updated June 4, 1997
GEOMETRY OF CHAOS
Spring quarter 1997
Physics D60-0: NU Graduate Chaos Course
Course schedule
Predrag Cvitanovic
Current schedule:
http://ChaosBook.org/~predrag/NUcourses/D60-0-sched97.html .
Lecture notes and problem sets: http://www.nbi.dk/ChaosBook/.
Problem with the problems is that numbers might differ from the lecture
notes you got off the web - simplest to go through problems with underlined
titles. I would like to receive solutions on Mondays.
Place and times:TTh 1:30 - 3:00 in Tech L386;
go up the main Tech building staircase to the third floor, turn left, go
past the Applied Math to the end of the large cross hallway; the classroom
is to your right across the hall.
Lecture 1 1:30
- 3:00 tuesday, April 1, 1997 in Tech L386
Preview
A brief historical introduction to the subject; Chapter 1 of
the Cyclist Treatise is recommended reading prior to the lecture, in order
to open up the discussion.
Lecture 2 1:30
- 3:00 thursday, April 3, 1997 in Tech L386
Dynamics, qualitative I
We start learning how to count: qualitative dynamics of simple
stretching and mixing flows is used to introduce symbolic dynamics and
Smale horseshoes.
Reading: chapter 2, sects. 2.1-2.2,
Problems: at least 1.1, 1.4, 1.5
Lecture 3 1:30
- 3:00 tuesday, April 8, 1997 in Tech L386
Dynamics, qualitative II
We continue learning how to count: qualitative dynamics of Smale
horseshoes is used to introduce pruning, finite subshifts, Markov Graphs
and transition matrices.
Reading: chapter 2, sects. 2.2-2.4,
Problems: at least 2.1, 2.2, 2.4, 2.6, 2.8
Lecture 4
1:30 - 3:00 thursday, April 10, 1997 in Tech L386
Dynamics, qualitative III
We finish learning how to count: the traces of powers of the
transition matrix count admissible cycles, and the largest eigenvalue of
the transition matrix yields the topological entropy. The secular determinant
of the transition matrix - the Artin-Mazur zeta function - is expressed
in terms of the loops of a Markov diagram.
By now we have covered for the first time the whole distance from diagnosing chaotic dynamcs to computing zeta functions. Historically, These topological zeta functions were the inspiration for injecting statistical mechanics into computation of dynamical averages; Ruelle's zeta functions are a weighted generalization of the counting zeta functions.
Lecture 5 1:30
- 3:00 tuesday, April 15, 1997 in Tech L386
Local dynamics, quantitative I
We review the basic concepts of local dynamics required to move
beyond mere counting in order to assign relative weights to topologically
distinct parts of the phase space. In this lecture we define flows and
maps, and discuss local properties of flows: linear stability, types of
eigenvalues for linear maps, stable/unstable manifolds, numerical methods.
Reading: Chapter 3
Lecture 6 1:30
- 3:00 thursday, April 17, 1997 in Tech L386
Local dynamics, quantitative II
We continue the discussion of local properties of flows and
maps: Henon map, Bunimovich-Sinai formula for linear stability in billiards.
Reading: Chapter 3
Problems:
1) Use your pinball program to numerically investigate the Poincare section;
strips of surviving initial conditions (exer. 3.6), phase space density
for closed system (exr. 3.7).
2) figure out how to compute stability of billiard trajectories, include
this in your numerical billiard dynamics program.
3) implement numerical integration (perhaps the Runge-Kutta of exer. 3.8)
for a continuos time dynamical system of your choice, plot some typical
trajectories.
Lecture 7 1:30
- 3:00 tuesday, April 22, 1997 in Tech L386
Fixed points, and what to do about them
In order to proceed, we shall need data about unstable periodic
orbits, so good numerical methods for their detemination are a necessity.
We shall start by determining periodic orbits of a unimodal map, and then
proceed to Newton-Raphson method for maps and Poincare maps of flows. Existence
of unit eigenvalues necessitates further cleverness.
Reading: Chapter 4
Problems:
1) use your pinball program to numerically determine a few shortest cycles,
presumably by implementing a minimization routine.
2) figure out how to compute stability of the shortest pinball cycles by
hand. Compare with your numerical billiard stability program.
3) start implementing numerical Poincare sections for a continuos time
dynamical system of your choice
4) start implementing a Newton-Raphson routine (only start - problems 3)
and 4) might take a week or two to get in running shape).
Lecture 8
1:30 - 3:00 thursday, April 24, 1997 in Tech L386
Dynamical averaging
In chaotic dynamics detailed prediction is impossible, as any
finitely specified initial condition, no matter how precise, will fill
out the entire accessible phase space (similarly finitely grained) in finite
time. Hence for chaotic dynamics one does not attempt to follow individual
trajectories to asymptotic times; what is possible (and sensible) is description
of the geometry of the set of possible outcomes, and evaluation of the
asymptotic time averages. Examples of such averages are transport coefficients
for chaotic dynamical flows, such as the escape rate, mean drift and the
diffusion rate; power spectra; and a host of mathematical constructs such
as the generalized dimensions, Lyapunov exponents and the Kolmogorov entropy.
We shall now set up the formalism for evaluating such averages within the
framework of the periodic orbit theory. The key idea is to replace the
expectation values of observables by the expectation values of generating
functionals. This associates an evolution operator with a given observable,
and leads to formulas for its dynamical averages.
Reading: chapter 6, sects. 6.1-6.2
Problems: at least 6.1, 6.2
Lecture 9 1:30
- 3:00 tuesday, April 29, 1997 in Tech L386
Evolution operators and their spectra
If there is one idea that you should learn about dynamics, it
happens in this lecture(s) and it is this: there is a fundamental local
- global duality which says that (global) eigenstates are dual to the (local)
periodic geodesics. For dynamics on the circle, this is called Fourier
analysis; for dynamics on well-tiled manifolds this is called Selberg trace
formulas and zeta functions; and for generic nonlinear dynamical systems
the duality is embodied in trace formulas, zeta functions and spectral
determinants that we will now introduce. These objects are to dynamics
what partition functions are to statistical mechanics. The bold claim is
that once you understand this, classical ergodicity, wave mechanics and
stochastic mechanics are but special cases, to be worked out at your leasure.
The strategy is this: Global averages such as escape rates can be extracted from the eigenvalues of evolution operators. The eigenvalues are given by the zeros of appropriate determinants. One way to evaluate determinants is to expand them in terms of traces, log det = tr log. The traces are evaluated as integrals over Dirac delta functions, and in this way the spectra of evolution operators become related to periodic orbits.
The rest of the course is making sense out of this objects and learning
how to apply them to evaluation of physically measurable properties of
chaotic dynamical systems.
Reading: chapter 6, sects. 6.3-6.5
Problems: at least 6.3, 6.6
Lecture 10 1:30
- 3:00 thursday, May 1, 1997 in Tech L386
Getting used to cycles
In last two lectures we have moved at rather brisk pace and
derived a spew of formulas. Just to make sure that the key message - the
``trace formulas'' and their ilk - have sunk in, in chapter ``Why cycle?''
we rederive them in a rather different, more intuitive way, and extol their
virtues. This is recommended bedtime reading, material that we will not
cover in today's lecture. Instead, we slow down to develop some fingertip
feeling for the objects evaluted so far; show that this is just a fancy
way to discretize integrals, evaluate the spectral determinant on a single
unstable fixed point, on a piecewise linear map, count eigenvalues, and
so on.
Reading: chapters 7 and 8
Problems: at least 8.1, 8.2, 8.3, 8.4
Lecture 11
1:30 - 3:00 tuesday, May 6, 1997 in Tech L386
Recycling
In last three lectures we have derived a plethora of periodic
orbit trace formulas, spectral determinants and zeta functions. Now we
learn how to expanded these as cycle expansions, series ordered by increasing
topological cycle length, and evaluate average quantites like escape rates.
These formulas are exact, and, when the winds are kind, highly convergent.
The pleasant surprise is that the terms in such expansions fall off exponentially
or even faster, so that a handful of shortest orbits suffices for rather
accurate estimates of asymptotic averages.
Reading: chapter 9, sects. 9.1-9.4,
Problems: at least 9.1,9.2, 9.5, 9.6
Lecture 12 1:30
- 3:00 thursday, May 8, 1997 in Tech L386
Applications of cycle expansions
Today we shall apply periodic orbit theory to evaluation of
Lyapunov exponents, entropies and dimensions.
Reading: the (old) chapter 9 is not worth printing out yet - too messy,
sorry
Problems: pause until I receive cycle expansion evaluations of escape rates
for either a 1-d map or the 3-disk billiard (old problem sets)
Lecture 13 1:30
- 3:00 tuesday, May 13, 1997 in Tech L386
Thermodynamic formalism
We continue discussing main applications of the periodic orbit
theory, this time in the guise of ``thermodynamic formalism''.
Reading: chapter 10, (previously numbered 9) is still a mess, not
worth printing out on paper yet.
Problems: evaluate the Lyapunov exponent by cycle expansion for any system
for which you have cycle data.
Lecture 14 1:30
- 3:00 thursday, May 15, 1997 in Tech L386
Quantum Mechanics I
We try to get from Schrödinger equation (January 1926)
via Madelung (October 1926) and Hamilton (1821) to the semiclassical propagator.
While the periodic orbit quantization trace formula cannot be honestly
derived from this in only one lecture, we will try to give you the feeling
for how it is derived in lecture 17.
Reading: chapter 11 (current homepage numbering), sects. 10.1-10.3
(as numerated in the current web version of the chapter)
Problems: at least 10.1, 10.2
Lecture 15 1:30
- 3:00 tuesday, May 20, 1997 in Tech L386
Carl Dettmann:
Statistical mechanics from deterministic chaos?
After the excursion into Lyapunov exponents, entropies, dimensions
and thermodynamical formalism, we are back to the meat of the subject;
can one derive statistical mechanics from deterministic chaos? We apply
the periodic orbit theory to evaluation of measurable properties of a very
simple model of ideal gas, periodic Lorentz gas, and derive closed-form
formulas for the diffusion constant.
Reading: current chapter 10, sects. 10.1, 10.2, 10.4,
Problems: at least 10.6, 10.9
Lecture 16 1:30
- 3:00 thursday, May 22, 1997 in Tech L386
Carl Dettmann:
Nonequilibrium statistical mechanics from deterministic
chaos?
Can one one go beyond equilibrium statistical mechanics and
derive properties of systems far from equilibrium by the methods discussed
in this course? This is currently a very lively research area, and we explain
how the periodic orbit theory yields transport properties in models of
dissipative driven systems, such as Guassian thermostatted Lorentz gas.
Lecture 17 1:30
- 3:00 tuesday, May 27, 1997 in Tech L386
Quantum Mechanics II
We continue the semiclassical quantization of chaotic mechanics
commenced in lecture 15. This seems to require an orgy of partial derivatives
which we shall try to avoid - the lecture will be essentailly a guided
tour to the Gutzwiller trace formula which is much simpler and more intuitive
than the derivation that leads to it; it has the same structure as the
classical trace formulas we are familiar with, except that now the cycle
weights are complex. Time permiting we shall sketch out how this is used
to quantize Helium.
Reading: browse chapters 11, 13
Problems: 2/3 of the registered students are way behind - we now concentrate
on the term paper projects
Lecture 18 1:30
- 3:00 thursday, May 29, 1997 in Tech L386
Why does it work? I
The heuristic manipulations that led to the trace formulas and
spectral determinants are potentially dangerous, as we are dealing with
infinite-dimensional vector spaces and singular integral kernels. Intuitively,
the theory should converge because long cycles are shadowed by nearby pseudo-cycles.
Actually, for clasess of not althogether too idealized smooth flows very
strong results exists.
Reading: chapter 15, sects. *.1, *.2 and *.3
Problems: we concentrate on the term paper projects
Lecture 19 1:30
- 3:00 tuesday, June 3, 1997 in Tech L386
Why does it work? II
For clasess of not althogether too idealized smooth flows very
strong results exists. We explain the ideas behind proofs of Ruelle and
Rugh which establish that for nice real analytic expanding or hyperbolic
flows the spectral (Fredholm) determinants are entire, and that at least
in that context the edifice constructed in this course has a mathematical
basis.
Reading: chapter 15, sects. *.1, *.2 and *.3
Problems: we concentrate on the term paper projects
Lecture 20 (the last of the course) 1:30
- 3:00 thursday, June 5, 1997 in Tech L386
What's wrong with this course?
A moment of truth; the theory we have learned this quarter
is beautiful, but it rests on romantic assumptions about dynamics that
most sytems of interest falil to live up to. The problems that we would
really like to tackle still mock us: they exhibit infinite symbolic dynamics,
intermittency, ``phase transitions'', cycle expansions that might not converge.
Other people have other visions of what ``quantum chaos'' might be, and
higher and infinite dimensional dynamical systems still elude us. Which
is the reason why this subject is so exciting - there is still so much
to do and understand.
Term
papers due
4:30 PM friday, June 13, 1997 - Predrag's office
return
to the Department of Physics & Astronomy.