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Phase Coexistence and Phase Changes in Clusters

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Title: Phase Coexistence and Phase Changes in Clusters


1
Phase Coexistence and Phase Changes in Clusters
  • By
  • Joseph H. Noroski
  • April 17, 2003

2
Two Common Phases
  • Solid Particles exist in well-defined sites,
    oscillating around their equilibrium positions in
    small amplitude motions. The potential well is
    deep and steep, yielding a low density of states.
  • Liquid Particles exhibit diffusive motion with
    large mean square displacements, have soft
    vibrational modes, and can permute (exchange
    positions) among themselves. The potential wells
    are less deep and steep, yielding a high density
    of states.

3
The Bulk World
  • The freezing point (Tf) and the melting point
    (Tm) are identical for a bulk sample a typical
    first order transition.
  • Phase equilibria can be described entirely by
    macroscopic thermodynamic variables and, as such,
    are STATIC equilibria.

4
The Cluster World
  • The freezing and melting points are not the same.
    There exists an equilibrium between phases over
    a range of T.
  • Phase equilibria must be considered in dynamic
    terms that is, consider ENSEMBLES of clusters.
  • The individual clusters freely pass from one
    phase to another.

5
Other Types of Phases in Clusters
  • Surface-melted solid core, liquid surface, and a
    few floaters above the surface The surface
    becomes liquid-like when about 1 atom in 30
    floats above.
  • Soft solid clusters can pass between a limited
    number of solid-like potential minima with
    relatively large amplitude motions no permuting
    of identical atoms among non-equivalent sites
  • Slush short duration of various phase-like forms

6
Examining Clusters
  • The majority of cluster research is done via
    computer simulation. The experimental
    difficulties, of course, result from synthesizing
    something with 10 1000 atoms in a reproducible
    way.
  • Probe atoms inserted into the clusters possess
    different spectra in one phase or another. These
    spectra are used to identify different phases.

7
Solid-Liquid Equilibrium in Clusters
  • There is only one minimum in the potential well
    below Tf and only one minimum above Tm.
  • For clusters there exists a RANGE of T (at a
    single pressure) for which the equilibrium (s) ?
    (l) exists. So, Keq liq/sol
    exp(-?F/kBT). ?F is the free energy difference
    in the minima for the solid and liquid.

8
Conditions for Coexistence
  • S-bends in the probability distributions of, for
    example, the canonical ensemble, P(E), or the
    grand canonical ensemble, P(N).
  • For example, an S-bend in the microcanonical
    caloric curve results when ln P(E) for the
    corresponding canonical distribution has two
    inflections.

9
A Triple Point is Now a Triple Range????
  • The Gibbs Phase rule says that three phases of
    one component can exist at only one T, the
    so-called triple point, T3.
  • Simulations show that surface-melted clusters can
    coexist with solid and liquid clusters over a
    range of T.
  • For clusters each phase is as much a component as
    it is a phase.
  • The Gibbs Phase rule has no meaning for ensembles
    of small systems.

10
More on Solid/Liquid/Surface-Melted Equilibrium
  • The grand canonical partition function is of the
    form Zc(mc)Zs(ms)Zf(mf)Zint(mc, ms, mf). c
    core s surface f floater int
    interaction. mxs are defects. For example, ms
    are floater-vacancy pairs.
  • Conditions for coexistence (?ln Zc/?mc)T 0 and
    (?ln ZsZf /?mf)T 0.
  • Number of analytical solutions indicates the
    number of phases present.
  • New types of phase diagrams are needed.

11
A Model for Phase Changes
  • Vekhter and Berry used simulations to examine
    Ar55 and (KCl)32 clusters.
  • Over a T range of 730-760 K two phases observed
    for KCl crystal-like and liquid-like. Over a T
    range near 40 K three phases observed for Ar55
    solid, liquid, and surface-melted.
  • The third phase of Ar55 is due to a third peak in
    the density of states not present for (KCl)32.

12
A Model for Phase Changes (cont.)
  • We can explain (KCl)32 by a two-level model with
    a nondegenerate ground state (where the solid
    is) and an N1-fold degenerate excited state
    (where the amorphous liquid states are). The
    difference in energy is d.
  • The population of the excited level is n1(T)
    N1exp(-d/kT)/1 N1exp(-d/kT). It is key to
    note that, as N1 grows, the solid to liquid
    transition temperature range gets smaller.

13
A Model for Phase Changes (cont.)
  • Ar55 requires an intermediate energy level, dsm.
  • s solid m surface-melted l liquid
  • Two consecutive transitions, (s) to (m), followed
    by (m) to (l), occur if Tsl Tsm, where kBTsm
    dsm/ln(Nsm) and kBTsl (d1 - dsm) /ln(N1/Nsm).
  • If Tsm Tsl, no surface-melted phase seen.
  • If Tsm Tsl, 3 phase coexistence is seen.

14
Other efforts with clusters
  • Nigra, et. al. have used parallel tempering Monte
    Carlo and multihistogram methods to study phase
    changes of (H2O)8.
  • There is a sharp Tm at 178.5 K.
  • However, a solid to solid phase change is found
    at 12 K. Here, the (H2O)8 clusters change
    symmetry from strictly D2d to a mixture of D2d
    and S4.
  • Others cluster research involves efforts to store
    data in condensed form using small clusters.

15
References
  • R. S. Berry, in Large Clusters of Atoms and
    Molecules, edited by T.P. Martin (Kluwer,
    Dordrecht, 1996), p. 281.
  • R. S. Berry, in Scientific American, (August,
    1990), p. 68.
  • P. Nigra, M. A. Carignano, and S. Kais, J. Chem.
    Phys. 115, 2621 (2001).
  • Benjamin Vekhter and R. S. Berry, J. Chem. Phys.,
    106, 6456 (1997).
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