Supercritical CO2 and CH4 uptake by illite-smectite clay minerals
File(s) Manuscript.pdf (471.1 KB)
Accepted version
Author(s)
Hwang, Junyoung
Pini, Ronny
Type
Journal Article
Abstract
Clay minerals abound in sedimentary formations and the interaction of reservoir gases with their sub-micron features has direct relevance to many geo-energy applications. The quantification of gas uptake over a broad range of pressures is key towards assessing the significance of these physical interactions on enhancing storage capacity and gas recovery. We report a systematic investigation of the sorption properties of three source clay minerals – Na-rich montmorillonite (SWy-2), illite-smectite mixed layer (ISCz-1), and illite (IMt-2) – using CO2 and CH4 up to 30 MPa at 25 to 115 °C. The textural characterization of the clays by gas physisorption indicates that micropores are only partly accessible to N2 (77 K) and Ar (87 K), while larger uptakes are measured with CO2 (273 K) in the presence of illite. The supercritical excess sorption experiments confirm these findings, while revealing differences in uptake capacities that originate from the clay-specific pore size distribution. The Lattice Density Functional Theory (LDFT) model describes accurately the measured sorption isotherms by using a distribution of properly weighted slit pores and clay-specific solid-fluid interaction energies, which agree with isosteric heats of adsorption obtained experimentally. The model indicates that the maximum degree of pore occupancy is universal to the three clays and the two gases, and it depends solely on temperature, reaching values near unity at the critical temperature. These observations greatly support the model's predictive capability for estimating gas adsorption on clay-bearing rocks and sediments.
Date Issued
2019-10-01
Date Acceptance
2019-09-03
Citation
Environmental Science & Technology, 2019, 53 (19), pp.11588-11596
ISSN
0013-936X
Publisher
American Chemical Society (ACS)
Start Page
11588
End Page
11596
Journal / Book Title
Environmental Science & Technology
Volume
53
Issue
19
Copyright Statement
© 2019 American Chemical Society. This document is the Accepted Manuscript version of a Published Work that appeared in final form in Environmental Science & Technology, after peer review and technical editing by the publisher. To access the final edited and published work see https://doi.org/10.1021/acs.est.9b03638
Sponsor
Commission of the European Communities
Identifier
https://pubs.acs.org/doi/10.1021/acs.est.9b03638
Grant Number
764810
Subjects
Environmental Sciences
Publication Status
Published
Article Number
acs.est.9b03638
Date Publish Online
2019-09-03
