An equation of state for accurate thermodynamic modeling of water and carbon dioxide from triple points to 647 K and 100-200 MPa

被引:8
作者
Du, Guoqiang [1 ,2 ,4 ]
Hu, Jiawen [2 ,3 ]
机构
[1] Hebei Univ Geosci, Sch Math & Sci, Shijiazhuang 050031, Hebei, Peoples R China
[2] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China
[3] Hebei Univ Geosci, Coll Resources, Shijiazhuang 050031, Hebei, Peoples R China
[4] Minist Land & Resources, Key Lab Gas Hydrate, Qingdao 266071, Shandong, Peoples R China
基金
中国国家自然科学基金;
关键词
Equation of state; Water; Carbon dioxide; Phase equilibrium; PVT properties; Density; Residual enthalpy; Residual entropy; Critical region; RENORMALIZATION-GROUP THEORY; GENERALIZED CROSSOVER DESCRIPTION; NEAR-CRITICAL CORRECTION; INTERFACIAL-TENSION; PVTX PROPERTIES; PURE FLUIDS; CO2; STORAGE; GEOLOGICAL SEQUESTRATION; TRANSPORT-PROPERTIES; PHASE-EQUILIBRIA;
D O I
10.1016/j.ijggc.2016.02.025
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
An equation of state with near-critical corrections is developed for water (H2O) and carbon dioxide (CO2). The equation is constrained by the critical conditions and optimized with highly accurate pressure-volume-temperature (PVT) and phase equilibrium data at temperatures from the triple point to 647.096 K and pressures from zero to 80 MPa. The resulting equation is systematically checked in the above P-T range. For H2O, the vapor pressures are reproduced within 0.032%, with an average deviation of only 0.005%; the average deviations of the saturated vapor and liquid volumes, and the volumes in the single-phase regions are 0.047%, 0.019% and 0.058%, respectively. The maximum deviations of the above mentioned volumes are 1.26%, 0.91% and 1.06%, respectively, which are all in the immediate vicinity of the critical point. Below 520 K, the deviations of PVT and saturation properties are all within 0.06%. For subcritical CO2, the average and maximum deviations of vapor pressures are 0.011%, 0.077%, respectively; the average deviations of the saturated vapor and liquid volumes, and the volumes in the single-phase regions are 0.099%, 0.058% and 0.126%, respectively. The largest deviations of the above volumes are 0.230%, 0.173% and 0.358%, respectively. For supercritical CO2 below 650 K, the average volume deviation is 0.080%. The equation also agrees very well with many high-quality density and phase equilibrium data not used to fit the equation. The equation gives excellent prediction of fugacity coefficients, residual enthalpies and entropies and heats of vaporization, and can be extrapolated to 200 MPa for H2O, or to 100 MPa for CO2. The equation can serve as a good starting point for the thermodynamic modeling of many industrial and geological processes, including carbon capture and sequestration. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:94 / 107
页数:14
相关论文
共 90 条
[1]   CO2/CaCl2 solution interfacial tensions under CO2 geological storage conditions: Influence of cation valence on interfacial tension [J].
Aggelopoulos, C. A. ;
Robin, M. ;
Perfetti, E. ;
Vizika, O. .
ADVANCES IN WATER RESOURCES, 2010, 33 (06) :691-697
[2]   Thermodynamic model of aqueous CO2-H2O-NaCl solutions from-22 to 100°C and from 0.1 to 100 MPa [J].
Akinfiev, Nikolay N. ;
Diamond, Larryn W. .
FLUID PHASE EQUILIBRIA, 2010, 295 (01) :104-124
[3]   Prediction of water-rock interaction and porosity evolution in a granitoid-hosted enhanced geothermal system, using constraints from the 5 km Basel-1 well [J].
Alt-Epping, P. ;
Diamond, L. W. ;
Haering, M. O. ;
Ladner, F. ;
Meier, D. B. .
APPLIED GEOCHEMISTRY, 2013, 38 :121-133
[4]  
Anisimov M.A., 2000, Equations of State for Fluids and Fluid Mixtures, V1, P381
[5]  
Atilhan M., 2007, HIGH ACCURACY P RHO, P1
[6]   Dependence of CO2-brine interfacial tension on aquifer pressure, temperature and water salinity [J].
Bachu, Stefan ;
Bennion, D. Brant .
GREENHOUSE GAS CONTROL TECHNOLOGIES 9, 2009, 1 (01) :3157-3164
[7]   Interfacial Tension between CO2, Freshwater, and Brine in the Range of Pressure from (2 to 27) MPa, Temperature from (20 to 125) °C, and Water Salinity from (0 to 334 000) mg.L-1 [J].
Bachu, Stefan ;
Bennion, D. Brant .
JOURNAL OF CHEMICAL AND ENGINEERING DATA, 2009, 54 (03) :765-775
[8]   Package FLUIDS. Part 3: correlations between equations of state, thermodynamics and fluid inclusions [J].
Bakker, R. J. .
GEOFLUIDS, 2009, 9 (01) :63-74
[9]   Improvements in clathrate modelling .1. The H2O-CO2 system with various salts [J].
Bakker, RJ ;
Dubessy, J ;
Cathelineau, M .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1996, 60 (10) :1657-1681
[10]   Package FLUIDS 1.: Computer programs for analysis of fluid inclusion data and for modelling bulk fluid properties [J].
Bakker, RJ .
CHEMICAL GEOLOGY, 2003, 194 (1-3) :3-23