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Non-Commutative Geometry and QuantumPhysicsS.N. Bose Institute, Kolkata, Jan 4-11, 2006
Quantization of Contact Manifoldsand Liquid Crystal Flow
S. G. Rajeev
Department of Physics and AstronomyUniversity of Rochester, Rochester, NY14627email: [email protected]
Prepared using pdfslide developed by C. V. Radhakrishnan of River Valley Technologies,Trivandrum, India
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What is a Contact Manifold?
A contact manifold is the odd dimensional analogue of a symplectic
manifold. This idea emerges in classical mechanics in two different ways:
1. A system whose hamiltonian that depends explicitly on time; time
must be included as a co-ordinate in the phase space, hence it is
odd dimensional.
2. For a conservative system, the orbits lie in the surface of constant
energy, which is again odd dimensional.
Contact manifolds also arise in geometry: the co-sphere bundle of a
Riemannian manifold is a contact manifold. (It is the phase space of
the geodesic equations.)
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Contact Structure
Defn.
A contact form on a manifold of dimension n = 2k + 1 is a one-form
that satisfies
α ∧ (dα)k 6= 0
at each point. Two such forms are considered equivalent if they only
differ by multiplication by a positive function (a ‘gauge transformation’):
α ∼ fα.
A contact manifold has a contact form in each co-ordinate patch, there
being such positive functions that relate the contact forms on overlap-
ping patches.
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Examples
The analogue of Darboux’s theorem says that there is a local co-
ordinate system ( and choice of gauge) in which a contact form is
α = dz +
k∑i=1
pidqi.
Thus R2k+1 with this choice is the basic example of a contact manifold.
Given a symplectic manifold and a function w on it, the surface w =
constant is (up to minor technicalities) a contact manifold. Locally we
can choose the symplectic form to be of the form
ω = dθ, θ = w(dz + pidqi)
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The sub-manifold w = constant carries the induced one-form
α = dz + pidqi;
the ambiguity in the choice of co-ordinate is refected in the gauge trans-
formation α → fα.
A special case is a co-sphere bundle of a Riemannian manifold: the
bundle of 1-forms of unit length. The co-tangent bundle of any manifold
is a symplectic manifold. The length of the co-tangent vector set to one
is the constraint.
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Contrast with Symplectic Reduction
A single constraint W = constant is always first class. Dirac’s philos-
ophy of symplectic reduction is to regard as the true or ‘reduced’ phase
space the quotient of this constrained space by the orbits of the canoni-
cal transformation generated by W . Alternately, we allow as observables
only functions of the total space that have zero Poisson bracket with
W .
This procedure is not physically correct in all cases: we will show an
example from the theory of liquid crystals where we need to consider all
functions on the constrained phase space,not just those that commute
with W .
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A Fatal Flow in Symplectic Reduction
The quotient of the constained phase space by the orbits of w simply
may not exist as a manifold: the orbit can be dense in w. In fact
generically such orbits do not exist when w is the hamiltonian of a
conservative mechanical system due to chaos.
For example, the co-sphere bundle of a Riemann surface of constant
negative curvature does not admit a quotient by the orbits, as the orbits
fill all of the manifold.
We need a way to think of the odd dimensional space itself as a phase
space.
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Lightning Review of Mechanics
A symplectic form is a closed two-form that is non-degenerate:
dω = 0, ivω = 0 ⇒ v = 0.
This of course requires the manifold carrying ω to be even dimensional.
A symplectomorphism (‘canonical transformation’) is a diffeomor-
phism that preserves the sympletic form, φ∗ω = ω. Infinitesimally,
a symplectic vector field satisfies Lvω = 0. Since Lvω = d(ivω), this
implies that locally there is a function (‘generating function’) such that
ivω = gv.
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The commutator of two symplectic vector fields is also symplectic.
This defines a commutator (‘Poisson bracket’) on the generating func-
tions:
g1, g2 = r(dg1, dg2)
where r is the inverse tensor of ω. These brackets satisfy the axioms of
a Poisson Algebra
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Poisson Algebra
Defn.
A Poisson Algebra is a commutative algebra A with identity along
with a bilinear , : A⊗ A → A that satisfies
1. g1, g2 = −g2, g2
2. g1, g2, g3 + g2, g3, g1 + g3, g1, g2 = 0 Jacobi identity
3. g1, g2g3 = g1, g2g3 + g2g1, g3 Leibnitz Rule
The last property implies that the Poisson bracket of a constant with
any function is zero.
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Examples of Poisson Algebras
The basic example is the algebra of functions on the plane:
g1, g2 = ∂xg1∂yg2 − ∂yg1∂xg2.
More generally the set of function on a symplectic manifold form a
Poisson algebra, with bracket we gave earlier. Conversely, if the Pois-
son algebra is non-degenerate (the only elements that have zero Poisson
bracket with everything are constants) it arises from a symplectic man-
ifold this way.
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Also, the set of functions on the dual of a Lie algebra is a Poisson
algebra (Kirillov):
F, G(ξ) = iξ[dF, dG]
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A Generalization of Poisson Algebra
Defn
A commutative algebra A with identity and a bilinear , : A×A → Ais a Generalized Poisson Algebra if
1. g1, g2 = −g2, g2
2. g1, g2, g3 + g2, g3, g1 + g3, g1, g2 = 0
3. g1, g2g3 = g1, g2g3 + g2g1, g3 + 1, g1g2g3.
Generalized Leibnitz Rule
The main point is that the constant function is no longer in the center.
The commutant of the constant function is a Poisson algebra.
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Applications
1. The quantization of time dependent systems: phase space includes
time
2. Quantization of the phase space with constant energy in a conser-
vative system
3. Cholesteric Liquid Crystals- We will focus on this example in this
talk.
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Contact Manifolds Give Generalized Poisson Algebras
We will restrict to the case of R3 for simplicity. Let α be a contact
form. Then the condition on a vector field v to preserve the contact
structure is that there exist a function fv with
Lvα = fvα ⇒ α ∧ Lvα = 0.
Then, fv will satisfy the condition for a one-cocycle:
Lvfv − Lvfv = f[v,v]
It is useful to write the condition Lvα = fvα in the more elementary
notation of vector calculus:
∇(α · v) + β × v = fvα
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where β = curl α. Taking cross product with α, we can solve for v
since α. curl α 6= 0.
v =α×∇gv + βgv
α · β, gv = α · v.
Thus the component of the velocity along the director determines the
others. Putting this back into Lvα,
fv =β · ∇gv
α · β
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Gauge Invariance
Recall the contact form is only given up to multiplication by a non-
zero function, α → λα. Thus all observables such as velocity must be
gauge invariant under this transformation. In fact
gv → λgv, α×∇gv → α×∇λ gv + λα×∇gv
β → ∇λ× α + λβ, α → λ2α · β,
imply that the above formula for v is gauge invariant. We can regard
α×∇g + βg as a kind of covariant derivative.
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The Commutator
The commutator of vector fields induces a bracket on the generating
functions:
g[v,v] = Lvgv − fvgv
Or more explicitly, we have an analogue of the Poisson bracket for func-
tions on a three dimensional manifold:
g, g =α · [∇g ×∇g] + β[g∇g −∇g g]
α · β
This is obviously anti-symmetric and the Jacobi identity can also be
checked.
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This is not a Poisson Algebra
However, the Leibnitz rule is not satisfied!
g1, g2g3 − g1, g2g3 − g2g1, g3 =β · ∇g1
α · βg2g3 6= 0.
In particular,
1, g =β · ∇g
α · β.
So we have instead of the Leibnitz rule, a new identity
g1, g2g3 = g1, g2g3 + g2g1, g3 + 1, g1g2g3.
Note that if g2 = 1 both sides reduce to g1, g3.
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Commutation RelationsWith the choice α = dz+ 1
2[xdy−ydx] the analogue of the canonical
commutation relations can be worked out:
x, y = w, w, x = 0, w, y = 0
z, x =1
2x, z, y =
1
2y, z, w = w
The element w (which correspond to the constant function 1) is not
central anymore. w, x, y span a Heisenberg sub-algebra. z generates
the automorphism of the Heisenberg algebra which scales w, x, y. Since
the Leibnitz rule is replaced by the new identity, we have to be careful
about using these commutation relations to derive brackets for more
general functions. e.g., z, xy = 0.
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Representation of Commutation Rela-tions
A unitary representation of this Lie algebra can be constructed using
the usual ideas of induced representation theory. On functions of two
variables, w, y (which are represented by multiplication):
x = −iw∂
∂y, z = − i
2x
∂
∂x− i
2y
∂
∂y− iw
∂
∂w.
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Fluid Mechanics
Fluids display many phenomena that remain puzzling to physicists.The
motion of individual molecules in the fluid follows simple well-understood
laws of classical mechanics. The collective motion of a large number of
these molecules causes pheneomens such as
1. Turbulence. Onset of turbulence could be a kind of critical phenomenon-
still poorly understood.Large scale disorder.
2. Chaos. Extreme sensitivity to initial conditions. “ A butterfly flaping
its wings in Australia can cause rain in New Jersey”
3. Stable Vortices How can hurricanes and the ‘Red Eye of Jupiter’-
stable over long distances and times-arise out of chaos? .
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Collective Variables
We need to give up on describing a fluid in terms of the position and
momentum of each molecule, and instead pass to macroscopic variables
such as pressure, density and velocity of fluid elements that contain
averges over many molecules. This was done already in the eighteenth
century by Leonhard Euler, “the Master of us all” mathematical physi-
cists.
He applied this philosophy also to a rigid body, a collection of molecules
that move together,keeping the distance between two of them fixed.
There is a surprising mathematical similarity between these two systems,
a connection that could not have escaped Euler: In modern language,
they both describe geodesic motion on subgroups of the diffeomorphism
group. V. I. Arnold and B. Khesin Topological Methods in Hydrodynamics
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Mechanical Systems out of Lie Algebras
Given a Lie algebra G and a positive (not invariant) bilinear A on it,
we can define a mechanical system. The dual of the Lie algebra defines
a Poisson bracket on the functions of its dual (Kirillov):
ωa, ωb = ω[a,b], F, G(ω) =< ω, [dF, dG] >
The positive bilinear defines a function H = 12 < ω, A−1ω > which serves
as the hamiltonian (kinetic energy). Together they yield the equations
of motiondω
dt= ad∗A−1ωω.
Geometrically, this describes geodesic motion on the group G of the Lie
algebra, with respect to the left-invariant (but not isotropic) metric A.
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Examples: Various Collective Motions
Each collective motion is determined by the physical quantity it leaves
invariant:
1. Rigid Body: Isometries, Lvgij = 0 ⇐⇒ ∂ivj + ∂jvi = 0.
2. One dimensional compressible flow: Diff(R)
3. Two dimensional incompressible flow: Canonical Transformations,
Lvω = 0 ⇐⇒ vi = ωij∂jf .
4. Liquid Crystals: transformations preserving a direction Lvα = fα.
Nematic: dα ∧ α = 0 chiral nematic:dα ∧ α 6= 0.
5. Three dimensional incompressible flow: Lvρ = 0 ⇐⇒ div v = 0
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Poisson Algebras in Fluid Mechanics
Poisson algebras and their generalizations appear in fluid mechanics
at two levels: as a hamiltonian system, the fluid has a phase space with
a Poisson bracket and hamiltonian.
But also the velocity fields of the fluid is also sometimes required to
preserve a symplectic or contact form. Incompressible vector fields in
two dimensions are the same as symplectic vector fields: the area form
is the symplectic form. We will see that three dimensional analogue
is a contact vector field, which decsribes the flow of cholesteric liquid
crystals.
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The Euler Equations
The Euler equations of an incompressible inviscid fluid are
∂
∂tv + (v · ∇)v = −∇p, div v = 0.
We can eliminate pressure p by taking a curl. Defining the vorticity
ω = curl v and using (v · ∇)v = ω × v + 12∇v2, we get,
∂
∂tω + curl [ω × v] = 0.
We can regard ω as the basic dynamic variable of the system, since v
determined by it 1.
1 We assume that the circulation∫
Cv around con-contactible loops (if any) C are zero and
that the boundary values of the velocity are given.
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Incompressible Flows
If the velocity of the fluid is small compared to the speed of sound in
it, the density of the fluid cannot change. This imposes a constraint of
incompressibility, weaker than that of a rigid body:
det∂φ
∂x= 1.
The velocity has to satisfy the infinitesimal version of this condition,
div v = 0. There are still an infinite number of such vectors.
See V. I. Arnold and B. Khesin Topological Methods in Hydrodynam-
ics for more on the geometrical picture of fluid flow.
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Geodesic Motion
There is a natural way to measure the ‘size’ of an incompressible
vector field:
||v||2 =
∫v2(x)dx.
It has a simple physical meaning as well: it is proportional to the total
kinetic energy of the fluid. This defines a metric on the tangent space
of the group of volume preserving diffeomorphisms. By left translation
this becomes a homogenous but not isotropic metric on the group itself.
Euler’s equations simply state that the fluid always moves along the
geodesics of this metric!
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Poisson Brackets
The Poisson bracket of two functions of vorticity is defined to be
F, G =
∫ω ·
[curl
δF
δω× curl
δG
δω
]d3x
This is just the natural Poisson bracket on the dual of the Lie algebra
of incompressible vector fields: recall that the dual of any Lie algebra
has a natural Poisson structure (Kirillov).
Using the identity div [a× b] = b · curl a− a · curl b this may also
be written as
F, G =
∫curl
[ω × curl
δF
δω
]· δGδω
d3x
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The Hamiltonian Formalism
The hamiltonian is
H =1
2
∫v · vd3x.
Using the identity
curlδF
δω=
δF
δvwe get H, ω = curl [ω × v] as needed to get the Euler equations.
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Analogy to Rigid Body Mechanics
The Euler equations of a rigid body are
dL
dt= L× Ω, L = AΩ
Its analogy with his equations of a fluid could not have escaped Euler.
Vorticity ω is analogous to angular momentum L; fluid velocity v to
angular velocity Ω; the curl operator is analogous to moment of inertia
tensor A.
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Hamiltonian Formulation of the RigidBody
The Poisson brackets are those of the dual of the Lie algebra of rota-
tions
Li, Lj = εijkLk
The hamiltonian that gives the Euler equations is
H =1
2< L,A−1L >
It is well known that these are the geodesics of a homogenous but not
always isotropic metric on the rotation group, determined by A.
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Sensitivity to Initial Conditions
In flat space, geodesics are straight lines: a small change in the initial
point or direction only grows as a power of time. But if the space
has negative curvature, geodesics that start out close depart from each
other exponentially fast. ( They focus towards each other for positive
curvature, as in the case of great circles on a sphere).
The reason why hydrodynamics is so unstable is that the curvature
of the metric of the configuration space is negative all except a finite
number of directions. This means that even small fluctuations in initial
data cannot ever be ignored. Rigid body mechanics by contrast has only
one unstable dierection ( rotation around the eigenvector of the middle
eigenvalue of A).
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Entropy
We deal with such systems all the time in statistical mechanics. The
basic idea is to look for ‘macroscopic’ variables (density, pressure etd.)
that are averages over large numbers of particles so that fluctuations
average out. But then we have to live with partial information: with
entropy. The most likely state of the system will be one that maximizes
this entropy for a given value of the consderved quantities.
Is there a similar notion of entropy for turbulent fluctuations?
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Matrix Models
It has emerged recently that many of the above examples of collective
motion of molecules also arise as collective motion of matrix models.
Perhaps the most well-known is the case of a hermitean matrix model
(Sakita,Jevicki, Das, Karabali..). The motion of eigenvalues is mapped
first to a system of free fermions and then to a compressible one dimen-
sional fluid with a non-local ( integro-differential) equation of motion of
the Benjamin-Ono type.
Two dimensional incompressible flow is also connected to a hermitean
matrix model, with a different hamiltonian which is not invariant un-
der unitary transformations(Fairley, Zachos,Dowker,Rajeev). Indeed the
eigenvalues flow trivially (are conserved quantities). In a sense this is
the opposite of the previous case.
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Regularization by Matrix Models
It is not unusual that very different microscopic dynamics can lead
to the same collective motion. Both molecular dynamics and Matrix
models lead to the same kind of fluid flow as collective motion: they
can both be thought of as regularizations of fluid flow with a finite
number of degrees of freedom.
The regularization using matrix models is more elegant as it retains a
geometric flavor: in essence the underlying manifold is replaced by a non-
commutative manifold. This preserves all the conservation laws, which
is difficult to do in other regularization schemes for fluids. Practically
useful for numerical solutions.
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Two-Dimensional Euler Equations
It is useful to look first at the much simpler example of two dimensional
incompressible flow.
Area preserving transformations are the same as canonical transfor-
mations. The corresponding Lie algebra is the algebra of symplectic
transformations on the plane:
[f1, f2] = εab∂af1∂bf2.
The above Lie bracket of functions gives the Poisson bracket for vorticity:
ω(x), ω(y) = εab∂bω(x)∂aδ(x− y).
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Hamiltonian Formulation
Euler equations follow from these if we postulate the hamiltonian to
be the total energy of the fluid,
H =1
2
∫u2d2x =
1
2
∫G(x, y)ω(x)ω(y)d2xd2y.
The quantities Qk =∫
ωk(x)d2x are conserved for any k = 1, 2 · · ·:these are the Casimir invariants. In spite of the infinite number of
conservation laws, two dimensional fluid flow is chaotic.
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Lie Algebra of Canonical Transforma-tions
The Lie algebra of symplectic transformations can be thought of as
the limit of the unitary Lie algebra as the rank goes to infinity. To see
this, impose periodic boundary conditions and write in terms of Fourier
coefficients as
H = (L1L2)2
∑m 6=(0,0)
1
m2|ωm|2, ωm, ωn = − 2π
L1L2εabmanbωm+n.
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Non-Commutative Regularization
Using an idea of Fairlie and Zachos, we now truncate this system
by imposing a discrete periodicity mod N in the Fourier index m; the
structure constants must be modified to preserve peridocity and the
Jacobi identity:
ωm, ωn =1
θsin[θ(m1n2 −m2n1)]ωm+n mod N , θ =
2π
N.
This can be thought of as a ‘quantum deformation’ of the Lie algebra of symplectic transformations. This is the Lie
algebra of U(N).
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Regularized hamiltonian
The hamiltonian also has a periodic truncation
H =1
2
∑λ(m)6=0
1
λ(m)|ωm|2,
λ(m) =
N
2πsin
[2π
Nm1
]2
+
N
2πsin
[2π
Nm2
]2
.
This hamiltonian with the above Poisson brackets describe the geodesics
on U(N) with respect to an anisotropic metric. We are writing it in a
basis in which the metric is diagonal.
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Entropy of Matrix Models
The constants Qm =∫
ωm(x)d2x define some infinite dimensional
surface in the space of all functions on the plane. The micro-canonical
entropy (a la Boltzmann) of this system will be the log of the volume of
this surface. How to define this volume of an infinite dimensional man-
ifold? We can compute it in the regularization and take the limit. It is
convenient to regard ω as a matrix by defining ω =∑
m ωmU(m) where
U(m) = Um11 Um2
2 with the defining relations U1U2 = e2πiN U2U1. In this
basis, the Lie bracket of vorticity is just the usual matrix commutator.
Then the regularized constants of motion are Qk = 1N trωk. The
set of herimtean matrices with a fixed value of these constants has a
finite volume,known from random matrix theory:∏
k<l(λk − λl)2, the
λk being the eigenvalues.
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Entropy of Turbulent Flow
The entropy is thus
S =1
N 2
∑k 6=l
log |λk − λl| = P∫
log |λ− λ′|ρ(λ)ρ(λ′)
where ρ(λ)dλdλ′ = 1N
∑k δ(λ− λk).
In the continuum limit this tends to a remarkably simple formula:
S = P∫
log |ω(x)− ω(y)|d2xd2y
Even without a complete theory based on the Fokker-Plank equa-
tion (assuming that its continuum limit does exist) we can make some
predictions about two dimensional turbulence.
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Entropy for Two Dimensional Flow
Savitri V. Iyer and S.G. Rajeev Mod.Phys.Lett.A17:1539-1550,2002;
physics/0206083
We found a remarkably simple formula that measures the turbulent
entropy for two dimensional incompressible flow:∫log |ω(x)− ω(y)|dxdy.
We don’t have one yet for three dimensional flow yet.
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The Profile of a Hurricane
What is the vorticity profile that maximizes entropy for fixed value of
mean vorticity Q1 and enstrophy 2? This should be the most probable
configuration for a vortex profile. Using a simple variational argument
we get the answer in parametric form
ω(r) = 2σ sin φ + Q1, r2 =1
2[a2
1 + a22]± [a2
2− a21]
1
π
[φ +
1
2sin (2φ)
]in the region a1 ≤ r ≤ a2. We should expect this to be the vorticity
distribution of the tornados and hurricanes.
2 Q2 = σ2 + Q21
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Vorticity vs Radial Distance
2 4 6 8 10 12 14radius
4
5
6
7
Vorticity
Notice the ‘eye’of the hurricane: the flow is fastest right inside the
eyewall and then decreases gradually to the outer wall.
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Reverse Cascade
In three dimensions, vortices tend to break up into smaller scales,
leading to very complicated behavior (the ‘cascade’ effect). In two di-
mensional flow, the opposite can be observed: vortices tend to combine
into a few big ones. We have a simple explanation for this phenomenon:
The entropy of vortices increases as they combine!
The hurricane is stable in a chaotic environment because it maximises
the entropy.
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What Lies in Between Two and ThreeDimensions?
Such a non-commutative geometric regularization is not completely
understood for three dimensional flow yet. I will describe a case in-
termediate between two and three dimensions, that of liquid crystals,
where we can find a ‘matrix regularization’ of fluid motion. There are
also interesting connections to ideas of differential geometry.
Liquid crystals are very convenient media on which to perform exper-
iments. Phenomena are simpler than in three dimensions yet complex
enough to demonstrate turbulence and chaos.
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Flow of Liquid Crystals
Liquid crystals are molecules that are so long that they cannot freely
move past each other. In the simplest phase (‘nematic’) the molecules
are all aligned in the same direction. Only motion that preserves this
direction can happen at small cost of energy. Just as we can deform
even a rigid body at some cost of elastic energy, the direction can also
be changed: by exerting external forces by an electric field for example-
how an LCD works.
Thus liquid crystal flow is an intermediate case in between two and
three dimensional flow. Geometrically, the direction of the molecules is
best described as a one-form α (the director). However if we multiply
α by an everywhere non-zero function the orientation described by it
doesn’t change.
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Liquid Crystal Groups
The flow of a liquid crystals is described by diffeomorphisms that
preserve the director up to such a multiplication:
φ∗α = fα.
We need to distinguish two very different cases:
α ∧ dα = 0
the nematic phases and the cholesteric or chiral nematic phase
α ∧ dα 6= 0.
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Frobenius Integrabiity
One is tempted to call the nematic phase where α∧dα = 0 the Frobe-
nius phase. Its geometric meaning is that the tangent planes transversal
to α at each point can be integrated (locally) into a two dimensional
submanifold. Frobenius theorem tells us that locally there are func-
tions τ and σ such that α = τdσ Reminds one of thermodynamics a
la Caratheodory! Unlike in thermodynamics, we have the freedom to
multiply α by a non-zero function.
We can even choose ‘the gauge’ α = dσ The vector fields transversal
to α are tangential to the surfaces
σ = constant.
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Contact Geometry
The cholesteric phase is the exact opposite: the integrability condi-
tion for the transversal planes to fit into a local submanifold is violated
everywhere. In this case, the director defines a contact structure on
R3. The analogue of Darboux theorem for contact manifolds says that
locally there are functions z, x, y such that
α = dz +1
2[xdy − ydx].
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Flow Vector Fields of the Nematic phase
Suppose α ∧ dα = 0. The allowed flows are such that
Lvα = fvα
where fv is a function that depends linearly on v. Suppose we choose
the z-axis along the director. Then α = dz an the condition above
becomes dvz = fvdz. This means that
∂vz
∂x= 0 =
∂vz
∂y.
There is no condition on the transversal components vx, vy. Such vector
fields form a Lie algebra.
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Cholesteric Flows preserve Contact Structure
A contact structure on a three dimensional manifold is a one form
(modulo multiplication by a non-zero function) satisfying α ∧ dα 6= 0.
( see V. I. Arnold Classical Mechanics). Thus the group of flows of
the cholesteric phase (satisfying φ∗α = fφα) are precisely the ‘contact
transformations’ familiar from classical mechanics.
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Cholesteric Equations of MotionIn the absence of external forces, the liquid crystal will flow subject
to internal forces necessary to maintain the constraint α ∧ Lvα = 0. If
we impose the condition with a Lagrange multiplier p ( a vector field
playing the same role that pressure plays for incompressible fluids), these
forces are given by
δ
δv
∫p · [α×∇(α · v) + βα · v − vα · β]d3x
Thus the analogues of Euler’s equations are
∂v
∂t+ v · ∇v = α[ div (α× p) + β · p]− α · β p
The constraint of preserving the director can be used to determine the
additional unknowns p.
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The Non-Commutative T 3
This leads us to a non-commutative analogue of the three torus:
XY = WY X, XN = Y N = WN = 1, (1)
ZXZ−1 = Xr ZY Z−1 = Y r, ZWZ−1 = W r2
where N is a prime number and 2 ≤ r ≤ N − 1.
What is the non-commutative S3?