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微观非均相润湿性和孔喉结构对致密砂岩中沥青质沉淀的影响:核磁共振结果

Effects of Microheterogeneous Wettability and Pore-Throat Structure on Asphaltene Precipitation in Tight Sandstone: Results from Nuclear Magnetic Resonance.

作者信息

Zhou Zhen, Qu Yiqian, Cheng Xin, Cheng Yuting, Lan Shuqi, Yang Zhengqi, Wei Liancheng, Sun Wei, Wu Hanning

机构信息

State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China.

Shaanxi Key Laboratory of Carbon Dioxide Sequestration and Enhanced Oil Recovery, Xi'an 710065, China.

出版信息

ACS Omega. 2024 Oct 23;9(45):45487-45500. doi: 10.1021/acsomega.4c07672. eCollection 2024 Nov 12.

Abstract

The pore throat structure and microheterogeneous wettability of tight sandstone reservoirs are complex, which leads to varying asphaltene precipitation locations, contents, and distributions in different pores during CO flooding. Clarifying the heterogeneous wettability of different pore throat structures and their effects on asphaltene precipitation and adsorption is crucial for improving CO displacement efficiency. A series of experiments were conducted in this study, including X-ray diffraction (XRD), cast thin section (CTS), field emission scanning electron microscopy (FE-SEM), high-pressure mercury intrusion (HPMI), environmental scanning electron microscopy (E-SEM), nuclear magnetic resonance (NMR), and CO flooding experiments, to investigate the pore structure complexity of tight sandstone reservoirs of the Yanchang Formation in the Ordos Basin, China. Furthermore, we investigated the variations in microheterogeneous wettability across diverse pore-throat structures and elucidated the impact of heterogeneous wettability on asphaltene precipitation during CO flooding. The findings indicate that the type and configuration of pore throats are crucial factors influencing microheterogeneous wettability. The intergranular pores are dominated by mixed wetting, and most of the dissolution pores exhibit oil wetting. The surface of Illite shows drop-like water under E-SEM, which is mainly oil wetting, whereas the surface of chlorite shows film-like water, which is water wetting. The configuration of chlorite intercrystalline pores and intergranular pores shows water wetting, whereas the configuration of Illite intergranular pores and dissolution pores shows oil wetting. During the CO flooding process, asphaltene tends to be adsorbed in the intercrystalline Illite with dissolution pores, reducing the dissolution pore volume and blocking small pores, and the displacement efficiency becomes low. In addition, asphaltene precipitation also occurs in the pore configuration of chlorite intercrystalline and intergranular pores, causing a wetting reversal on hydrophilic mineral surfaces. This reversal increases the pore throat structure complexity but has less of an impact on the flooding efficiency. A high Illite content is more likely to lead to asphaltene precipitation, significantly influencing small pore structure and the oil displacement efficiency.

摘要

致密砂岩储层的孔喉结构和微观非均质性润湿性复杂,这导致在CO驱替过程中,不同孔隙内沥青质的析出位置、含量和分布各异。阐明不同孔喉结构的非均质性润湿性及其对沥青质析出和吸附的影响,对于提高CO驱替效率至关重要。本研究开展了一系列实验,包括X射线衍射(XRD)、铸体薄片(CTS)、场发射扫描电子显微镜(FE-SEM)、高压压汞(HPMI)、环境扫描电子显微镜(E-SEM)、核磁共振(NMR)以及CO驱替实验,以研究中国鄂尔多斯盆地延长组致密砂岩储层的孔隙结构复杂性。此外,我们研究了不同孔喉结构间微观非均质性润湿性的变化,并阐明了非均质性润湿性对CO驱替过程中沥青质析出的影响。研究结果表明,孔喉的类型和形态是影响微观非均质性润湿性的关键因素。粒间孔以混合润湿性为主,大多数溶蚀孔表现为油湿性。在环境扫描电子显微镜下,伊利石表面呈滴状水,主要为油湿性,而绿泥石表面呈膜状水,为水湿性。绿泥石晶间孔和粒间孔的形态表现为水湿性,而伊利石粒间孔和溶蚀孔的形态表现为油湿性。在CO驱替过程中,沥青质倾向于吸附在含有溶蚀孔的伊利石晶间,减小溶蚀孔体积并堵塞小孔,驱替效率降低。此外,沥青质也会在绿泥石晶间孔和粒间孔的孔隙形态中析出,导致亲水性矿物表面发生润湿性反转。这种反转增加了孔喉结构的复杂性,但对驱替效率的影响较小。伊利石含量高更易导致沥青质析出,对小孔结构和驱油效率有显著影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/457b/11561598/1da2b6a21947/ao4c07672_0001.jpg

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