scholarly journals New Equation of State for Water and Steam in the Critical Region

1968 ◽  
Vol 34 (259) ◽  
pp. 501-516 ◽  
Author(s):  
Koichi WATANABE ◽  
Ichimatsu TANISHITA ◽  
Hiroyasu OZAWA
1968 ◽  
Vol 11 (48) ◽  
pp. 1145-1160 ◽  
Author(s):  
Koichi WATANABE ◽  
Hiroyasu OZAWA ◽  
Ichimatsu TANISHITA

1964 ◽  
Vol 86 (3) ◽  
pp. 320-326 ◽  
Author(s):  
E. S. Nowak

A parametric equation of state was derived for water and water vapor in the critical region from experimental P-V-T data. It is valid in that part of the critical region encompassed by pressures from 3000 to 4000 psia, specific volumes from 0.0400 to 0.1100 ft3/lb, and temperatures from 698 to 752 deg F. The equation of state satisfies all of the known conditions at the critical point. It also satisfies the conditions along certain of the boundaries which probably separate “supercritical liquid” from “supercritical vapor.” The equation of state, though quite simple in form, is probably superior to any equation heretofore derived for water and water vapor in the critical region. Specifically, the deviations between the measured and computed values of pressure in the large majority of the cases were within three parts in one thousand. This coincides approximately with the overall uncertainty in P-V-T measurements. In view of these factors, the author recommends that the equation be used to derive values for such thermodynamic properties as specific heat at constant pressure, enthalpy, and entropy in the critical region.


2006 ◽  
Vol 23 (12) ◽  
pp. 1709-1728 ◽  
Author(s):  
David R. Jackett ◽  
Trevor J. McDougall ◽  
Rainer Feistel ◽  
Daniel G. Wright ◽  
Stephen M. Griffies

Abstract Algorithms are presented for density, potential temperature, conservative temperature, and the freezing temperature of seawater. The algorithms for potential temperature and density (in terms of potential temperature) are updates to routines recently published by McDougall et al., while the algorithms involving conservative temperature and the freezing temperatures of seawater are new. The McDougall et al. algorithms were based on the thermodynamic potential of Feistel and Hagen; the algorithms in this study are all based on the “new extended Gibbs thermodynamic potential of seawater” of Feistel. The algorithm for the computation of density in terms of salinity, pressure, and conservative temperature produces errors in density and in the corresponding thermal expansion coefficient of the same order as errors for the density equation using potential temperature, both being twice as accurate as the International Equation of State when compared with Feistel’s new equation of state. An inverse function relating potential temperature to conservative temperature is also provided. The difference between practical salinity and absolute salinity is discussed, and it is shown that the present practice of essentially ignoring the difference between these two different salinities is unlikely to cause significant errors in ocean models.


1928 ◽  
Vol 63 (5) ◽  
pp. 229 ◽  
Author(s):  
James A. Beattie ◽  
Oscar C. Bridgeman

1929 ◽  
Vol 15 (1) ◽  
pp. 11-18 ◽  
Author(s):  
H. J. Brennen

1991 ◽  
Vol 95 (8) ◽  
pp. 3351-3357 ◽  
Author(s):  
Arturo G. Aizpiri ◽  
Antonio Rey ◽  
Jorge Davila ◽  
Ramon G. Rubio ◽  
John A. Zollweg ◽  
...  

1995 ◽  
pp. 358-364
Author(s):  
J. M. H. Levelt Sengers ◽  
W. L. Greer ◽  
J. V. Sengers

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