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2009 J. Phys.: Condens. Matter 21 474220 (11pp) doi: 10.1088/0953-8984/21/47/474220
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Abstract.
We investigate the intermediate-and longest-range decay of the total pair correlation function
h(r)
in model fluids where the inter-particle potential decays as
−r−6, as is appropriate to real fluids in which dispersion forces govern the attraction
between particles. It is well-known that such interactions give rise to a term in
q3
in the expansion of
, the Fourier transform of the direct correlation function. Here we show that the presence of the
r−6
tail changes significantly the analytic structure of
from that found in models where the inter-particle potential is short ranged. In particular the pure imaginary
pole at q = iα0, which generates monotonic-exponential decay of
rh(r)
in the short-ranged case, is replaced by a complex (pseudo-exponential) pole at
q = iα0+α1 whose
real part α1
is negative and generally very small in magnitude. Near the critical point
α1~−α02
and we show how classical Ornstein–Zernike behaviour of the pair correlation function is
recovered on approaching the mean-field critical point. Explicit calculations, based on the
random phase approximation, enable us to demonstrate the accuracy of asymptotic formulae for
h(r)
in all regions of the phase diagram and to determine a pseudo-Fisher–Widom
(pFW) line. On the high density side of this line, intermediate-range decay of
rh(r)
is exponentially damped-oscillatory and the ultimate long-range decay is power-law, proportional
to r−6, whereas on the low density side this damped-oscillatory decay is sub-dominant to both
monotonic-exponential and power-law decay. Earlier analyses did not identify the
pseudo-exponential pole and therefore the existence of the pFW line. Our results enable us
to write down the generic wetting potential for a 'real' fluid exhibiting both short-ranged
and dispersion interactions. The monotonic-exponential decay of correlations associated
with the pseudo-exponential pole introduces additional terms into the wetting
potential that are important in determining the existence and order of wetting
transitions.
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