GPA TP-14-1987 Energy Functions for Gaseous CO2-H2O Mixtures《气态二氧化碳和水混合物的能量函数》.pdf
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1、Energy Functions for Gaseous C02-H20 Mixtures Mukund R. Patel James C. Holste Kenneth R. Hall Philip T. Eubank Department of Chemical Engineering Texas A and for the infringement of any patent or the violation of any federal, state or municipal law or regula- tion arising from the use of, any inform
2、ation, apparatus, method or process disclosed in this report. i GPA TP-14 87 3824b99 0011449 bbL FOREWORD Thennophysical properties of the carbon dioxide/water system have long been important in geological studies. have been used for enhanced oil recovery in Texas and Oklahoma oil fields. Recently,
3、large amounts of carbon dioxide Much of this carbon dioxide is produced in Colorado and moved via pipeline to its final destination. The removal of water from carbon dioxide prior to pipelining to prevent the formation of a condensed phase at elevated pressures relies upon the properties shown in TP
4、-14. While the primary support for this research came from the National Science Foundation, the experimental techniques and calculational methods were developed under GPA Research Project #772, a similar study of wet natural gas systems. authors have expressed their appreciation to the GPA Enthalpy
5、Committee for its technical advice and support during the past 10 years. The OXY % Car B. Sutton, GPA Secretary ii GPA TP-14 87 3824677 OOL1450 383 1 ENERGY FUNCTIONS FOR GASEOUS CO2-H2O MIXTURES A tabulation of total energy properties derived from experimental data for mixtures of 2% 5%, lo%, 25%,
6、and 50% H20 in CO2 along with pressure- enthalpy diagrams for the same. Mukund R. Patel, James C. Holste, Kenneth R. Hall, and Philip T. Eubank Department of Chemical Engineering Texas A making an isochoric run (pressure measurements at fixed temperature increments); returning the cell to the origin
7、al condition; and performing an expansion of the sample into a previously evacauted secondary cell volume. A series of such isochoric runs coupled with isothermal expansions, typically at the highest temperature, constitute a B-I surface run. An important feature of the B-l method is that it generat
8、es an entire P-p-T surface with one filling of the sample; hence, for mixtures there is no need to duplicate a composition. Being the only two observables in the B-I experiment, the pressure and temperature are measured with exterme accuracy and precision. Pressure measurements are accurate to 0.01%
9、 and precise to 0.001%, whereas the temperatures are accurate to 10 mK with a precision of 5 mK or better. DATA REDUCTION TO ENERGY FUNCTIONS Analysis of the measured pressures and temperatures for a B-I surface run provides the densities and compressibilitics. However, for systems for which adsorpt
10、ion is diagnosed, corrections for adsorption contributions have to be made independently. GPA TP-14 87 3824699 0011452 i156 H 3 Such was the case for the present COi-HzO mixtures and the data were corrected as described in detail by Patel 114. Once these corrections have been made and the densities
11、and cornpressibilities determined, calculation of the thermodynamic properties is achieved through the use of residual properties. A residual property is defined as the real fluid property value less the perfect gas state property value. Of the various forms of such property changes discussed by Hal
12、l et al. Id, the one discussed here is the real fluid property at the temperature and density of the fluid less the perfect gas property at a reference temperature, Tref, and reference pressure, Pref. Thus, for a property M, the residual property is defined as where the * indicates the hypothetical
13、perfect gas state. integration is: The path chosen for With this formulation, it is most convenient to establish (U - U;,.) and (S - S,Cf), and then to calculate the other properties from these two. The starting equations are and dU=CvT+R - - (lfT),d,p (,“;T), - 1 $ dT T S=Cv-+R - - The residual int
14、ernal energy then is determined using and the residual entropy using (3) GPA TP-14 87 3824677 0011453 O92 4 Finally, the remaining residual properties are calculated from and u - “;er + z re ref = H - H* RT RT T A- A* U- UTef S-SI*, S* R ref = - RT RT R Any reference state may be specified, but for
15、a reference state for which H,“,f and Skf are chosen to equal zero, as is the case here, Gr*ef = O, U* ref = - RTref, and A;ef = - RT,ef. Note that the only integrals required to calculate all the above residual properties are and C; dT JTref R The first two require simple applications of the equati
16、on of state, while the latter two involve only perfect-gas specific heats. Eubank et al. IA show that density data obtained by the B-I method yield the above thermodynamic properties more accurately than do data from either straight Burnett or straight isochoric -measurements. RESULTS Tables 1 throu
17、gh 5 present the total energy properties for the five mixtures. The reference state chosen here is the perfect-gas-state reference of zero enthalpy and entropy at 273.16 K and 1kPa. The perfect-gas specific heats for pure COP were taken from Angus et al. 18 and those for pure H20 were taken from Haa
18、r et a/. 19. The GPA TP-LLi 87 3824699 0011454 T29 5 properties listed have the following estimated accuracies: densities and compressibility factors, 0.05%; internal energies and enthapies, 0.15%; Helmholtz and Gibbs free energies, 0.20%; and entropies, 0.17%. Finally, Figures 1 through 5 give the
19、respective pressure-enthalpy (P-H) diagrams developed from the experimental data. ACKNOWLEDGEMENTS The principal sponsor for this work was the National Science Foundation (Grant CPE 8023182). Additional financial support was provided by the Exxon Research and Engineering Company and by the Gas Proce
20、ssors Association. NOTATION A = Helmholtz free energy C, G = Gibbs free energy H = enthalpy M P = pressure R S = entropy T = absolute temperature U = internal energy Z P = density = specific heat capacity at constant volume = general variable for U, H, A, G, or S = universal gas constant (8.31448 J/
21、mol-K) = compressibility factor (P / pRT) Superscripts * = perfect gas state Su bscripts ref = reference state value 6 LITERATURE CITED 1. Weibe, R., and V. L. Gaddy, “The Solubility in Water of Carbon Dioxide at 50, 75 and 100aCc, at Pressures to 700 Atmospheres“, J. Amer. Chem. Soc., 61, 315 (1939
22、). 2. Weibe, R., and V. L. Gaddy, “The Solubility of Carbon Dioxide in Water at Various Temperatures from 12 to 40” and at Pressures to 500 Atmospheres. Critical Phenomena”, J. Amer. Chem. Soc., 62, 815 (1940). 3. Weibe, R., and V. L. Gaddy, “Vapor Phase Composition of Carbon Dioxide-Water Mixtures
23、at Various Temperatures and at Pressures to 700 Atmospheres”, J. Amer. Chem. Soc, 63, 475 (1941). 4. Houghton, G., A. M, McLean, P. D. Ritchie, “Compressibility, fugacity, and water solubility of carbon dioxide in the region 0-36 atm. and O-100C“, Chem. Eng. Sci., 6, 132 (1957). 5. Coan, C. R., and
24、A. D. King, “Solubility of Water in Compressed Carbon Dioxide, Nitrous Oxide, and Ethane. Evidence for Hydration of Carbon Dioxide and Nitrous Oxide in the Gas Phase”, J. Amer. Chem. Soc., 93, 1857 (1971). 6. Zawisza, A., and B. Malesihska, “Solubility of Carbon Dioxide in Liquid Water and of Water
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