3

2

23

3

3

3

3

1

2

2

3

Page 96: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

4

4

44

4

4

4

4

4 4

4

3

3

3

3

3

3

3

3

3

3

2

2

2

22

4

2

2

2

1

1

3

4

1

43

4

0

2

4

4

2

3

4

2

4

23

3

3

3

3

1 4

2

4

4

2

4

4

4

3

Page 97: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

5

5

55

5

5

5

5

5

5

4

4

44

4

4

4

4

4 4

4

3

3

3

3

3

5

3

3

3

3

3

2

2

2

22

4

2

2

2

1

1

55

5

5

3

4

1

5

5

5

4

5

5

3

4

0

2

4

4

2

3

5

4

2

4

2

5

5

3

3

3

3

3

5

1

5

4

2

4

4

2

4

4

4

3

Page 98: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

6

6

6

6

6

6

5

5

55

5

5

5

5

5

5

4

6

4

44

4

4

4

4

4 4

4

3

3

3

3

3

5

6

3

3

3

3

3

6

2

2

2

66

22

4

2

6

2

66

66 6

6

2

1

1

55

5

5

3

4

1

5

5

5

4

65

5

3

4

0

2

46

4

2

3

5

6

6

4

2

4

2

5

5

3

3

3

3

3

5

1

5

4

2

4

4

2

4

4

4

3

Page 99: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

7

7

7

7

7

6

6

6

6

6

6

5

5

7

55

5

5

7

5

5

75

5

7

4

6

4

44

4

4

4

4

4 4

7

4

3

7

3

77

7

7

7

3

3

7

3

5

6

7

3

3

7

3

7

3

3

6

2

2

2

66

22

4

2

6

2

66

66 6

6

2

1

1

55

7

5

5

3

4

1

5

5

5

4

6

75

5

3

4

0

2

46

4

2

3

5

6

6

4

2

4

2

5

5

3

3

3

3

3

5

1

5

4

2

4

4

2

4

4

4

3

Page 100: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

8

7

7

7

7

7

6

6

6

6

6

6

8

5

5

7

55

8

5

8

5

7

5

5

75

8

5

7

8

8

4

6

4

44

48

4

4

4

8

4 4

7

4

8

8

8

3

7

3

77

7

7

7

3

3

7

3

5

6

7

3

3

7

3

7

3

3

6

2

2

2

66

22

4

2

6

2

66

66 6

6

2

1

1

55

7

5

5

3

4

1

5

5

5

4

6

75

5

3

4

0

2

46

4

2

3

5

6

6

4

2

4

2

5

5

3

3

3

3

3

5

1

5

4

2

4

4

2

4

4

4

3

Page 101: Generalized CDT as a scaling limit of planar maps

Appendix: canonical labeling

8

7

7

7

7

7

6

9

69

6

6

6

6

8

5

5

7

55

8

5

8

9

5

7

5

5

75

8

5

9

7

8

8

4

6

4

44

48

4

4

4

8

4 4

7

4

8

8

8

3

7

3

77

7

7

7

3

3

7

3

5

6

7

3

3

7

3

7

3

3

6

2

2

2

66

22

4

2

6

2

66

66 6

6

2

1

1

55

7

5

5

3

4

1

5

5

5

4

6

75

5

3

4

0

2

46

4

2

3

5

6

6

4

2

4

2

5

5

3

3

3

3

3

5

1

5

4

2

4

4

2

4

4

4

3

Page 102: Generalized CDT as a scaling limit of planar maps

Including boundaries [Bouttier, Guitter ’09, Bettinelli ’11, Curien, Miermont ’12]

I A quadrangulations withboundary length 2l

and anorigin.

I Applying the same prescriptionwe obtain a forest rooted at theboundary.

I The labels on the boundaryarise from a (closed) randomwalk.

I A (possibly empty) tree growsat the end of every +-edge.

I There is a bijection [Bettinelli]

56

76

56

54

34

54

32

34

34

56

78

98

98

76

{Quadrangulations with originand boundary length 2l

}↔ {(+,−)-sequences} × {tree}l

Page 103: Generalized CDT as a scaling limit of planar maps

Including boundaries [Bouttier, Guitter ’09, Bettinelli ’11, Curien, Miermont ’12]

I A quadrangulations withboundary length 2l and anorigin.

I Applying the same prescriptionwe obtain a forest rooted at theboundary.

I The labels on the boundaryarise from a (closed) randomwalk.

I A (possibly empty) tree growsat the end of every +-edge.

I There is a bijection [Bettinelli]

56

76

56

54

34

54

32

34

34

56

78

98

98

76

{Quadrangulations with originand boundary length 2l

}↔ {(+,−)-sequences} × {tree}l

Page 104: Generalized CDT as a scaling limit of planar maps

Including boundaries [Bouttier, Guitter ’09, Bettinelli ’11, Curien, Miermont ’12]

I A quadrangulations withboundary length 2l and anorigin.

I Applying the same prescriptionwe obtain a forest rooted at theboundary.

I The labels on the boundaryarise from a (closed) randomwalk.

I A (possibly empty) tree growsat the end of every +-edge.

I There is a bijection [Bettinelli]

5

6

7

6

5

65 4

34

5

4

3

23

4

3

4

5

6

78

9

898

76

56

76

56

54

34

54

32

34

34

56

78

98

98

76

{Quadrangulations with originand boundary length 2l

}↔ {(+,−)-sequences} × {tree}l

Page 105: Generalized CDT as a scaling limit of planar maps

Including boundaries [Bouttier, Guitter ’09, Bettinelli ’11, Curien, Miermont ’12]

I A quadrangulations withboundary length 2l and anorigin.

I Applying the same prescriptionwe obtain a forest rooted at theboundary.

I The labels on the boundaryarise from a (closed) randomwalk.

I A (possibly empty) tree growsat the end of every +-edge.

I There is a bijection [Bettinelli]

5

6

7

6

5

65 4

34

5

4

3

23

4

3

4

5

6

78

9

898

76

56

76

56

54

34

54

32

34

34

56

78

98

98

76

{Quadrangulations with originand boundary length 2l

}↔ {(+,−)-sequences} × {tree}l

Page 106: Generalized CDT as a scaling limit of planar maps

Including boundaries [Bouttier, Guitter ’09, Bettinelli ’11, Curien, Miermont ’12]

I A quadrangulations withboundary length 2l and anorigin.

I Applying the same prescriptionwe obtain a forest rooted at theboundary.

I The labels on the boundaryarise from a (closed) randomwalk.

I A (possibly empty) tree growsat the end of every +-edge.

I There is a bijection [Bettinelli]

5

6

7

6

5

65 4

34

5

4

3

23

4

3

4

5

6

78

9

898

76

-

-+

+-+

+

+-

-+

+

+-

-+-

-

-

-

-

-+-+

+

+

+

{Quadrangulations with originand boundary length 2l

}↔ {(+,−)-sequences} × {tree}l

Page 107: Generalized CDT as a scaling limit of planar maps

Including boundaries [Bouttier, Guitter ’09, Bettinelli ’11, Curien, Miermont ’12]

I A quadrangulations withboundary length 2l and anorigin.

I Applying the same prescriptionwe obtain a forest rooted at theboundary.

I The labels on the boundaryarise from a (closed) randomwalk.

I A (possibly empty) tree growsat the end of every +-edge.

I There is a bijection [Bettinelli]

5

6

7

6

5

65 4

34

5

4

3

23

4

3

4

5

6

78

9

898

76

-

-+

+-+

+

+-

-+

+

+-

-+-

-

-

-

-

-+-+

+

+

+

{Quadrangulations with originand boundary length 2l

}↔ {(+,−)-sequences} × {tree}l

Page 108: Generalized CDT as a scaling limit of planar maps

Disk amplitudes

w(g , l) = z(g)l

w(g , x) =∞∑l=0

w(g , l)x l =1

1− z(g)x

w(g , l) =

(2ll

)z(g)l

w(g , x) =1√

1− 4z(g)x

Generating functionfor unlabeled trees:

z(g) =1−√

1− 4g

2g

0+

+000

- 0-+

+0 --0

- 00+

--

Generating functionfor labeled trees:

z(g) =1−√

1− 12g

6g

Page 109: Generalized CDT as a scaling limit of planar maps

Disk amplitudes

w(g , l) = z(g)l

w(g , x) =∞∑l=0

w(g , l)x l =1

1− z(g)x

w(g , l) =

(2ll

)z(g)l

w(g , x) =1√

1− 4z(g)x

Generating functionfor unlabeled trees:

z(g) =1−√

1− 4g

2g

0+

+000

- 0-+

+0 --0

- 00+

--

Generating functionfor labeled trees:

z(g) =1−√

1− 12g

6g

Page 110: Generalized CDT as a scaling limit of planar maps

Disk amplitudes

w(g , l) = z(g)l

w(g , x) =∞∑l=0

w(g , l)x l =1

1− z(g)x

w(g , l) =

(2ll

)z(g)l

w(g , x) =1√

1− 4z(g)x

Generating functionfor unlabeled trees:

z(g) =1−√

1− 4g

2g

0+

+000

- 0-+

+0 --0

- 00+

--

Generating functionfor labeled trees:

z(g) =1−√

1− 12g

6g

Page 111: Generalized CDT as a scaling limit of planar maps

Disk amplitudes

w(g , l) = z(g)l

w(g , x) =∞∑l=0

w(g , l)x l =1

1− z(g)x

w(g , l) =

(2ll

)z(g)l

w(g , x) =1√

1− 4z(g)x

Generating functionfor unlabeled trees:

z(g) =1−√

1− 4g

2g

0+

+000

- 0-+

+0 --0

- 00+

--

Generating functionfor labeled trees:

z(g) =1−√

1− 12g

6g

Page 112: Generalized CDT as a scaling limit of planar maps

Continuum limit

w(g , x) =1

1− zx

WΛ(X ) =1

X + Z

w(g , x) =1√

1− 4zx

W ′Λ(X ) =1√

X + Z

z(g) = 1−√

1−4g2g

Z =√

Λ

0+

+000

- 0-+

+0 --0

- 00+

--

z(g) = 1−√

1−12g6g

Z =√

Λ

I Expanding around critical point in terms of “lattice spacing” ε:

g = gc(1− Λε2), z(g) = zc(1− Zε), x = xc(1− X ε)

I CDT disk amplitude: WΛ(X ) = 1X+√

Λ

I DT disk amplitude with marked point: W ′Λ(X ) = 1√X+√

Λ. Integrate

w.r.t. Λ to remove mark: WΛ(X ) = 23 (X − 1

2

√Λ)√

X +√

Λ.

Page 113: Generalized CDT as a scaling limit of planar maps

Continuum limit

w(g , x) =1

1− zx

WΛ(X ) =1

X + Z

w(g , x) =1√

1− 4zx

W ′Λ(X ) =1√

X + Z

z(g) = 1−√

1−4g2g

Z =√

Λ

0+

+000

- 0-+

+0 --0

- 00+

--

z(g) = 1−√

1−12g6g

Z =√

Λ

I Expanding around critical point in terms of “lattice spacing” ε:

g = gc(1− Λε2), z(g) = zc(1− Zε), x = xc(1− X ε)

I CDT disk amplitude: WΛ(X ) = 1X+√

Λ

I DT disk amplitude with marked point: W ′Λ(X ) = 1√X+√

Λ. Integrate

w.r.t. Λ to remove mark: WΛ(X ) = 23 (X − 1

2

√Λ)√

X +√

Λ.

Page 114: Generalized CDT as a scaling limit of planar maps

Continuum limit

w(g , x) =1

1− zx

WΛ(X ) =1

X + Z

w(g , x) =1√

1− 4zx

W ′Λ(X ) =1√

X + Z

z(g) = 1−√

1−4g2g

Z =√

Λ

0+

+000

- 0-+

+0 --0

- 00+

--

z(g) = 1−√

1−12g6g

Z =√

Λ

I Expanding around critical point in terms of “lattice spacing” ε:

g = gc(1− Λε2), z(g) = zc(1− Zε), x = xc(1− X ε)

I CDT disk amplitude: WΛ(X ) = 1X+√

Λ

I DT disk amplitude with marked point: W ′Λ(X ) = 1√X+√

Λ. Integrate

w.r.t. Λ to remove mark: WΛ(X ) = 23 (X − 1

2

√Λ)√

X +√

Λ.

Page 115: Generalized CDT as a scaling limit of planar maps

Continuum limit

w(g , x) =1

1− zx

WΛ(X ) =1

X + Z

w(g , x) =1√

1− 4zx

W ′Λ(X ) =1√

X + Z

z(g) = 1−√

1−4g2g

Z =√

Λ

0+

+000

- 0-+

+0 --0

- 00+

--

z(g) = 1−√

1−12g6g

Z =√

Λ

I Expanding around critical point in terms of “lattice spacing” ε:

g = gc(1− Λε2), z(g) = zc(1− Zε), x = xc(1− X ε)

I CDT disk amplitude: WΛ(X ) = 1X+√

Λ

I DT disk amplitude with marked point: W ′Λ(X ) = 1√X+√

Λ. Integrate

w.r.t. Λ to remove mark: WΛ(X ) = 23 (X − 1

2

√Λ)√

X +√

Λ.

Page 116: Generalized CDT as a scaling limit of planar maps

Continuum limit

w(g , x) =1

1− zx

WΛ(X ) =1

X + Z

w(g , x) =1√

1− 4zx

W ′Λ(X ) =1√

X + Z

z(g) = 1−√

1−4g2g

Z =√

Λ

0+

+000

- 0-+

+0 --0

- 00+

--

z(g) = 1−√

1−12g6g

Z =√

Λ

I Expanding around critical point in terms of “lattice spacing” ε:

g = gc(1− Λε2), z(g) = zc(1− Zε), x = xc(1− X ε)

I CDT disk amplitude: WΛ(X ) = 1X+√

Λ

I DT disk amplitude with marked point: W ′Λ(X ) = 1√X+√

Λ. Integrate

w.r.t. Λ to remove mark: WΛ(X ) = 23 (X − 1

2

√Λ)√X +

√Λ.