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Laurette TUCKERMAN laurette@pmmh.espci.fr Hamiltonian Systems Hamiltonian Systems H ( p 1 , . . . p N , q 1 , . . . q N ) q i = H p i = H p i q i q i : positions p i : momenta convention for number of degrees of freedom:


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Laurette TUCKERMAN laurette@pmmh.espci.fr

Hamiltonian Systems

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Hamiltonian Systems

H(p1, . . . pN, q1, . . . qN) ˙ qi = ∂H ∂pi ˙ pi = −∂H ∂qi qi : positions pi : momenta convention for number of degrees of freedom: N (for dissipative systems, convention would be 2N)

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Conservation of volumes for ˙ x = f(x) V (t + dt) − V (t) = dt

  • surface

f · n da = dt

  • volume

∇ · fdv = dt

  • volume
  • i

∂ ˙ xi ∂xi dv = dt

  • volume
  • i

∂ ˙ qi ∂qi + ∂ ˙ pi ∂pi

  • dv

= dt

  • volume
  • i

∂2H ∂qi∂pi − ∂2H ∂qi∂pi

  • dv

= 0

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Developed in 18th century for celestial mechanics, now used in plasma physics (e.g. fields in a Tokamak) quantum systems (e.g. quantum optics, Bose-Einstein conden- sation) Fluid mechanics: 2D streamfunction ψ(x, y) u = ez × ∇ψ. Motion of particle at (x, y): dx dt = u = −∂ψ ∂y dy dt = v = ∂ψ ∂x Particles move along streamlines = curves of constant ψ ⇐ ⇒ In general, trajectories move along curves/surfaces of constant energy H

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Integrable systems

Hamiltonian system with N degrees of freedom is integrable if ∃ N functions Fj(p, q) such that dFj dt = 0 and [Fj, Fk] ≡

  • i

∂Fj ∂qi ∂Fk ∂pi − ∂Fj ∂pi ∂Fk ∂qi

  • = 0

Already have dH dt =

  • i

∂H ∂qi ˙ qi + ∂H ∂pi ˙ pi

  • =
  • i

∂H ∂qi ∂H ∂pi − ∂H ∂pi ∂H ∂qi

  • = 0

so any system with one degree of freedom is integrable,

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[Fj, H] =

  • i

∂Fj ∂qi ∂H ∂pi − ∂Fj ∂pi ∂H ∂qi

  • =
  • i

∂Fj ∂qi ˙ qi + ∂Fj ∂pi ˙ pi

  • = dFj

dt so dFj dt = 0 = ⇒ [Fj, H] = 0 N − 1 functions Fj are needed for an N-degree-of-freedom system to be integrable.

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For an integrable system, there exists a transformation (I, θ) ← (p, q) H′(I, θ) = H(p, q) where, in fact, H′(I, θ) = H′(I) so that the dynamics in the (I, θ) variables are ˙ Ii = −∂H′ ∂θi = 0 ˙ θi = ∂H′ ∂Ii = ωi(I) Ii(t) = Ii(0) θ(t) = θ(0) + tωi Called twist map (I, θ) are called action-angle variables

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Classic pendulum H = 1 2p2 − cos q q: angle (position), p: (velocity = momentum) Phase portrait for the classic pendulum

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I ≡ 1 2π

  • pdq

Integral taken over a closed trajectory, on which H has the constant value H. For the pendulum: H = 1 2p2 − cos q p2 = 2(H + cos q) p =

  • 2(H + cos q)

I = 1 2π 2π

  • 2(H + cos q) dq

= ⇒ I (canonical action variable) as a function of value of H (can be inverted to define H′ as function of I) Also define θ (canonical angle variable) such that ˙ θ = ω is constant in time

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Left: H(I). Middle: pendulum configuration for H > 1 (repeated clock- wise or counterclockwise rotations) and H < 1 (small oscillations) Right: (q, p) trajectories, heteroclinic orbit at H = 1, ω = dH/dI = 0.

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Non-integrable perturbations

All Hamitonian systems with N = 1 are integrable Simplest non-integrable systems are of form: H(p1, p2, q1, q2) N = 2 H(p, q, t) sometimes called N = 1.5 Rotor in horizontal plane gets a “kick” with period τ = 2π

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H(v, θ, t) = v2 2 + ǫ cos θ

  • n

δ(t − nτ) ˙ θ = ∂H

∂v = v

θn+1 − θn = vn mod 2π ˙ v = −∂H

∂θ = ǫ sin θ n δ(t − nτ) vn+1 − vn = ǫ sin θn+1

H = H0(θ, v) + ǫ H1(θ, v, t) H0 = v2 2 H0 = v2/2 is integrable and already in action-angle variables = ⇒ phase space = set of concentric curves, each with its own (constant) angular velocity.

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Unperturbed Twist Map

Points on circle Ij rotate with velocity Ij Here I ∼ p ∼ v ∼ ω ∼ r

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Define the Poincar´ e or first return map arising from H0: T0(I, θ) = (I, θ)(t = 2π) = (I, (θ + 2πI) mod 2π) Each circle is invariant under T0, but its individual points are not necessarily invariant. Circle v = 0 circle consists of fixed points, circle v = 1/2 consists of 2-cycles, circle v = 1/3 consists of 3-cycles. Five-cycles of map T0

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Define nth iterate of T0. T n

0 (I, θ) = (I, θ)(t = 2πn) = (I, (θ + 2πn I) mod 2π)

If v = I = ω(I) = m/n, then T n

0 (I, θ) =

  • I,
  • θ + 2π n m

n

  • mod 2π
  • = (I, (θ + 2π m) mod 2π) = (I, θ)

so circles I = m/n consist of fixed points of T n

0 .

Re-introduce the perturbation: Hǫ ≡ H0 + ǫ H1 and the corresponding maps T n

ǫ (I, θ) ≡ (I, θ)(t = 2π n)

where I and θ evolve according to Hamiltonian Hǫ

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Poincar´ e-Birkhoff Theorem

Action of map T n

ǫ on curve I = m n :

–The image of (I, θ) under T n

ǫ is

T n

ǫ (I, θ) = (I′, θ)

The radius changes but not the angle. –Curves (I, θ) and (I′, θ) intersect each other a multiple of 2n times, creating alternating hyperbolic and elliptic points. –Area inside (I′, θ) is the same as that inside (I, θ).

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Dynamics of T q near a circle with rational I = p/q

Left: Points on intermediate circle are fixed, those on outer (inner) circle rotate counterclockwise (clockwise) Right: P-B theorem implies curves (I, θ) and T n

ǫ (I, θ) = (I′, θ) intersect

at alternating set of elliptic and hyperbolic fixed points. Angular flow is counterclockwise outside and clockwise inside and radial flow alternates inwards and outwards.

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Each new elliptic point is now surrounded by invariant circles, some of which have rational winding numbers. Poincar´ e-Birkhoff theorem applies recursively to each one! Fixed points of T n = ⇒ elliptic or hyperbolic points of T n

ǫ

What happens to new hyperbolic points?

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Unstable and stable manifold of hyperbolic A and B are points approaching them in iterating backwards or forwards: W U(A) ≡

  • x : lim

k→∞ T −k(x) = A

  • W S(B) ≡
  • x : lim

k→∞ T k(x) = B

  • W U(A) = W S(B) intersect transfersely

integrable H non-integrable H

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Non-integrable pert = ⇒ W U(A) and W S(B) cross at C T k and T −k map C into other points, all in W U(A)∩W S(B) Infinite number of intersections accumulate at A and B Intersections along decreasing distances + area conservation = ⇒ perpendicular directions increase = ⇒ homoclinic tangles near A and B = ⇒ chaos = separation of nearby points = sensitivity to initial conditions (SIC)

From E. Weisstein, Homoclinic Tangle, MathWorld: A Wolfram Web Resource http://mathworld.wolfram.com/HomoclinicTangle.html

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From P. So, Unstable periodic orbits, Scholarpedia 2(2): 1353

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The combined complexity of the chains of elliptic and hyper- bolic points and the homoclinic tangles was said by Poincar´ e to be too complicated to describe. Arnold tried:

Solid ellipses: surviving tori, whose winding numbers are sufficiently far from any ratio-

  • nal. Others break into alternating elliptic and hyperbolic points. Around each elliptic

point is a set of elliptical trajectories. Each hyperbolic point is surrounded by a chaotic

  • region. From V.I. Arnol’d, Small denominators and problems of stability of motion in classi-

cal and celestial mechanics, Russian Mathematical Surveys 18:6, 85–191 (1963). Reprinted in Hamiltonian Dynamical Systems: a reprint collection, ed. R.S. MacKay & J.D. Meiss

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KAM Theorem

Kolmogorov (1954), Arnold (1961-3), Moser (1962) Poincar´ e-Birkhoff Theorem: tori with rational winding numbers w are destroyed by non-integrable perturbation What about tori with irrational w? If the perturbation is sufficiently small, some survive. A torus whose w is close to a rational with small denominator, (“not very irrational”) is destroyed by a small perturbation. A torus whose w is sufficiently far from all rationals (i.e. is “very irrational”) requires a large perturbation to be destroyed. “Most irrational” number is golden mean (1 + √ 5)/2, whose torus is last one destroyed, i.e. perturbation required is largest.

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∃K(ǫ) such that lim

ǫ→0 K(ǫ) = 0

and such that if w satisfies ∀m, n

  • w − m

n

  • > K(ǫ)

n5/2 then torus with winding number w survives pert of size ǫ Estimate measure of interval of w of surviving tori: Each denominator n corresponds to ∼ n rationals 1

n, 2 n, . . . n−1 n

Surrounding each rational is w-interval of destroyed tori

m n − K n5/2 < w < m n + K n5/2 ∞

  • n=1

2K(ǫ) n5/2 n = 2K(ǫ)

  • n=1

1 n3/2 ≤ 2K ∞

n=1

dx 1 x3/2 = 2K(ǫ)

  • −2

3 1 x1/2 ∞

1

= 4K(ǫ) 3 < 1 for small ǫ For small ǫ, set of surviving w has finite (non-zero) measure!

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Celestial Mechanics: I. Two-body problem

Mass µ has position q = (r, φ) momentum p = (pr, pφ) = (µ ˙ r, µr2 ˙ φ) H0(q, p) = |p|2 2µ − GMµ r = p2

r + p2 φ/r2

2µ − GMµ r dr dt = ∂H0 ∂pr = pr µ dpr dt = −∂H0 ∂r = p2

φ

µr3 − GMµ r2 dφ dt = ∂H0 ∂pφ = pφ µr2 dpφ dt = −∂H0 ∂φ = 0 N = 2 degrees of freedom (r, pr, φ, pφ) angular momentum pφ conserved = ⇒ integrable

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Three-body problem

Historically, main motivation for studying celestial mechanics has been to determine whether the solar system is stable. Even three-body problem is known to be non-integrable. Euler, Lagrange, Jacobi, Hill, Poincar´ e, Levi-Civita and Birkhoff studied circular restricted three-body problem (CRTBP): M ≫ m ≫ µ m has circular orbit around M. Neither is affected by µ.

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M (sun) ≫ m (planet) ≫ µ (asteroid) Integrable two-body problem: µ moves under influence of M Non-integrable perturbation: m perturbs motion of µ µ small: –neglect effect of µ on m and M –identify center of mass of M − m system with center of M In addition, assume: –m rotates about M in circular orbit –µ remains in plane containing M and m

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Integrable Hamiltonian system H0 without mass m H0(q, p, t) = p2

r + p2 φ/r2

2µ − GMµ r where pφ is the angular momentum µr2 ˙ φ dr dt = ∂H0 ∂pr = pr µ dφ dt = ∂H0 ∂pφ = pφ µr2 = ˙ φ dpr dt = −∂H0 ∂r = p2

φ

µr3 − GMµ r2 = µ2r4 ˙ φ2 µr3 − GMµ r2 = µr ˙ φ2 − GMµ r2 dpφ dt = ∂H0 ∂φ = 0 = ⇒ conserved quantity

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Introduce intermediate mass m, at distance |q − Rm| from µ: H(q, p, t) = |p|2 2µ − GMµ r − Gmµ |q − Rm(t)| Mass m follows circular orbit = ⇒ Rm(t) changes orientation = ⇒ H is non-autonomous (depends explicitly on time) Autonomous H via rotating frame φ → φ′ but retain pφ: φ′ = φ − Ωt ∂H′ ∂pφ = dφ′ dt = dφ dt − Ω = pφ µr2 − Ω H′

0(q′, p) =

p2

r + p2 φ/r2

2µ − Ωpφ − GMµ r H′(q′, p) = p2

r + p2 φ/r2

2µ − Ωpφ − GMµ r − Gmµ |q′ − Rm| where Rm is now constant. Ωpφ is Coriolis term.

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Action variable Iφ = 1 2π 2π pφ dφ = pφ Action variable Ir p2

r = 2µ(H0 + ΩIφ + GMµ/r) − I2 φ/r2

Ir = 1 2π

  • prdr = −Iφ +

GMµ2

  • −2µ(H0 + ΩIφ)

1 Ir + Iφ =

  • −2µ(H0 + ΩIφ)

GMµ2 H0 = −ΩIφ − 1 2µ GMµ2 Ir + Iφ 2 ≡ H0(Ir, Iφ) Frequencies ω0r = ∂H0 ∂Ir = (GM)2µ3 (Ir + Iφ)3 ≡ ωµ ω0φ = ∂H0 ∂Iφ = −Ω + (GM)2µ3 (Ir + Iφ)3 = −Ω + ωµ

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H′(q′, p) = p2

r + p2 φ/r2

2µ − Ωpφ − GMµ r − Gmµ |q′ − Rm| H′ depends on φ′ through q′ so dpφ dt = −∂H′ ∂φ′ = − ∂H′ ∂|q′ − Rm| ∂|q′ − Rm| ∂φ = 0 H′ non-integrable = ⇒ m destroys tori with rational w of H′ Winding number w is ratio ω0φ ω0r = −Ω + ωµ ωµ = 1 − Ω ωµ For M=sun and m=Jupiter, Poincar´ e-Birkhoff theorem = ⇒ Kirkwood gaps in frequencies (orbital paths) of asteroids µ For M=Saturn and m=moon of Saturn, P-B theorem = ⇒ gaps in the particles µ in the rings of Saturn

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Kirkwood gaps

Gaps in the distribution of main belt asteroids as function of semi-major axis (equivalent to orbital period). They correspond to the location of orbital resonances with Jupiter. From Wikipedia, Kirkwood gap

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Billiards

Generalized billiard table bounded by closed curve r(φ)

From H.J. Korsch & F. Zimmer, Chaotic Billiards, http://kluedo.ub.uni-kl.de/frontdoor.php?source opus=1202 M.V. Berry, Regularity and chaos in classical mechanics, illustrated by three deformations of a circular billiard, Eur. J. Phys 2, 91-102 (1981)

Trajectory = sequence of bounces = (φn, αn) Bounce = (angular position φ, angle α with tangent to table) (φn, αn) = ⇒ (φn+1, αn+1) Alternately, use arclength S along table and/or p = cos(α) (Sn, pn) = ⇒ (Sn+1, pn+1)

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Circle r = c = ⇒ integrable dynamics since α is conserved Orbits are

  • periodic

if α/2π is rational quasiperiodic if α/2π is irrational Elliptical billiards are also integrable.

Trajectories in elliptical billiards. From H.J. Korsch & F. Zimmer, Chaotic Billiards http://kluedo.ub.uni-kl.de/frontdoor.php?source opus=1202.

Stadium (Bunimovich) = two line segments connected by two semi-circles. Dynamics are ergodic: all points are visited.

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Cosine Billiards

r(φ) = 1 + ǫ cos(φ) ǫ = 0 ǫ = 0.1 ǫ = 0.2 ǫ = 0.3 ǫ = 0: integrable circle case ǫ increases: rational tori break up, destroying irrational tori close to small-denominator fractions ǫ = ǫc: last torus, with w = w∗ golden mean, breaks up

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Low-denominator fractions m/n with angles α

m/n α p = cos(α) m/n α p = cos(α) 1/2 90◦ 1/5 36◦ 0.809 1/3 60◦ 1/2 2/5 72◦ 0.309 2/3 120◦ −1/2 3/5 108◦ −0.309 1/4 45◦ 1/ √ 2 4/5 144◦ −0.809 3/4 135◦ −1/ √ 2 √ 2 127.279◦ −0.6057 w∗ = 0.618 291.262◦ 0.3626

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ǫ = 0.1 ǫ = 0.2 p = cos α ǫ = 0.3 ǫ = 0.4 p = cos α S (arclength) S (arclength)

From H.J. Korsch & F. Zimmer, Chaotic Billiards http://kluedo.ub.uni-kl.de/frontdoor.php?source opus=1202.

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Fluid dynamics

Fluid-dynamical streamfunction can play role of Hamiltonian: dx dt = u = −∂ψ ∂y dy dt = v = ∂ψ ∂x In fluid context, chaos can be desirable: promotes mixing Non-integrable perturbation: blinking vortex Vortex at (+a, 0) is switched on for time T then vortex at (−a, 0) is switched on for time T

  • H. Aref: theory, 1984

Ottino: experiments, 1989

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Rotate ∆θ around (+a, 0): x′ y′

  • =

a

  • +

cos ∆θ − sin ∆θ sin ∆θ cos ∆θ x − a y

  • where ∆θ+(x, y) = κT/((x − a)2 + y2)

Rotate ∆θ around (−a, 0): x′′ y′′

  • =

−a

  • +

cos ∆θ − sin ∆θ sin ∆θ cos ∆θ x′ + a y′

  • where ∆θ−(x′, y′) = κT/((x′ + a)2 + y′2)

Non-dimensional parameter controlling non-integrability: µ = κT/a2

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Simulation of blinking vortex flow shows increasing degree of chaos as µ increases. From H. Aref, Stirring by chaotic advection, J. Fluid Mech. 143, 1–21 (1984).

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Hamiltonian saddle-node bifurcation

center and saddle meet and annihilate δ = 0.2 δ = 0

  • 0.2
  • 0.1

0.1 0.2

  • 0.075
  • 0.05
  • 0.025

0.025 0.05 0.075

  • 0.2
  • 0.1

0.1 0.2

  • 0.075
  • 0.05
  • 0.025

0.025 0.05 0.075

  • 0.2
  • 0.1

0.1 0.2

  • 0.075
  • 0.05
  • 0.025

0.025 0.05 0.075

  • 0.4
  • 0.2

0.2 0.4

  • 0.002
  • 0.001

0.001 0.002

q p q B p q p A C D

q ø

A B C

Q Q Q Q Q +

  • Q-

+ +

  • δ = 0.1

Φ(q)

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Normal form: ¨ q = δ − q2 ⇐ ⇒

  • ˙

q = p = ∂H

∂p

˙ p = δ − q2 = −∂H

∂q = −Φ′(q)

where H = p2 2 + Φ(q) = p2 2 + q3 3 − δq Fixed points are extrema of Φ p = 0 q = ± √ δ for δ > 0 Stability is determined by

  • 1

−2q 0

⇒ λ(−λ) = 2q q = + √ δ ⇐ ⇒ −λ2 > 0 ⇐ ⇒ λ = ±iω ⇐ ⇒ q a center q = − √ δ ⇐ ⇒ −λ2 < 0 ⇐ ⇒ λ = ±σ ⇐ ⇒ q a saddle At δ = 0, a saddle and center are created simultaneously

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Hamiltonian pitchfork bifurcation

Saddle ⇐ ⇒ Saddle-Center-Saddle (or Center ⇐ ⇒ Center-Saddle-Center)

µ = −1 µ = +1

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H = v2 2 − Φ(u) = v2 2 − u4 4 + µu2 2 ¨ u = u3 − µu ⇐ ⇒      ˙ u = v = ∂H ∂v ˙ v = u3 − µu = −∂H ∂u = ∂Φ ∂u