Fluid inclusion analyses leave little doubt that solutions containing large concentrations of H
2 O, CO 2, and electrolytes are involved in a wide range of geologic processes. Although the …

Fluid inclusion analyses reported in the literature, together with experimental data and
thermodynamic calculations indicate that nonideality in the system H2O-CO2-NaCl may …

The equation of state developed by Bowers and Helgeson ([Bowers, TS, Helgeson, HC,
1983. Calculation of the thermodynamic and geochemical consequences of nonideal mixing …

Phase equilibria in the ternary systems H 2 O–CO 2–NaCl and H 2 O–CO 2–CaCl 2 have
been determined from the study of synthetic fluid inclusions in quartz at 500 and 800° C, 0.5 …

Understanding the role of fluids in geologic processes requires a knowledge of the PVT
properties of fluids over a wide range of conditions. Comparisons of several published …

The compositional limits of fluid immiscibility in the system NaCl H 2 O CO 2 were
investigated from 500° to 700° C at pressures of 1, 2 and 3 kbar. Synthetic fluid inclusions …

Realistic simulations of fluid flow in geologic systems have severely been hampered by the
lack of a consistent formulation for fluid properties for binary salt–water fluids over the …

An equation of state (EOS) has been developed for the NaCl H2O CO2 system which
consistently predicts various properties including PVTX, immiscibility or phase equilibria …

Fluids containing substantial amounts of CO2 and NaC1 in addition to H20 are common in
hydrothermal environments in the earth's crust. Interpretation of the characteristics of fluid …

The ternary system H2O-NaCl-CO2 is one of the most important fluid systems in
geochemistry and petrology. However, there is little information on the phase equilibrium …