Existence and regularity for solutions to Hyperbolic
Monge-Ampere equations with applications to
Non-Euclidean elasticity.
CMU CNA Seminar September 11, 2018
Shankar Venkataramani
Toby Shearman
Ken Yamamoto
John Gemmer
My Ph.D students
John Gemmer
Toby Shearman
φ
h
′2
+
r
′2
= 1
N
= (
h
′
,
−r
′
)
= (sin(
θ
)
,
cos(
θ
))
dω
= sin(
θ
)
dθ
∧
dφ
=
−
d
cos(
θ
)
∧
dφ
=
r
′′
ds
∧
dφ
dA
=
d
φ
∧
ds
⇒
r
′′
=
−
k
(
s
)
r
In addition, we require that
1
r
0
1.
If
k(s)
c >
0, then we cannot have solutions on the entire real line. At
some finite
s
we have
r
0=
±
1.
Nonexistence results for isometric immersions of
the Hyperbolic plane
•
Hilbert
(1901): There is no real analytic isometric immersion of
H
2onto a
complete subset of
R
3•
Holmgren
(1902): Given a (local) smooth embedding of
H
2in
R
3, the
embedding cannot be extended isometrically and smoothly beyond is a
finite distance
d
.
•
Amsler
(1955): Every su
ffi
ciently smooth immersion of the hyperbolic plane
into
R
3has a singular “edge”,
i.e
, a one-dimensional submanifold beyond
which the embedding cannot be smoothly extended.
•
Efimov
(1962): No
C
2isometric embedding of
H
2, or any complete
mani-fold with curvature that is uniformly negative in
R
3.
Overview
•
Quick review of differential geometry
•
C
1,1
isometric immersions, branch points.
•
Construction of branched surfaces -
Discrete differential
geometry
.
•
Continuum mechanics for discrete surfaces.
•
Applications to geometry, dynamics.
x
y
u
v
w
Φ
Elastic energy of a thin sheet
E
=
!
∥
γ
∥
2
+
ϵ
2
∥
κ
∥
2
κ
= ˆ
n
·
D
2
Φ
γ
= (
D
Φ)
T
·
D
Φ
−
g
Elastic energy
E
t
[ ] =
S
[ ] +
t
2
B
[
H, K
]
=
Z
⌦
Q
( )
dxdy
+
t
2
Z
⌦
(4
H
2
2
K
)
dxdy,
Lewicka and Pakzad (2011).
–limit:
lim
t
!
0
t
2
E
t
=
(R
⌦
(4
H
2
2
K
)
dxdy
2
W
2
,
2
iso
+
1
otherwise
x
y
u
v
w
ΦImmersion
:
⌦
!
R
3
of the center surface.
Reference Riemannian metric
g
.
N
(
p
)
·
d
r
(
p
) = 0
I
≡
ds
2
=
d
r
(
p
)
·
d
r
(
p
)
Geometry: The Gauss Normal map
p
Hyperbolic Monge Ampere equations
n
= (
w
x
, w
y
,
1)
N
=
k
n
n
k
.
dA
= (
w
xx
w
yy
w
xy
2
)
dx
^
dy
.
d
=
k
dA
n
k
4dp
^
dq
=
K
F vK
(
x, y
)
dx
^
dy
.
dp
^
dq
=
K
k
(
n
x,y
k
4)
dx
^
dy
For any domain on which the normal map is one-to-one, the area of the
spherical image cannot exceed 2⇡
. No such restriction for the planar image.
Hyperbolic Monge-Ampere equations
Au
xx
+ 2
Bu
xy
+
Cu
yy
+
D
(
u
xx
u
yy
u
2
xy
) +
E
= 0
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Elliptic:
AC
B
2
DE >
0
Hyperbolic:
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B
2
DE <
0
M
=
R
5with coordinates (
p, q, u, x, y
). A Monge-Ampere equation is an
EDS generate by the contact form
✓
=
du
pdx
qdy
and a 2-form
=
Adp
^
dy
+
B
(
dq
^
dy
dp
^
dx
)
Cdq
^
dx
+
Ddp
^
dq
+
Edx
^
dy,
that is linearly independent from
d
✓
mod
✓
.
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Hyperbolic surfaces: A quadratic saddle
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
).
Piecewise quadratic surfaces
w
(
x, y
) =
(
xy
y
2
cot(
✓
+
))
0
✓
✓
+
xy
+
y
2
cot(
✓
))
✓
✓
0
Let us consider solutions of det(
D
2
w
) =
1
w
is
C
1
,
1
.
All the straight lines
through any point
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
Index of a branch point
C
2
isometries are not
dense in
W
2
,
2
isometries!
Consequences for Numerics?
Amsler surfaces
Sine-Gordon equation:
uv
= sin
.
Self-similar reduction:
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u, v
) = (2
p
uv
)
, z
= 2
p
uv.
Painlev´e III:
zz
+
1
z
z
= sin
.
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Hyperbolic disks: Full geometry
By allowing non-smooth embeddings, we can decrease the
curvature, and the energy.
Geodesics and Asymptotic lines: C
2
surfaces
Constructing K = -1 surfaces
N
=
N
(
u
,
v
),
N
⋅
N
= 1
∂
u
N
⊥
N
,
∂
v
N
⊥
N
∂
u
r
=
∂
u
N
×
N
,
∂
v
r
=
− ∂
v
N
×
N
Lelieuvre formulae
∂
u
N
× ∂
v
N
=
− ∂
u
r
× ∂
v
r
=
−
sin(
φ
)
|
∂
u
r
||
∂
v
r
|
N
“Material coordinates” for
ℍ
2
0 ⇡ 4 ⇡ 2 3⇡ 4 ⇡ 5⇡ 4 3⇡ 2 7⇡ 4Poincare disk model:
g
=
4
dz d
z
¯
(1
−
|
z
|
2
)
2
Asymptotic coordinates to Material coordinates (u, v
)
7!
z
(u, v).
∂
uv
z
=
z
¯
∂
u
z
∂
v
z
The art of M.C. Escher
Mapping the Hyperbolic plane
Quad-mesh
Although we have used the notation
for a mapping
r
:
Z
2
!
R
3
, this makes
sense as a map
r
:
G
!
R
3
, where
G
⇢
R
2is a connected planar graph where every vertex has even degree.
Red curve is a Hamburger
Polygon
A distributional Sine-Gordon equation
The angle
'
between the asymptotic directions satisfies:
'
uv
= sin
'
'
jumps across the “lines of inflexion”
!
=
u
du
v
dv
Hilbert’s Theorem
I
Hilbert (1901): In
E
3there is no complete, analytic surface
of constant negative curvature.
I
Efimov (1968): In
E
3there is no complete,
C
2surface with
curvature
K
c <
0
.
I
Nash (1954): In
E
3there exist complete,
C
1surfaces with
K
c <
0
“Theorem” (A Quantitative Hilbert’s Theorem (TS, SV))
For the elastic energy given previously,
i)
inf
C1,1
E
.
exp
R
1/2
ii)
inf
C2
E
&
exp
R
E
=
k
H
2
k
1
↵
=
⇣
⇤⌘
p
+
=
+
↵
+
=
↵
↵
⇣
⇤⌘
p
&
⇤ p!
An upper bound over
C
1
,
1
surfaces:
A recursion formula
:
n+1
=
n✓
1 +
↵
4
4
◆
s
n+1=
s
n2
↵
2cos
n2
with
↵
=
ln
⇤
n
0 2 4 6 8 10 R, normalized radius
100 101 102 W 2 ,
1 -Energy C2-Catenoid
Periodic Amsler ecpR
Branched
0.0 2.5 5.0 7.5 10.0
R
, normalized radius
Dynamic geometries
Hydrogel with
programmed geometry.
Eran Sharon et al,
Hebrew University.
What does all this mean?
•
Free sheets:
the relevant singularities are
branch points
and
lines of inflection
.
The tangent plane is continuous and the
normal is Lipschitz.
•
Unique —
they
do not concentrate elastic energy
in the
vanishing thickness limit. They are not picked out by the
Gamma-limit.
•
Degeneracy:
The construction with branch points is very
flexible. These sheets have lots of isometries with finite
bending energy, so thin free sheets should be very floppy.
Need a statistical mechanical description.
•
Extrinsic flow:
”Uniformization” of immersions of
Thank you for your attention!