Empirical formulae are presented for calculating vapor-liquid equilibria (VLE) in the CO 2 -H 2 O system at 10 temperatures between 110 and 350 °C. At each temperature, separate functions are used to represent the bubble- and dew-point boundary curves that: originate at the saturation vapor pressure of water (P sat; H₂O ) at X CO₂ = 0; diverge with increasing pressure up to ~P(X max CO₂ ) where ∂P/∂X CO₂ = +∞ along the dew-point curve; then converge with increasing pressure above P(X max CO₂ ). At temperatures below 265 °C and pressures > P(X max CO₂ ), the compositions of coexisting liquid and vapor [X CO₂ L(V) and X CO₂ V(L) ] do not converge completely with increasing pressure due to the absence of critical behavior. Thus, relatively simple functions suffice to accurately represent VLE at those temperatures. In contrast, at T > 265 °C, X CO₂ L(V) and X CO₂ L(V) converge rapidly as P approaches P c (the critical pressure in the CO 2 -H 2 O system at a given temperature between 265 and 374 °C and P ≤ 215 MPa). For those temperatures, therefore, more complex VLE formulae are required to achieve close representation of phase relations. For dew-point equations, this includes adding an exponential “correction term” to ensure that ∂P/∂X CO₂ = 0 at the critical points indicated by corresponding bubble-point functions. Stable liquid-vapor coexistence in mixed-volatile systems requires ƒ L i = ƒ V I (isofugacity conditions) for all “i” (volatile components) in the two fluid phases. Thus, the equations presented in this paper specify numerous P-T-X conditions where ƒ L H₂O = ƒ V H₂O and ƒ L CO₂ = ƒ V CO₂ in the CO 2 -H 2 O system. These results have important applications in the ongoing effort to develop a more rigorous thermodynamic model for CO 2 -H 2 O fluids at geologically relevant temperatures and pressures.
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