Topographies, Dynamics and Kinetics on the Landscape of Multidimensional Potential Surfaces PowerPoint PPT Presentation

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Title: Topographies, Dynamics and Kinetics on the Landscape of Multidimensional Potential Surfaces


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Topographies, Dynamics and Kinetics on the
Landscape of Multidimensional Potential Surfaces
  • R. Stephen Berry
  • The University of Chicago
  • Global Optimiization Theory Institute
  • Argonne National Laboratory
  • 8-10 September 2003

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An Overview
  • First, identify the issues and the problems What
    are the important, challenging problems from the
    perspective of the physicist or chemist? What
    steps have we made toward elucidating them? What
    tools have we used?
  • Then, what lies ahead What kinds of known
    problems have resisted explication? What new
    directions might we explore?

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What are obvious, big problems?
  • Dealing with incredibly complex landscapes with
    all sorts of topographies
  • Deciding what information is useful (Wayne Booth
    What information is worth having?)
  • Connecting topographies with kinetics and
    dynamics how can we infer about these from
    knowledge of topography?

4
What are some of the steps weve made toward
elucidating these?
  • Inventing efficient algorithms for finding
    stationary points, even in many dimensions
  • Inventing ways to identify sequences of
    geometrically-linked stationary points
  • Inventing patterns of topographies by using
    disconnection diagrams
  • Learning how to construct reliable master
    equations

5
Some more steps accomplished
  • Devising ways to simplify multidimensional
    surfaces, such as smoothing bumps and
    characterizing gross structure (Scheraga)
  • Finding ways to extract key variables, e.g.
    principal components principal coordinates
  • Linking dynamics with character of
    topography--but just qualitatively, so far

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First example Ar19Samples of its monotonic
sequences
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Ar19 has a sawtooth topography!
  • This makes it a glass-former quenched from
    liquid, it becomes amorphous
  • The topography is a consequence of short-range
    interparticle forces
  • Hence few particles move when the cluster passes
    from one local minimum to the next

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Ah, but then theres (KCl)32!A very different
beast
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(KCl)32 is a structure-seeker with a staircase
topography!
  • (KCl)32 finds a rocksalt structure when quenched
    from liquid in more than ca. 5 vibrations,
    against naïve odds of 1/1011
  • Characterized by long-range or effective
    long-range interparticle forces
  • Many particles move in most well-to-well passages

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What about proteins? Shouldnt they be
structure-seekers?
  • Look first at the topography of a protein model,
    a 46-bead object developed by Skolnick and then
    Thirumalai, a system that forms a b-barrel
    efficiently
  • The long-range character of its forces comes from
    the constraint of retaining the integrity of the
    polymer chain

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So whats its topography?
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Not a bad staircase at all, but...
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This model system, like the alkali halide
cluster, has lots of deep basins, very much alike
  • The pathways down into one look about the same as
    those in all of the others
  • Puzzle In a real protein, what makes the native
    structure so special? How does the topography
    lead the system there?

14
Push that question furtherCould there be more
than onethere?
  • Do we know whether native structures are really
    unique? NO! Active sites may well have unique
    structures, but we dont know whether variability
    may occur in the outer scaffolding. There is
    some evidence that it may, but nothing definite.
  • Experimental tests might be possible.

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What is the evidence for uniqueness?
  • First and foremost, crystal structures.
  • But crystals are selective, and may only admit
    molecules with the same structure as those
    already there.
  • Moreover crystallographers are also selective.
    Who wants to take an X-ray picture of a crystal
    that doesnt give clean, bright, interpretable
    spots?

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Return to what is established we can sometimes
infer topographiesfrom kinetics
  • Forward and backward rates, and microscopic
    reversibility, allow us to infer barrier heights,
    for effective potential landscapes as well as for
    real and explicitly simulated ones.

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Example Bovine Pancreatic Trypsin Inhibitor
(BPTI)(Fernández, Kostov, RSB)
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The effective potential, found by a kind of Monte
Carlo search procedure with folding and
unfolding, is indeed staircase-like
  • So lets generalize
  • Structure-seekers, vs.
  • Glass-formers

19
Now what are some problems that have resisted
explication?
  • Simply classifying and quantifying the kinds of
    complexity of surfaces (but the classification of
    disconnection diagrams is a significant step in
    this direction)
  • From this, determining the gross basin structure
    (again, the kind of disconnection diagrams tells
    much)

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Here are disconnection diagrams for LJ13 and
LJ19, two examples of palm trees (Wales)
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And a pathological case, LJ38
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Why pathological? One close-packed structure,
the deepest,in a sea of icosahedra
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More open problems
  • How can we construct efficient, reliable
    simplified representations of kinetics, e.g. from
    simplified master equations?
  • How can we determine the reliability of a method
    of simplification, e.g. a statistically-based
    master equation, or a principal component
    representation or some combination of these?

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Still more and more...
  • How can we coarse-grain mechanical
    representations in ways that give reliable
    results for long-time processes, such as those
    taking milliseconds?
  • How can we integrate coarse-grained and
    finer-grained approaches?
  • How can we characterize the variety and
    multiplicity of folding or relaxation paths?

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And then,
  • What should our priorities be now, and
  • How should we set them? How should we balance
    whats important, with whats possible?

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Connect topography with dynamics Ar55 simulated
_at_15, 20, 25 K
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Likewise, (KCl)32 _at_ 350, 550 and 600 K High T gt
fast, deep
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