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(1)

Geometry and Topology in the "real world".

Math 586/RTG February 19, 2020

(2)

Part 1

(3)

People who did the real work!

John Gemmer

Toby Shearman

Ken Yamamoto

(4)

Nudibranch “Spanish dancer”

Video used with permission from the copyright holders: Wavelength Reef Cruises, Port Douglas, Australia

Ruffled

“hyperbolic”

(5)
(6)

Physics of thin sheets

Bending is “easy”

Stretching is “hard”

(7)
(8)
(9)

Theorema Egregium III

Mapping the Hyperbolic plane

(10)

The prescribed Gauss curvature equation

Theorema Egregium:

I

=

g

)

det(II

)

det(I

)

=

K

[g].

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d

=

KdA

=

Kd(i

N

(dV

)).

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In (Eulerian) coordinates:

w

xx

w

yy

w

xy

2

(1 +

|r

w

|

2

)

2

=

K

.

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K <

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0 gives a Hyperbolic Monge-Ampere equation.

Local models:

u

xx

u

yy

u

2xy

=

±

1. Solutions:

u

=

12

[x y]Q[x y]

T

with

det(Q) =

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±

1.

(11)

Hyperbolic surfaces: A quadratic saddle

These surfaces are “doubly ruled”.

w

=

1

2

(ax

2

+ 2bxy

+

cy

2

) =

(12)

Negatively curved sheets: Disk geometry

Small slopes approximation:

det(

⇥⇥

w) = 1

Solutions:

w

=

1

2

ax

2

y

a

2

.

w

= 0 for

y

=

±

ax

. Pick

a

= cot(

/n

).

Resulting surface is C

1,1

. Piecewise smooth and patched across

“Lines of inflection”.

(13)

Defects : Scales of smoothness.

Fold or corner

Inflection

Flat sheets

Hyperbolic sheets

Crumpling

Undulating

Lipschitz (C0,1) but not di↵erentiable (C1).

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(14)

Origami vs. “hyperbolic origami”

Edges and corners.

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(15)

4

see Fig. 4(e-f). Note that, if a hyperbolic surface is C2, every point is locally a (regular) saddle (as in Fig. 4(a)) and there-fore cannot contain branch points. Non-C2 immersions are therefore qualitatively di↵erent from C2 immersions in that

they admit 3-saddles (“monkey saddles”) and higher order saddles, which can mediate a local refinement of the buckling wavelength (See Fig. 5).

FIG. 4. (a-b) Small slope isometric immersions w0

4(x1, x2) and w04(x1, x2) for constant Gaussian curvature K = 1. w04(x1, x2) is

con-structed by taking odd periodic reflections of the piece of w0

4(x1, x2)

bounded between the green lines. The mesh on both of these sur-faces correspond to their asymptotic lines. (c-d) Projection of the asymptotic lines of w0

4(x1, x2) and w04(x1, x2) onto the x1, x2 plane.

(e-f) Direction of the gradient rw along circles centered at the ori-gin. The regular saddle in (a) corresponds to a gradient field with winding number -1, so the gradient map is 1 to 1. The 4-saddle in (b) has winding number -3, so the gradient map is a 3 sheeted covering near the origin.

Multiple branch points can be introduced on the surface by replicating the above process at any point, not just the origin. For example, consider the surface w02(x1, x2) = x1x2 which is

ruled by the asymptotic lines x1, x2 = const. A branch point

can be added at (x1, x2) = (1/ p2,1/ p2) by removing the

sec-tor x1, x2 1/ p2 and in this region fitting three rotated and

translated copies of w06(x1, x2) = x2(x1 p3x2) so that the

resulting surface has continuous partial derivatives across the cut; see Fig 5(a). Three more branch points b2,1, b2,2, b2,3

at a radial distance of 1/4 from b1,1 can be added along rays

emanating from b1,1 that bisect the lines of inflection; see Fig

5(b). This construction can be continued so that at the n-th it-eration 3n new branch points are added at a radial distance of (1/2)n from the previous branch points. The surface w(x1, x2)

formed in the limit n ! 1 is a fractal with an infinite number of subwrinkles in the region x1 0, x2 0, x21 + x22 1, and

it satisfies [w, w] = 1. The solution can be extended by odd

periodic reflections to give a small-slopes isometric immer-sion of the unit disk with K = 1. To illustrate the wrinkling

behavior near the edge we map w to a strip geometry through a conformal map h[x + iy] = w[ex+iy]; see Figs. 5(c-d).

FIG. 5. Finite bending energy solutions to the Monge-Ampere equa-tion [w0,w0] = 1. (a) Three subwrinkle solution created by

insert-ing three rotated and translated copies of the solution w0

6(x1, x2) = x2(x1 p3x2) onto the solution w0

2(x1, x2) = x1x2 at a branch point.

(b) Nine subwrinkle solution created by inserting nine copies of

w0

12(x1, x2) = x2(x1 (2 + p

3)x2) at three branch points added onto the three subwrinkle solution. (c) Extension of the nine subwrinkle solution to the full circular domain. (d) The nine subwrinkle solution mapped to the strip geometry by a conformal map.

The existence of self-similar isometric immersions has im-plications to the modeling of non-Euclidean elastic sheets. As for the strip with = 1, the solution w02(x1, x2) is

har-monic yet the extension of w02(x1, x2) to an exact

isomet-ric immersion has divergent bending energy for R ' 1.25

with the bending content concentrated near the singular point

x1 = x2 ⇡ 1.25/ p2 [22]. We can isometrically immerse disks

with larger R by a global refinement of the wavelength i.e taking n > 2. These solutions increase the bending energy

globally. An energetically favorable alternative might be to introduce a branch point in the n = 2 solution near the

singu-lar point, and locally refining the wavelength instead. Indeed, numerics for = 1/3 in the strip geometry indicate that, even

within the small slopes approximation, localized self similar wrinkling profiles may be energetically preferred over global refinement of the wavelength [2, 23].

Crumpled sheets have an energy scale t5/3 which is

inter-mediate between the stretching and bending energies [32, 33]. In contrast, the existence of W2,2 isometric immersions for

Topology: Index of a branch point

Consequences for Numerics?

Energy gap?

Branched isometries cannot

be approximated by smooth

(16)

Quad-Graphs: Geometry of Characteristics

Smooth saddle

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Monkey saddle

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(17)
(18)

Growing surfaces

(19)

A spinning “hyperbolic coin”

The formulation of the mechanics requires 3 natural frames!

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(20)

Three frames are better than two

Dynamics is driven by a Goldstone mode

Asymptotic

)

Lagrangian:

(

x

+

iy

) =

e

i⌦t

(

u

+

iv

)

Asymptotic

)

Eulerian:

(X

+

iY, Z

) =

e

i

t

(u

+

iv

),

1

2

(1 +

uv

)

(21)

A “discrete isometric” sea-slug

A

wave-walker

(22)

Part 2

(23)

Collaborators

Gabriela Jaramillo

Guanying Peng

Alan Newell

(24)

Energy driven pattern formation

Heated from below

Cooled from above

courtesy of Michael Schatz, GeorgiaTech

Model equation:

u

t

=

µu

(

+

k

02

)

2

u

u

3

.

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(25)

Patterns in nature

(26)

Phase description and Eikonal equation

|

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r

|

= 1

(27)

θ

Line vs. point defects

Eikonal equation

Swift-Hohenberg numerics

(28)
(29)

Square: Smooth function

θ

1

(

x, y

)

Circle: Smooth function

θ

2

(

x, y

)

Overlap:

!

{

1

,

1

}

k

Z

(30)

Symmetry allows more ”freedom” for directors

Vectors vs. directors

(31)
(32)

The order parameter for layered structures

A half-layer

n+1

k

n+1

=

M

n

n

k

n

.

“Order parameter”

=

(

n

, k

n

)

, where

is an integer,

k

=

±

1.

M

f±

=

1

±

1

0

1

,

M

h

=

M

h 1

=

1

1

0

1

,

M

h

M

f±

M

h 1

=

M

f

.

(33)

Topology, Group theory and defects

M

f

+

and

M

h

generate the infinite dihedral group

D

1

=

Z

o

Z

2

.

If a closed curve

intersects an even number of half-layers, the product

of the matrices

M

n

is a fixed matrix

A

or its inverse

A

1

independent of the

starting point

.

Analogy: Dislocations and disclinations in solids.

E

3

=

R

3

o

O

(3).

(34)

Universal framework

Idea:

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Directions = Eigenvectors.

Convection Patterns

Hyperbolic sheets

M

=

a

b

c

d

,

a

+

d

= 0

, ad

bc

=

1

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M

=

a

b

c

d

,

b

=

c, ad

bc

= 0

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(35)

Thank you for your attention!

What I like about all of this

No boundaries:

Physics/Math, Pure/Applied, “theory”/“numerics”/“experiments”

Work with people:

Students, postdocs, colleagues,...

Always learning something new

Figure

FIG. 5. Finite bending energy solutions to the Monge-Ampere equa-tion [w0, w0] = �1. (a) Three subwrinkle solution created by insert-ing three rotated and translated copies of the solution w06(x1, x2) =p

References

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