unit 1
C-O-H-S FLUID COMPOSITION AN OXYGEN FUGACITY IN GRAPHITIC METAPELITES
C-O-H-S fluid produced by the equilibration of water and excess graphite must mantain the atomic H/O ratio of water 2:1. This constract implies that all thermodynamic properties of the fluid are uniquely determined by isobaruc-isothermal conditions. By mathematical models fugacities of oxygen ,water and carbon dioxide.
[10] unit 2
OSMOTIC AND MEAN ACTIVITY COEFFICIENTS OF UNI-UNIVALENTS ELECTROLYTES IN WATER @25ºC
This paper studies uni-univalent aqueous solutions by 2 diffenter methods: osmotic coefficient and activity coefficient.
These values were obatained or calculated considerating thermodynmaic properties. They were also representated in therms of: standard deviation, variance, normalized standard deviation, in order to express these quantities as function of electrolyte concentartions. [9] unit 3
Application of the Cell Potential Method To Predict Phase Equilibria of Multicomponent Gas Hydrate SystemsThis paper presents the application of a mathematical and statistical model with the unknown function being the intermolecular potential between the molecules (guest and host).
[8] Calculation of multicomponent chemical equilibria in gas-solid-liquid systems: Calculation methods, thermochemical data, and applications to studies of high-temperature volcanic gases with examples from Mt. St. Helens
This paper documents the numerical formulations, thermochemical, and possible applications of computer programs, for calculating multicomponent chemical equilibria in gas-solid-liquid systems. [7] |
2015. Ana Botello, Jessica Moctezuma, Lenia Sánchez, Mariana Muñoz, María José Morales
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