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Microscopic pore structure of Chang 63 reservoir in Huaqing oilfield, Ordos Basin, China and its effect on water flooding characteristics

机译:鄂尔多斯盆地华清油田长6 3 储层微观孔隙结构及其对水驱特征的影响

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Chang 63 reservoir in Huaqing oilfield, Ordos Basin, China is featured by strong pore structure heterogeneity, which leads to prominent Jamin effect in the water flooding, difficult development process, low productivity, and massive residual oil. Accordingly, this study aims to explore the microscopic pore structure of Chang 63 reservoir and investigate its influence on the water flooding efficiency, based on a series of comprehensive analyses, including physical property analysis, casting thin section observation, scanning electron microscopy measurement, high-pressure mercury injection, constant rate mercury injection, and microscopic real sandstone water flooding model. It is demonstrated that gray and gray-brown feldspathic sandstone are the main reservoir lithology in the study area, with dominant pore types of residual intergranular pores and feldspar dissolution pores. Pore throat radius is unevenly distributed, and small and micro pores take the majority. Based on the comparison of capillary pressure curve characteristics and comprehensive analysis of corresponding parameters, the pore structure of the Chang 63 reservoir is divided into four types, namely types I–IV. They have different reservoir spaces, and their reservoir and seepage capacities decrease in the order of types I–IV pore structures. Moreover, displacement patterns in them are also different, with the finger-like-reticular displacement as the primary. In addition, pore throat radius and distribution play a critical role in the water flooding. It is also demonstrated that the water flooding efficiency increases with permeability and porosity, pore structure quality, and pore throat distribution evenness.
机译:鄂尔多斯盆地华庆油田长63储层孔隙结构非均质性强,在注水中贾明效应突出,开发过程困难,产量低,残留油量大。因此,本研究的目的是在一系列综合分析的基础上,探索长63油层的微观孔隙结构,并研究其对注水效率的影响,包括物性分析,铸件薄层观察,扫描电子显微镜测量,高压汞注入,恒速汞注入和微观真实砂岩注水模型。结果表明,灰色和灰褐色的长石砂岩是该研究区的主要储层岩性,主要孔隙类型为残余粒间孔和长石溶蚀孔。孔喉半径不均匀分布,小孔和微孔占大多数。基于毛细管压力曲线特征的比较和相应参数的综合分析,Chang 63储层的孔隙结构分为I–IV型四种。它们具有不同的储层空间,其储层和渗流能力按I–IV型孔隙结构的顺序降低。而且,它们的位移模式也不同,以手指状网状位移为主要。另外,孔喉半径和分布在注水中起关键作用。还表明,注水效率随渗透率和孔隙率,孔隙结构质量和孔喉分布均匀性而增加。

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