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Published on: October 21, 2016
Structural Properties of Kerogens with Different Maturities
Wei-Shan Chiang1,2,3, Jin-Hong Chen1, David Jacobi1
1Aramco Services Company: Aramco Research Center-Houston, Texas, USA.
The study reveals that as kerogen matures, its pore network and surface area increase, enhancing gas storage. This research utilized advanced techniques to analyze kerogen structure and composition for better resource recovery.
Area of Science:
- Geochemistry
- Petroleum Geology
- Materials Science
Background:
- Kerogen maturation creates pore networks crucial for hydrocarbon storage and recovery in source rocks.
- Understanding nanoscale pore structure, surface properties, and connectivity is vital but challenging.
Purpose of the Study:
- To investigate the pore structure, surface heterogeneity, and composition of kerogens at varying thermogenic maturities.
- To establish relationships between chemical composition, pore characteristics, surface properties, and maturity.
Main Methods:
- Prompt gamma-ray activation analysis (PGAA) for elemental composition.
- Nitrogen and methane gas sorption for pore volume and surface area analysis.
- Small-angle neutron scattering (SANS) and an extended generalized Porod's scattering law method (GPSLM) for pore structure and surface heterogeneity.
Main Results:
- Higher maturity kerogens exhibit lower hydrogen/carbon ratios and increased pore volume and accessible surface area.
- Methane sorption indicates a transition from heterogeneous to homogeneous binding sites with increasing maturity.
- SANS and GPSLM reveal increased surface roughness and fractal characteristics in mature kerogens, with developing microporous regions around nanopores.
Conclusions:
- Kerogen maturity significantly impacts pore structure, surface properties, and chemical homogeneity, influencing gas storage capacity.
- The developed GPSLM effectively quantifies surface heterogeneity in fractal kerogen systems.
- Findings provide insights into optimizing gas recovery from unconventional source rocks by understanding nanoscale pore evolution.
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