New equation of state as international standard to describe thermodynamics of heavy water

Scilight ◽  
2018 ◽  
Vol 2018 (49) ◽  
pp. 490004
Author(s):  
Drew DeJarnette
Keyword(s):  
Equation Of State ◽  
Heavy Water ◽  
International Standard ◽  
New Equation

Algorithms for Density, Potential Temperature, Conservative Temperature, and the Freezing Temperature of Seawater

2006 ◽  
Vol 23 (12) ◽  
pp. 1709-1728 ◽  
Author(s):  
David R. Jackett ◽  
Trevor J. McDougall ◽  
Rainer Feistel ◽  
Daniel G. Wright ◽  
Stephen M. Griffies
Keyword(s):  
Thermal Expansion ◽  
Equation Of State ◽  
Thermodynamic Potential ◽  
Potential Temperature ◽  
Inverse Function ◽  
Freezing Temperature ◽  
Ocean Models ◽  
The Difference ◽  
New Equation ◽  
Density Equation

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.

A New Equation of State for Fluids

1928 ◽  
Vol 63 (5) ◽  
pp. 229 ◽  
Author(s):  
James A. Beattie ◽  
Oscar C. Bridgeman
Keyword(s):  
Equation Of State ◽  
New Equation

scholarly journals A NEW EQUATION OF STATE

1929 ◽  
Vol 15 (1) ◽  
pp. 11-18 ◽  
Author(s):  
H. J. Brennen
Keyword(s):  
Equation Of State ◽  
New Equation

A new equation of state for the Aral Sea water

Oceanology ◽  
2011 ◽  
Vol 51 (3) ◽  
pp. 367-369 ◽  
Author(s):  
I. Gertman ◽  
P. O. Zavialo
Keyword(s):  
Equation Of State ◽  
Sea Water ◽  
Aral Sea ◽  
New Equation

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
Keyword(s):  
Equation Of State ◽  
Critical Region ◽  
New Equation

A new equation of state for hard chain molecules

1994 ◽  
Vol 100 (9) ◽  
pp. 6633-6639 ◽  
Author(s):  
Dhananjay Ghonasgi ◽  
Walter G. Chapman
Keyword(s):  
Equation Of State ◽  
Chain Molecules ◽  
New Equation

Impact of the new equation of state of seawater (TEOS-10) on the estimates of water mass mixture and meridional transport in the Atlantic Ocean

2018 ◽  
Vol 162 ◽  
pp. 13-24 ◽  
Author(s):  
Lucas Almeida ◽  
José Luiz Lima de Azevedo ◽  
Rodrigo Kerr ◽  
Moacyr Araujo ◽  
Mauricio M. Mata
Keyword(s):  
Equation Of State ◽  
Atlantic Ocean ◽  
Water Mass ◽  
Meridional Transport ◽  
New Equation
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