渗吸
大孔隙
油页岩
地质学
矿物学
石油工程
材料科学
化学
生物化学
植物
介孔材料
生物
发芽
古生物学
催化作用
作者
Jianhong Zhu,Junbin Chen,Zhi-wei Gong,Tuan-qi Yao,Xiaoming Wang,Xiangrong Nie
出处
期刊:Springer series in geomechanics and geoengineering
日期:2023-01-01
卷期号:: 6337-6355
标识
DOI:10.1007/978-981-99-1964-2_542
摘要
Spontaneous imbibition is an important mechanism governing the shale oil reservoir production performance, especially in the early stage of production after multi-stage volume hydraulic fracturing. The microscopic pore structure of reservoirs is an important factor affecting imbibition. In this study, for the samples drilled from Chang 7 continental shale reservoirs of the Yanchang Formation in Ordos Basin, China, scanning electron microscope (SEM), high-pressure mercury injection (HPMI), and nuclear magnetic resonance (NMR) T2 with water saturated were preformed to study pore structure characteristics and characterize quantitatively pore-size distribution. The results showed that the rock is tight shale and contains various clays and minerals, and micropores (≤0.1 μm) and small pores (0.1 μm–1.0 μm) are the main pore types and accounts for almost more than 90% of total pore volume. Next, conducted spontaneous imbibition experiments to reveal the SI law of Chang 7 continental shale, using NMR technology. Results show that the imbibition recovery is inverse proportion to the length of cores. And the micro-characteristics of spontaneous imbibition recovery is different with the pores, the imbibition amount of micropores is most, next is small pores, that of macropores is least, and the recovery degree is macropores, micropores and small pores from large to small. Furthermore, the initial imbibition rate is the largest in macropores, followed by micropores. Meanwhile, the spontaneous imbibition of macropores reach the equilibrium stage firstly, followed by small pores and finally micropores. The results show that the imbibition process of Chang 7 continental shale is not only affected by capillary force, but also affected by obvious oil-water viscous resistance.
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