TY - JOUR
T1 - Simulations of the structure and thermodynamic properties of water at high pressures and temperatures
AU - Brodholt, John
AU - Wood, Bernard
PY - 1993
Y1 - 1993
N2 - Precise pressure-volume-temperature (PVT) data for water
exist to pressures of only 8.9 kbar and temperatures of 900°C. Since aqueous
fluids are important in many processes at much higher pressures and
temperatures, there is a need to develop reliable extrapolations of the low
pressures experimental data. In this paper we present the results of molecular
dynamics simulations of water properties over a wide P-T range. It has been
shown that at a density of 1.0 g/cm3, the TIP4P intermolecular
potential (Jorgensen et al., 1983) very accurately reproduces the available
thermodynamic and structural properties of water at pressures of 1 bar to 10
kbar (Brodholt and Wood, 1990). This is extended here by testing TIP4P at
temperatures to 2500 K and 350 kbar. The PVT predictions are compared to the
experimental data of Bumham et al. (1969) at low pressures, and with the data
of Kormer (1968) and Bridgman (1942) at higher pressures. We conclude that
there is good reason to be confident of the predictive powers of the TIP4P
intermolecular potential in the high-pressure and high-temperature regime. Heat
capacities and structural properties have also been calculated and compared to
available data. High-pressure simulations have also been made with two other
intermolecular potentials which accurately represent water properties at low
pressures, SPC/E (Berendsen et al., 1987) and WK (Watanabe and Klein, 1989).
SPC/E predicts PVT properties that are similar to those of TIP4P, while WK is
accurate only at densities of about 1.0 g/cm3. At high pressures the
spherical potential of Belonoshko and Saxena (1991) predicts volumes that are
within 0.5 m of those predicted by TIP4P. A modified Redlich Kwong (MRK) type
equation of state based on the molecular dynamics simulations is presented
which can be used at pressures in excess of 10 kbar. This is used to predict
the location of the brucite dehydration reaction which has recently been
determined to 120 kbar (Johnson et al., 1991).
AB - Precise pressure-volume-temperature (PVT) data for water
exist to pressures of only 8.9 kbar and temperatures of 900°C. Since aqueous
fluids are important in many processes at much higher pressures and
temperatures, there is a need to develop reliable extrapolations of the low
pressures experimental data. In this paper we present the results of molecular
dynamics simulations of water properties over a wide P-T range. It has been
shown that at a density of 1.0 g/cm3, the TIP4P intermolecular
potential (Jorgensen et al., 1983) very accurately reproduces the available
thermodynamic and structural properties of water at pressures of 1 bar to 10
kbar (Brodholt and Wood, 1990). This is extended here by testing TIP4P at
temperatures to 2500 K and 350 kbar. The PVT predictions are compared to the
experimental data of Bumham et al. (1969) at low pressures, and with the data
of Kormer (1968) and Bridgman (1942) at higher pressures. We conclude that
there is good reason to be confident of the predictive powers of the TIP4P
intermolecular potential in the high-pressure and high-temperature regime. Heat
capacities and structural properties have also been calculated and compared to
available data. High-pressure simulations have also been made with two other
intermolecular potentials which accurately represent water properties at low
pressures, SPC/E (Berendsen et al., 1987) and WK (Watanabe and Klein, 1989).
SPC/E predicts PVT properties that are similar to those of TIP4P, while WK is
accurate only at densities of about 1.0 g/cm3. At high pressures the
spherical potential of Belonoshko and Saxena (1991) predicts volumes that are
within 0.5 m of those predicted by TIP4P. A modified Redlich Kwong (MRK) type
equation of state based on the molecular dynamics simulations is presented
which can be used at pressures in excess of 10 kbar. This is used to predict
the location of the brucite dehydration reaction which has recently been
determined to 120 kbar (Johnson et al., 1991).
UR - http://www.scopus.com/inward/record.url?scp=0027387933&partnerID=8YFLogxK
U2 - 10.1029/92JB01407
DO - 10.1029/92JB01407
M3 - Article
AN - SCOPUS:0027387933
VL - 98
SP - 519
EP - 536
JO - Journal of Geophysical Research
JF - Journal of Geophysical Research
SN - 0148-0227
IS - B1
ER -