EGU26-2355, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-2355
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 07 May, 08:30–10:15 (CEST), Display time Thursday, 07 May, 08:30–12:30
 
Hall X4, X4.80
Study of the macromolecular structure of kerogen for CO2/H2 and CH4/H2 competitive adsorption capacity: 3D molecular reconstruction, spectroscopic experiments, molecular simulations
Zhikai Liang1,2,3 and Guangyou Zhu1,2
Zhikai Liang and Guangyou Zhu
  • 1Hubei Key Laboratory of Complex Shale Oil and Gas Geology and Development in Southern China, Wuhan, China
  • 2School of Geoscience, Yangtze University, Wuhan, China
  • 3Department of Chemical & Petroleum Engineering, Khalifa University of Science and Technology, Abu Dhabi, United Arab Emirates

The nanopores in organic matter (OM) in shale are considered to be the main storage space for methane. However, there is still limited understanding of the role of OM in underground hydrogen storage(UHS) in retaining shale gas reservoirs. To investigate the influence of kerogen on hydrogen storage, this study employs multiple spectroscopic techniques (solid-state 13C nuclear magnetic resonance, Fourier transform infrared spectroscopy, and X-ray photoelectron spectroscopy) to establish macromolecular structure models of kerogens of high and over-mature stages. Using molecular simulation techniques (GCMC and MD methods), the adsorption characteristics of hydrogen on kerogen under conditions of 333.15 K-393.15 K and 0-30 MPa are studied. The result shows: Longmaxi kerogen is carbon-dominant (>80%), featuring an extensive aromatic framework in over-mature stages. The high content of protonated and branched aromatic carbon, alongside a well-developed graphite (002) crystal plane, confirms high graphite-like crystallinity in over-mature structures. CH4/H2 competitive adsorption is primarily governed by van der Waals forces. CH4 molecule exhibits stronger surface affinity, preferentially occupying high-energy sites with densities exceeding twice the bulk phase. Conversely, H2 interactions are extremely weak, primarily controlled by pore space confinement and thermodynamic conditions, leading to a bulk-phase distribution. CH4/H2 selectivity decreases with pressure. The limited impact of maturity on selectivity reflects the stability of the dispersion-dominated mechanism. CO2 molecule exhibits strong electrostatic and inductive interactions with polar functional groups. This leads to markedly higher isosteric heats and selectivity compared to the CH4 system. The CO2 molecule exhibits strong electrostatic and inductive interactions with polar groups and aromatic structures, showing significantly higher isosteric heat and selectivity coefficients compared to the CH4/H2 system. The CO2 molecule has the lowest diffusion coefficient due to stable adsorption configurations and long residence times. At high pressures, a pore confinement effect restricts the H2 molecule mean free path, increasing collision resistance and reducing its effective diffusion rate. These findings provide critical theoretical support for assessing the safety and capacity of large-scale UHS in depleted shale gas reservoirs.

How to cite: Liang, Z. and Zhu, G.: Study of the macromolecular structure of kerogen for CO2/H2 and CH4/H2 competitive adsorption capacity: 3D molecular reconstruction, spectroscopic experiments, molecular simulations, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-2355, https://doi.org/10.5194/egusphere-egu26-2355, 2026.