TY - JOUR
T1 - Self-diffusion coefficients of the binary (H2O + CO2) mixture at high temperatures and pressures
AU - Moultos, Othonas A.
AU - Tsimpanogiannis, Ioannis N.
AU - Panagiotopoulos, Athanassios Z.
AU - Economou, Ioannis G.
N1 - Funding Information:
This publication was made possible thanks to an NPRP award [NPRP 6-1157-2-471] from the Qatar National Research Fund (a member of The Qatar Foundation). The statements made herein are solely the responsibility of the authors. We are grateful to the High Performance Computing Center of Texas A&M University at Qatar for a generous resource allocation. INT is thankful to Texas A&M University at Qatar for a visiting research position.
Publisher Copyright:
© 2015 Elsevier Ltd. All rights reserved.
Copyright:
Copyright 2015 Elsevier B.V., All rights reserved.
PY - 2016/2/1
Y1 - 2016/2/1
N2 - An extensive study of the self-diffusion coefficients in the (H2O + CO2) mixture was carried out using atomistic molecular dynamics simulations. The conditions studied cover a wide range of temperatures (323.15 K ≤ T ≤ 1023.15 K) and pressures (200 MPa ≤ P ≤ 1000 MPa), of interest for geological and carbon sequestration applications. A combination of simple but accurate point charge force fields was employed, specifically the TIP4P/2005 for H2O and EPM2 for CO2. The simulations were found to be in good agreement with available experimental data at these high temperature and pressure conditions, but extend at conditions for which experiments have not been previously reported. The results were correlated with a generalized form of the Speedy-Angel (1976) relationship. The new phenomenological correlation is a function of pressure and temperature and is shown to reproduce all values to excellent accuracy. Thus, it can be used reliably for engineering calculations.
AB - An extensive study of the self-diffusion coefficients in the (H2O + CO2) mixture was carried out using atomistic molecular dynamics simulations. The conditions studied cover a wide range of temperatures (323.15 K ≤ T ≤ 1023.15 K) and pressures (200 MPa ≤ P ≤ 1000 MPa), of interest for geological and carbon sequestration applications. A combination of simple but accurate point charge force fields was employed, specifically the TIP4P/2005 for H2O and EPM2 for CO2. The simulations were found to be in good agreement with available experimental data at these high temperature and pressure conditions, but extend at conditions for which experiments have not been previously reported. The results were correlated with a generalized form of the Speedy-Angel (1976) relationship. The new phenomenological correlation is a function of pressure and temperature and is shown to reproduce all values to excellent accuracy. Thus, it can be used reliably for engineering calculations.
KW - Carbon dioxide
KW - Correlation
KW - Diffusion coefficient
KW - Geological applications
KW - Molecular dynamics
KW - Water
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U2 - 10.1016/j.jct.2015.04.007
DO - 10.1016/j.jct.2015.04.007
M3 - Article
AN - SCOPUS:84947130251
SN - 0021-9614
VL - 93
SP - 424
EP - 429
JO - Journal of Chemical Thermodynamics
JF - Journal of Chemical Thermodynamics
ER -