Eg. Ponyatovsky et al., THE METASTABLE T-P PHASE-DIAGRAM AND ANOMALOUS THERMODYNAMIC PROPERTIES OF SUPERCOOLED WATER, The Journal of chemical physics, 109(6), 1998, pp. 2413-2422
The metastable T-P phase diagram and the anomalies of the thermodynami
c properties of supercooled water are calculated on the basis of a two
-level thermodynamic model. Water is considered as a mixture of two co
mponents which differ in atomic configurations and correspond to low-d
ensity amorphous (Ida) and high-density amorphous (hda) ice. The expre
ssion for the Gibbs potential of water is written in the form which is
analogous to that of usual regular binary solutions. But this model c
onsiders the concentration, c, of the components, as a pressure and te
mperature-dependent internal parameter. There are only four constants
in the expression for the Gibbs potential: the differences in the spec
ific volumes, entropies, and energies of the two components and the mi
xing energy of the components whose values are Delta V-0= -3.8 cm(3)/m
ol, Delta S-0=4.225J/mol, Delta E-0=1037J/mol, and U=3824J/mol, respec
tively. The lda-hda phase equilibrium line terminates at the critical
point, T-cr= 230 K and P-cr= 0.173 kbar, the second critical point in
the phase diagram of water. The anomalous thermal dependence of the sp
ecific volume, the heat expansion coefficient, and the specific heat o
f water calculated for the atmospheric pressure is in a good quantitat
ive agreement with the available experimental data. Thus anomalous pro
perties of supercooled water are well explained by the occurrence of t
he second critical point close to the atmospheric pressure. The absolu
te value of parameter c is not crucial for the thermal behavior of pro
perties, instead, the anomalies in water are due to the dependence on
pressure and temperature. The parameter c behavior is analyzed in vari
ous pressure and temperature ranges around the second critical point.
The thermal dependence of parameter c is very weak in the temperature
range of 290-350 K at atmospheric pressure. As a consequence, the ther
modynamic properties of water behave in this range like those of a nor
mal liquid though water stays a mixture of two components, Ida-like an
d hda-like, in an approximate proportion 2:3. (C) 1998 American Instit
ute of Physics.