Occurrence Characteristics of Fluids in Shale Oil Reservoirs via a 2D NMR and Frozen Core Analysis: A Case Study of the Jurassic Lianggaoshan Formation in Central Sichuan Basin
The T1-T2 two-dimensional nuclear magnetic resonance (2D NMR) technique, combined with cryogenic core preservation, provides a novel approach to characterize in situ fluid occurrence states in shale oil reservoirs. This study investigates the Jurassic Lianggaoshan Formation in the Sichuan Basin through 2D NMR experiments under frozen (-10 °C) and formation-temperature (60 °C) conditions, followed by measurements on oil-washed, water-saturated, and oil-saturated cores. The results distinguish key components such as bitumen/kerogen (T1/T2 > 100), adsorbed oil (T1/T2 ≈ 5), and free oil (T1/T2 ≈ 1) and reveal that temperature elevation significantly enhances free oil mobility (T2 range expanded by 4.9-fold). A fluid identification chart was established to quantify shale oil movability, offering a practical tool for reservoir evaluation.
Authors
- Haoming Chen (ORCID: https://orcid.org/0000-0002-2227-3515)
- Chunyu Qin
- Qiang Xie (ORCID: https://orcid.org/0000-0002-7003-7533)
- Changhong Cai (ORCID: https://orcid.org/0000-0002-0582-3394)
- Yiqing Zhu (ORCID: https://orcid.org/0000-0002-2668-2252)
- Rui Zhang (ORCID: https://orcid.org/0000-0002-4441-4761)
- Kai Yu (ORCID: https://orcid.org/0000-0001-7939-0950)
- Qian Pang (ORCID: https://orcid.org/0000-0001-5169-5859)
Institutions
- Planetary Science Institute (US)
- Southwest Petroleum University (CN)
- Yangtze University (CN)
- Chengdu University of Technology (CN)
- Ministry of Education (SA)
- State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (CN)
- Oil and Gas Center (CN)
- PetroChina Southwest Oil and Gas Field Company (China)
Publication Details
- Journal
- ACS Omega
- Published
- 2025-10-29
- DOI
- https://doi.org/10.1021/acsomega.5c06962
- Citations
- 1
- Primary Topic
- Hydrocarbon exploration and reservoir analysis
- Type
- article
- Field-Weighted Citation Impact
- 0.86