Ag. Kalinichev et K. Heinzinger, MOLECULAR-DYNAMICS OF SUPERCRITICAL WATER - A COMPUTER-SIMULATION OF VIBRATIONAL-SPECTRA WITH THE FLEXIBLE BJH POTENTIAL, Geochimica et cosmochimica acta, 59(4), 1995, pp. 641-650
Molecular dynamics (MD) computer simulations have been performed for a
system of 200 water molecules interacting by means of the Bopp-Jancso
-Heinzinger (BJH) intermolecular interaction potential under supercrit
ical conditions (630 < T < 770 K, or similar to 350-500 degrees C) ove
r a very wide range of densities (0.17 < rho < 1.28 g/cm(3)) and press
ures (0.25 < P < 30 kbar). The results are compared with available exp
erimental data and simulations using other water models. The flexibili
ty of the BJH water model made it possible to analyze the temperature
and density dependencies of the intramolecular geometry and vibrationa
l frequencies of water molecules along with the information on thermod
ynamic, structural, and kinetic properties of water, usually calculate
d from MD simulations. With temperature and density (pressure) increas
e, the average intramolecular O-H distance also increases, while the a
verage intramolecular H-O-H angle decreases. Both effects increase the
average dipole moment of a water molecule, which changes from 1.99 to
2.05 Debye at 400 degrees C and 0.1666 g/cm(3) and 0.9718 g/cm(3), re
spectively. The spectra of intramolecular vibrations are calculated as
Fourier transforms of the velocity autocorrelation functions of hydro
gen atoms. The frequencies of both symmetric and asymmetric stretching
vibrations increase with temperature and decrease with density (press
ure), while the frequency of the H-O-H bending vibrations remains almo
st constant over the wide range of thermodynamic conditions studied. T
hese findings are in good agreement with available IR and Raman spectr
oscopic measurements and allow us to expect the BJH potential to be ab
le to predict changes in the vibrational behavior of water molecules i
n response to changes of thermodynamic parameters covering the entire
range of temperatures, densities, and compositions characteristic of h
ydrothermal systems.