49 research outputs found
Phase transitions of fluids in heterogeneous pores
We study phase behaviour of a model fluid confined between two unlike
parallel walls in the presence of long range (dispersion) forces. Predictions
obtained from macroscopic (geometric) and mesoscopic arguments are compared
with numerical solutions of a non-local density functional theory. Two
capillary models are considered. For a capillary comprising of two
(differently) adsorbing walls we show that simple geometric arguments lead to
the generalized Kelvin equation locating capillary condensation very
accurately, provided both walls are only partially wet. If at least one of the
walls is in complete wetting regime, the Kelvin equation should be modified by
capturing the effect of thick wetting films by including Derjaguin's
correction. Within the second model, we consider a capillary formed of two
competing walls, so that one tends to be wet and the other dry. In this case,
an interface localized-delocalized transition occurs at bulk two-phase
coexistence and a temperature depending on the pore width . A
mean-field analysis shows that for walls exhibiting first-order wetting
transition at a temperature , , where the spinodal
temperature can be associated with the prewetting critical point, which
also determines a critical pore width below which the interface
localized-delocalized transition does not occur. If the walls exhibit critical
wetting, the transition is shifted below and for a model with the
binding potential , where is
the location of the liquid-gas interface, the transition can be characterized
by a dimensionless parameter , so that the fluid configuration
with delocalized interface is stable in the interval between and
.Comment: 18 pages, 12 figure
Bridging transitions for spheres and cylinders
We study bridging transitions between spherically and cylindrically shaped
particles (colloids) of radius separated by a distance that are
dissolved in a bulk fluid (solvent). Using macroscopics, microscopic density
functional theory and finite-size scaling theory we study the location and
order of the bridging transition and also the stability of the liquid bridges
which determines spinodal lines. The location of the bridging transitions is
similar for cylinders and spheres, so that for example, at bulk coexistence the
distance at which a transition between bridged and unbridged
configurations occurs, is proportional to the colloid radius . However all
other aspects, and, in particular, the stability of liquid bridges, are very
different in the two systems. Thus, for cylinders the bridging transition is
typically strongly first-order, while for spheres it may be first-order,
critical or rounded as determined by a critical radius . The influence of
thick wetting films and fluctuation effects beyond mean-field are also
discussed in depth
Filling transitions in acute and open wedges
We present numerical studies of first-order and continuous filling
transitions, in wedges of arbitrary opening angle , using a microscopic
fundamental measure density functional model with short-ranged fluid-fluid
forces and long-ranged wall-fluid forces. In this system the wetting transition
characteristic of the planar wall-fluid interface is always first-order
regardless of the strength of the wall-fluid potential . In the
wedge geometry however the order of the filling transition depends not only on
but also the opening angle . In particular we show that
even if the wetting transition is strongly first-order the filling transition
is continuous for sufficient acute wedges. We show further that the change in
the order of the transition occurs via a tricritical point as opposed to a
critical-end point. These results extend previous effective Hamiltonian
predictions which were limited only to shallow wedges
Crossover scaling of apparent first-order wetting in two dimensional systems with short-ranged forces
Recent analyses of wetting in the semi-infinite two dimensional Ising model,
extended to include both a surface coupling enhancement and a surface field,
have shown that the wetting transition may be effectively first-order and that
surprisingly the surface susceptibility develops a divergence described by an
anomalous exponent with value . We reproduce
these results using an interfacial Hamiltonian model making connection with
previous studies of two dimensional wetting and show that they follow from the
simple crossover scaling of the singular contribution to the surface
free-energy which describes the change from apparent first-order to continuous
(critical) wetting due to interfacial tunnelling. The crossover scaling
functions are calculated explicitly within both the strong-fluctuation and
intermediate-fluctuation regimes and determine uniquely and more generally the
value of which is non-universal for the latter regime.
The location and the rounding of a line of pseudo pre-wetting transitions
occurring above the wetting temperature and off bulk coexistence, together with
the crossover scaling of the parallel correlation length, is also discussed in
detail
The Influence of Intermolecular Forces at Critical Point Wedge Filling
We use microscopic density functional theory to study filling transitions in
systems with long-ranged wall-fluid and short-ranged fluid-fluid forces
occurring in a right-angle wedge. By changing the strength of the wall-fluid
interaction we can induce both wetting and filling transitions over a wide
range of temperatures and study the order of these transitions. At low
temperatures we find that both wetting and filling transitions are first-order
in keeping with predictions of simple local effective Hamiltonian models.
However close to the bulk critical point the filling transition is observed to
be continuous even though the wetting transition remains first-order and the
wetting binding potential still exhibits a small activation barrier. The
critical singularities for adsorption for the continuous filling transitions
depend on whether retarded or non-retarded wall-fluid forces are present and
are in excellent agreement with predictions of effective Hamiltonian theory
even though the change in the order of the transition was not anticipated