Thermodynamic properties of sea salt solutions

AIChE Journal ◽  
1974 ◽  
Vol 20 (2) ◽  
pp. 326-335 ◽  
Author(s):  
Leroy A. Bromley ◽  
Daljit Singh ◽  
Parthasarathi Ray ◽  
Srinivasan Sridhar ◽  
Stanley M. Read
Keyword(s):  
Thermodynamic Properties ◽  
Sea Salt ◽  
Salt Solutions

Thermodynamic properties of sea salt solutions

1967 ◽  
Vol 12 (1) ◽  
pp. 101-104 ◽  
Author(s):  
Raymond W. Stoughton ◽  
Milton H. Lietzke
Keyword(s):  
Thermodynamic Properties ◽  
Sea Salt ◽  
Salt Solutions

A new model for predicting thermodynamic properties of sea salt solutions

Desalination ◽  
1985 ◽  
Vol 56 ◽  
pp. 299-313 ◽  
Author(s):  
V. Brandani ◽  
G. Del Re ◽  
G. Di Giacomo
Keyword(s):  
Thermodynamic Properties ◽  
Sea Salt ◽  
Salt Solutions ◽  
New Model

Vapor pressure of sea-salt solutions

1954 ◽  
Vol 35 (5) ◽  
pp. 722 ◽  
Author(s):  
A. B. Arons ◽  
C. F. Kientzler
Keyword(s):  
Vapor Pressure ◽  
Sea Salt ◽  
Salt Solutions

scholarly journals A global algorithm for estimating Absolute Salinity

Ocean Science ◽  
2012 ◽  
Vol 8 (6) ◽  
pp. 1123-1134 ◽  
Author(s):  
T. J. McDougall ◽  
D. R. Jackett ◽  
F. J. Millero ◽  
R. Pawlowicz ◽  
P. M. Barker
Keyword(s):  
Thermodynamic Properties ◽  
North Atlantic ◽  
World Ocean ◽  
Practical Method ◽  
Sea Salt ◽  
The North ◽  
Salinity Anomaly ◽  
The World ◽  
Standard Composition ◽  
The Absolute

Abstract. The International Thermodynamic Equation of Seawater – 2010 has defined the thermodynamic properties of seawater in terms of a new salinity variable, Absolute Salinity, which takes into account the spatial variation of the composition of seawater. Absolute Salinity more accurately reflects the effects of the dissolved material in seawater on the thermodynamic properties (particularly density) than does Practical Salinity. When a seawater sample has standard composition (i.e. the ratios of the constituents of sea salt are the same as those of surface water of the North Atlantic), Practical Salinity can be used to accurately evaluate the thermodynamic properties of seawater. When seawater is not of standard composition, Practical Salinity alone is not sufficient and the Absolute Salinity Anomaly needs to be estimated; this anomaly is as large as 0.025 g kg−1 in the northernmost North Pacific. Here we provide an algorithm for estimating Absolute Salinity Anomaly for any location (x, y, p) in the world ocean. To develop this algorithm, we used the Absolute Salinity Anomaly that is found by comparing the density calculated from Practical Salinity to the density measured in the laboratory. These estimates of Absolute Salinity Anomaly however are limited to the number of available observations (namely 811). In order to provide a practical method that can be used at any location in the world ocean, we take advantage of approximate relationships between Absolute Salinity Anomaly and silicate concentrations (which are available globally).

Heat capacities and enthalpies of sea salt solutions to 200.deg.

1970 ◽  
Vol 15 (2) ◽  
pp. 246-253 ◽  
Author(s):  
Leroy A. Bromley ◽  
Anthony E. Diamond ◽  
Emilio Salami ◽  
David G. Wilkins
Keyword(s):  
Heat Capacities ◽  
Sea Salt ◽  
Salt Solutions
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