4.7 Article

Diffusion of fluids confined in carbonate minerals: A molecular dynamics simulation study for carbon dioxide and methane-ethane mixture within calcite

期刊

FUEL
卷 325, 期 -, 页码 -

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.fuel.2022.124800

关键词

Confined systems; Self-diffusion tensor; Calcite mesopores; Natural gas; CO2

资金

  1. Sao Paulo Research Foundation (FAPESP), Brazil [2018/02713-8]
  2. CNPq (Brazilian National Council for Scientific and Technological Development)
  3. (Brazilian National Council for Scientific and Technological Development) [2013/08293-7]
  4. Center for Computing in Engineering and Science at Unicamp, Brazil (FAPESP) [12S-0209-190064]
  5. High Performance Computing Center of Texas A&M University at Qatar
  6. Human Resources Program of Brazilian National Agency of Petroleum, Natural Gas and Biofuels-PRH-ANP
  7. Qatar National Research Fund [2013/08293-7]

向作者/读者索取更多资源

The ability to calculate the diffusion of different compounds within mesoporous structures is crucial for various applications in the oil and gas industry. Molecular Dynamics simulations provide an excellent alternative to experimental determination for fluids in mesopores. A study on fluids confined within calcite walls revealed the anisotropy among the diffusion tensor components at different directions and the influence of confinement on density distribution, even at the center of small mesopores.
The ability to calculate how different compounds diffuse within mesoporous structures is paramount for a number of applications in the oil & gas sector, from oil exploration to separation, and even for the design of Carbon Capture, Utilization, and Storage (CCUS) processes. Molecular Dynamics simulations entail an excellent alternative to cases for which an experimental determination is unfeasible or extremely difficult, as it happens for fluids in mesopores. Nonetheless, being confined within a mineral mesopore makes the fluid spatial distribution inhomogeneous, requiring appropriate methods to compute the diffusion coefficients. Recently, some of us presented a new method for this purpose (Franco et al. 2016). In this work, we present a detailed study on how to apply such a method exploring fluids confined within calcite walls, which is a mineral representative of carbonate rocks found in several geological formations. From our results, we were able to map the evolution of the self-diffusion tensor components throughout the pore, showing the anisotropy among the components at different directions. We also show the influence of confinement and observe a significant effect at the center of the pore for small mesopores (< 7.5 nm), where the density distribution is constant. This is an unexpected result that shows how the confinement effect is manifested even at the so-called bulk-likeregion at the center of the pore.

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