4.7 Article

Insights from molecular dynamics on CO2 diffusion coefficient in saline water over a wide range of temperatures, pressures, and salinity: CO2 geological storage implications

Journal

JOURNAL OF MOLECULAR LIQUIDS
Volume 345, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.molliq.2021.117868

Keywords

Diffusion Coefficient; Underground CO2 Storage; Saline Aquifers; Molecular Dynamics Simulation

Funding

  1. Nazarbayev University
  2. Faculty Development Competitive Research Grants Program [110119FD4529]

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This research utilized Molecular Dynamics simulation to calculate the CO2 diffusion coefficient under various NaCl saline water concentrations, temperatures, and pressures. Higher NaCl concentrations were found to lead to a decrease in CO2 diffusion coefficient, and a new precise correlation was proposed for estimation. The presence of other salts such as CaCl2 and KCl had varying effects on the CO2 diffusion coefficient, with CaCl2 having the highest impact and KCl having the lowest.
Successful design and execution of CO2 sequestration in saline aquifers requires a comprehensive understanding of CO2 transport properties. CO2 diffusion coefficient affects CO2 dissolution behavior in water/brine and controls phenomena such as shape of viscous fingers and onset of instabilities. Experimental determination of CO2 diffusion coefficient is a technically and economically challenging task. In this research work, we used Molecular Dynamics (MD) simulation to compute CO2 diffusion coefficient in various NaCl saline water concentrations (1-6 mol NaCl/kg water) under a broad range of temperatures (294-423 K) and pressures (10-30 MPa) to acquire a data set for CO2 diffusion coefficient in different conditions. According to the results, NaCl concentration increase gives rise to a decrease in CO2 diffusion coefficient by 15%, 29%, 49%, and 64% at 1 M, 2 M, 4 M, and 6 M solutions, respectively, compared to pure water. Presence of more cations due to salinity increase forms further hydration shells act as a barrier for CO2 diffusion. In addition, the rise in CO2 diffusion at elevated temperatures can be explained by the cation's hydration shell size reduction with temperature increment due to intensifying repulsive forces among water molecules. We proposed a new precise correlation for estimation of CO2 diffusion coefficients over temperatures and salinity ranges of this study. Regarding the pressure variation effects, no tangible changes were observed with pressure increase, validating a negligible influence on diffusion coefficient. Furthermore, the CO2 diffusion coefficient variability in presence of other salts, namely MgCl2, CaCl2, KCl, and Na2SO4, were computed separately. Comparing the influence of various salts, CaCl2 and KCl have the highest and lowest effect on the CO2 diffusion coefficient, respectively. Finally, a set of direct numerical simulations were conducted to study the impact of CO2 diffusion coefficient on CO2 dissolution process. The results obtained from this research work shed light on the importance of CO2 diffusion coefficient changes in saline water for prediction of dissolution process behavior. (C) 2021 Elsevier B.V. All rights reserved.

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