Sorption-Induced Permeability Evolution and Chemo-Mechanical Interactions of CO2 Sequestration in the Marcellus Shale

Abstract Recognizing the limitations of conventional reservoirs, we were inspired to investigate the underexplored potential of organic-rich shales for secure geological storage. This began with the puzzling observation that permeability in the Marcellus Shale, under CO2 injection, declined in two distinct stages: an unexpected behavior inconsistent with simple Darcy flow. To unravel this, we designed a multi-pronged investigation to probe both pore-scale dynamics and molecular-level interactions driving this phenomenon. We first applied pulse-decay coreflooding under triaxial confinement, comparing the behavior of helium, methane, and CO2. This revealed that CO2 uniquely exhibited an initial sharp reduction in permeability (adsorption-driven), followed by further constriction due to matrix reorganization; a behavior absent in helium flooding and subdued in methane flooding. To understand the role of pore structure and surface properties, we conducted BET and BJH analyses, which revealed a slit-like mesoporous and microporous network optimal for CO2 adsorption. Rivetted by the irreversible nature of these changes, we employed Raman spectroscopy to monitor the evolution of kerogen structure. Post-injection spectra showed increased aromatic ordering and subtle molecular reorganization, corroborating our hypothesis that CO2 not only occupies pores but also chemically interacts with the matrix. This comprehensive approach revealed a sorption–chemo-mechanical mechanism: CO2 is first adsorbed onto abundant micropores and kerogen, then induces subtle matrix restructuring and pore throat constriction, locking itself in place. These findings provide a predictive framework that links dynamic flow behavior, mineral–organic interactions, and structural evolution, demonstrating the Marcellus Shale's capacity as both an adsorptive sink and a structurally responsive sequestration medium. This work advances our understanding of how molecular-scale processes manifest in macroscopic storage security.

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Publication Details

Journal
SPE Annual Technical Conference and Exhibition
Published
2025-10-13
DOI
https://doi.org/10.2118/228837-stu
Primary Topic
Hydrocarbon exploration and reservoir analysis
Type
article
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article

Sorption-Induced Permeability Evolution and Chemo-Mechanical Interactions of CO2 Sequestration in the Marcellus Shale

Ilham El‐Monier, P. H. Sampson Eduam
SPE Annual Technical Conference and Exhibition
Hydrocarbon exploration and reservoir analysis
article

Sorption-Induced Permeability Evolution and Chemo-Mechanical Interactions of CO2 Sequestration in the Marcellus Shale

Ilham El‐Monier, P. H. Sampson Eduam
article en

Abstract

Abstract Recognizing the limitations of conventional reservoirs, we were inspired to investigate the underexplored potential of organic-rich shales for secure geological storage. This began with the puzzling observation that permeability in the Marcellus Shale, under CO2 injection, declined in two distinct stages: an unexpected behavior inconsistent with simple Darcy flow. To unravel this, we designed a multi-pronged investigation to probe both pore-scale dynamics and molecular-level interactions driving this phenomenon. We first applied pulse-decay coreflooding under triaxial confinement, comparing the behavior of helium, methane, and CO2. This revealed that CO2 uniquely exhibited an initial sharp reduction in permeability (adsorption-driven), followed by further constriction due to matrix reorganization; a behavior absent in helium flooding and subdued in methane flooding. To understand the role of pore structure and surface properties, we conducted BET and BJH analyses, which revealed a slit-like mesoporous and microporous network optimal for CO2 adsorption. Rivetted by the irreversible nature of these changes, we employed Raman spectroscopy to monitor the evolution of kerogen structure. Post-injection spectra showed increased aromatic ordering and subtle molecular reorganization, corroborating our hypothesis that CO2 not only occupies pores but also chemically interacts with the matrix. This comprehensive approach revealed a sorption–chemo-mechanical mechanism: CO2 is first adsorbed onto abundant micropores and kerogen, then induces subtle matrix restructuring and pore throat constriction, locking itself in place. These findings provide a predictive framework that links dynamic flow behavior, mineral–organic interactions, and structural evolution, demonstrating the Marcellus Shale's capacity as both an adsorptive sink and a structurally responsive sequestration medium. This work advances our understanding of how molecular-scale processes manifest in macroscopic storage security.

SPE Annual Technical Conference and Exhibition
The Ohio State University (US)
Openalex Percentile: Top 47%
Hydrocarbon exploration and reservoir analysis
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