UCL Discovery
UCL home » Library Services » Electronic resources » UCL Discovery

Methane transport through hierarchical silica micro-mesoporous materials: From non-equilibrium atomistic simulations to phenomenological correlations

Phan, A; Striolo, A; (2019) Methane transport through hierarchical silica micro-mesoporous materials: From non-equilibrium atomistic simulations to phenomenological correlations. Microporous and Mesoporous Materials , 288 , Article 109559. 10.1016/j.micromeso.2019.06.021. Green open access

[thumbnail of 1-s2.0-S1387181119304020-main.pdf]
Preview
Text
1-s2.0-S1387181119304020-main.pdf - Accepted Version

Download (5MB) | Preview

Abstract

Atomistic non-equilibrium molecular dynamics simulations were employed to quantify methane transport in hierarchical porous networks. Model amorphous silica materials were used as solid substrates, which allows us to construct pore networks with well-defined properties. The results show that the methane diffusivity and permeability through the pores strongly depend on the frameworks. Analysis of the vector fields for methane within the pores reveals the existence of local back-flow near the solid substrates, which disturbs methane transport. Varying the pore cross-sectional areas leads to changes in the entropy potential along the flow direction, which influences the molecular path length. The results show a linear relationship between methane transport (i.e., permeability) and a pore characteristic parameter that takes into consideration porosity, constriction factor, and tortuosity. This relation holds for hierarchical porous materials containing both micropores and mesopores. Diffusivity and permeability of methane through porous media are found to scale as a power function of porosity and constriction factor. These are measurable descriptors, suggesting that transport properties could be predicted for engineering and natural materials once characterisation data are available. For example, we show here that a power law can describe results obtained for Fontainebleau sandstone. The good agreement achieved suggests that using the approach presented not only enables the quantification of molecular effects influencing fluid transport, but also yields the reliable prediction of diffusivity and permeability of fluids through sedimentary rocks using as sole input macroscopic pore structure information.

Type: Article
Title: Methane transport through hierarchical silica micro-mesoporous materials: From non-equilibrium atomistic simulations to phenomenological correlations
Open access status: An open access version is available from UCL Discovery
DOI: 10.1016/j.micromeso.2019.06.021
Publisher version: https://doi.org/10.1016/j.micromeso.2019.06.021
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
Keywords: Molecular simulations, Amorphous silica, Transport diffusivity, Permeability, Tortuosity
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Engineering Science
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Engineering Science > Dept of Chemical Engineering
URI: https://discovery.ucl.ac.uk/id/eprint/10076887
Downloads since deposit
Loading...
67Downloads
Download activity - last month
Loading...
Download activity - last 12 months
Loading...
Downloads by country - last 12 months
Loading...

Archive Staff Only

View Item View Item