Bm. Law, SURFACE AMPLITUDE RATIOS AND NUCLEATED WETTING NEAR A CRITICAL END-POINT, Berichte der Bunsengesellschaft fur Physikalische Chemie, 98(3), 1994, pp. 472-477
Citations number
42
Categorie Soggetti
Chemistry Physical
Journal title
Berichte der Bunsengesellschaft fur Physikalische Chemie
We examine two recently discovered phenomena which occur at the liquid
/vapor surface of a critical binary liquid mixture; namely, (i) the un
iversality of the critical adsorption amplitude ratio and (ii) the obs
ervation of the nucleation of wetting droplets after a temperature que
nch from the one phase into the two phase region. The recent theoretic
al work of Fisher and Upton on the universality of the surface tension
amplitude ratio suggests that the ratio of the critical adsorption am
plitude above and below T(c) should also be universal. This is indeed
found to be the case for five critical liquid mixtures where the modif
ied critical adsorption amplitude ratio has an experimental value of R
(MA) = 1.18 +/- 0.13. This result agrees reasonable well with the RG c
alculations of Diehl and Smock. In the two-phase region, for sufficien
tly small reduced temperatures t, the critical liquid mixture hexadeca
ne + acetone has an acetone-rich wetting layer at the liquid/vapor sur
face at equilibrium. We examine the time development of this wetting l
ayer after a temperature quench from the one phase into the two phase
region. The liquid/vapor surface initially drops into a metastable sur
face state which is well described by critical adsorption. The lifetim
e ,tau0, of this metastable state is many hours and depends upon the r
educed temperature, t. At the nucleation time tau0 acetone-rich drople
ts nucleate and grow at the liquid/vapor surface; good agreement is fo
und for tau0 between theory and experiment for t greater-than-or-equal
-to 8 x 10(-5). An essential ingredient of the theory is the inclusion
of a line tension term in the free energy of the nucleated droplet. A
t large times tau the droplets coalesce into a metastable wetting film
which eventually undergoes a hydrodynamic instability to an equilibri
um wetting film.