Residual oil contents of dolomicrite and sandy dolomite tight oil reservoirs after CO2 huff and puff: An experimental study

被引:6
|
作者
Wei, Bo [1 ,4 ]
He, Xiaobiao [2 ]
Li, Xin [1 ]
Ju, Yiwen [3 ]
Jin, Jun [5 ]
Luo, Qiang [5 ]
机构
[1] Xinjiang Univ, Sch Geol & Min Engn, Room 512,77 Haurui Rd, Urumqi 830047, Xinjiang Uygur, Peoples R China
[2] China Univ Petr, Res Inst Unconvent Oil & Gas Sci & Technol, Beijing 100049, Peoples R China
[3] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Key Lab Computat Geodynam, Beijing 100049, Peoples R China
[4] Xinjiang Uygur Autonomous Reg 156, Coalfield Geol Explorat Team, Urumqi 830047, Xinjiang Uygur, Peoples R China
[5] PetroChina, Xinjiang Oilfield Branch Co, Expt Testing Inst, Karamay 834000, Peoples R China
基金
中国国家自然科学基金;
关键词
Tight oil reservoir; Residual oil distribution; Dolomicrite; Sandy dolomite; CO2 huff and puff; PERMIAN LUCAOGOU FORMATION; TRIASSIC YANCHANG FORMATION; NUCLEAR-MAGNETIC-RESONANCE; JUNGGAR BASIN; UNCONVENTIONAL OIL; ORDOS BASIN; PORE SIZES; JIMSAR SAG; FIELD; EOR;
D O I
10.1016/j.energy.2023.127510
中图分类号
O414.1 [热力学];
学科分类号
摘要
To clarify the differences in CO2 huff and puff (CO2-H-P) for reservoirs of different lithofacies, taking tight oil reservoirs located in northwestern China as object, lithofacies identification was conducted by analyzing mineral composition. By comparing low-field nuclear magnetic resonance (LF-NMR) T-2 spectra and full-scale pore-size distribution (PSD), the relationship between T-2 and pore-diameter was deduced, and T-2 spectra obtained during CO2-H-P were converted into PSD. Based on CO2-H-P experiments combined with LF-NMR measurements, the distributions of residual oil in reservoir rocks with different lithofacies were analyzed. The results: (1) Lithofacies of the sweet spot reservoirs were dolomicrite and sandy dolomite. The former was characterized by well-developed meso-pores (MEPs) while the latter was characterized by well-developed macro-pores (MAPs); (2) The CO2-H-P efficiency of dolomicrite was lower than that of sandy dolomite; (3) The residual oil in dolomicrite was mainly distributed in MEPs, while that in sandy dolomite was in MEPs and MAPs; (4) The existence of single fracture could promote CO2-H-P efficiency of dolomicrite while it had little influence on that of sandy dolomite. The results can promote the selection of tight oil producing intervals using CO2-H-P where reservoirs of multiple lithofacies are developed.
引用
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页数:16
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