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Influence of organic molecules on wetting characteristics of mica/H 2 /brine systems: Implications for hydrogen structural trapping capacities.
- Source :
-
Journal of colloid and interface science [J Colloid Interface Sci] 2022 Feb 15; Vol. 608 (Pt 2), pp. 1739-1749. Date of Electronic Publication: 2021 Oct 18. - Publication Year :
- 2022
-
Abstract
- Hypothesis: Actualization of the hydrogen (H <subscript>2</subscript> ) economy and decarbonization goals can be achieved with feasible large-scale H <subscript>2</subscript> geo-storage. Geological formations are heterogeneous, and their wetting characteristics play a crucial role in the presence of H <subscript>2</subscript> , which controls the pore-scale distribution of the fluids and sealing capacities of caprocks. Organic acids are readily available in geo-storage formations in minute quantities, but they highly tend to increase the hydrophobicity of storage formations. However, there is a paucity of data on the effects of organic acid concentrations and types on the H <subscript>2</subscript> -wettability of caprock-representative minerals and their attendant structural trapping capacities.<br />Experiment: Geological formations contain organic acids in minute concentrations, with the alkyl chain length ranging from C <subscript>4</subscript> to C <subscript>26</subscript> . To fully understand the wetting characteristics of H <subscript>2</subscript> in a natural geological picture, we aged mica mineral surfaces as a representative of the caprock in varying concentrations of organic molecules (with varying numbers of carbon atoms, lignoceric acid C <subscript>24</subscript> , lauric acid C <subscript>12</subscript> , and hexanoic acid C <subscript>6</subscript> ) for 7 days. To comprehend the wettability of the mica/H <subscript>2</subscript> /brine system, we employed a contact-angle procedure similar to that in natural geo-storage environments (25, 15, and 0.1 MPa and 323 K).<br />Findings: At the highest investigated pressure (25 MPa) and the highest concentration of lignoceric acid (10 <superscript>-2</superscript> mol/L), the mica surface became completely H <subscript>2</subscript> wet with advancing (θ <subscript>a</subscript> = 106.2°) and receding (θ <subscript>r</subscript> =97.3°) contact angles. The order of increasing θ <subscript>a</subscript> and θ <subscript>r</subscript> with increasing organic acid contaminations is as follows: lignoceric acid > lauric acid > hexanoic acid. The results suggest that H <subscript>2</subscript> gas leakage through the caprock is possible in the presence of organic acids at higher physio-thermal conditions. The influence of organic contamination inherent at realistic geo-storage conditions should be considered to avoid the overprediction of structural trapping capacities and H <subscript>2</subscript> containment security.<br />Competing Interests: Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2021 The Authors. Published by Elsevier Inc. All rights reserved.)
- Subjects :
- Aluminum Silicates
Salts
Wettability
Hydrogen
Subjects
Details
- Language :
- English
- ISSN :
- 1095-7103
- Volume :
- 608
- Issue :
- Pt 2
- Database :
- MEDLINE
- Journal :
- Journal of colloid and interface science
- Publication Type :
- Academic Journal
- Accession number :
- 34742087
- Full Text :
- https://doi.org/10.1016/j.jcis.2021.10.080