(441a) Modeling of CO2 Solubility in Electrolyte Solutions and Brines Using Statistical Associating Fluid Theory | AIChE

(441a) Modeling of CO2 Solubility in Electrolyte Solutions and Brines Using Statistical Associating Fluid Theory

Authors 

Jiang, H. - Presenter, Princeton University
Panagiotopoulos, A. Z., Princeton University
Economou, I. G., Texas A&M University at Qatar
Understanding the behavior of CO2, especially its solubility, in electrolyte solutions and brines is of great importance to the design of a CO2 geologic sequestration project. Since the properties of CO2 bearing electrolyte solutions are strongly affected by the long-rang Coulomb interactions of ions, an accurate description of ion-ion interactions is important to the modeling of CO2-H2O-electrolyte system. In this work, CO2 solubilities in single and mixed electrolyte solutions as well as synthetic geologic formation brines were correlated or predicted with statistical associating fluid theory (SAFT). [1, 2] In the proposed SAFT equation of state, the ion-ion interactions were represented by an improved mean spherical approximation in the primitive model using a parameter K to correct the excess energies (â??KMSAâ? for short). [3] The universal correction factor K was obtained by adjusting the internal and excess energies of mean spherical approximation to Monte Carlo simulation data. With the SAFT-KMSA model, we studied a range of aqueous electrolyte solutions including Na+, K+, Ca2+, Mg2+, Cl-, Br- and SO42- from 298.15 K to 473.15 K. The cross interactions for CO2-H2O and CO2-ion dispersion interactions were adjusted with binary interaction parameters kij, which were fitted to CO2 solubility data in water and single electrolyte solutions. Without additional parameters to fit, the proposed model was conveniently extended to predict CO2 solubilities in mixed electrolyte solutions, including NaCl+KCl, KCl+CaCl2, NaCl+KCl+CaCl2, and in synthetic geologic formation brines. The proposed model shows good predictive power for CO2 solubility in mixed electrolyte solutions and brines.

[1] Jiang, H.; Panagiotopoulos, A. Z.; Economou, I. G. Geochim. Cosmochim. Acta. 2016, 176, 185.

[2] Tan, S. P.; Ji, X.; Adidharma, H.; Radosz, M. J. Phys. Chem. B. 2006, 110, 16694.

[3] Jiang, H.; Adidharma, H. Mol. Simul. 2015, 41, 727.

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