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Characterization of micro-nano pore networks in shale oil reservoirs of Paleogene Shahejie Formation in Dongying Sag of Bohai Bay Basin, East China

机译:渤海湾盆地东营凹陷古近系沙河街组页岩油储层中的微纳孔隙特征

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AbstractFor typical blocky, laminated and bedded mudrock samples from the Paleogene Shahejie Formation in the Dongying Sag of Bohai Bay Basin, this work systematically focuses on their structure characterization of multiple micro-nano pore networks. A use of mercury injection capillary pressure (MICP) documented the presence of multiple μm-nm pore networks, and obtained their respective porosity, permeability and tortuosity. Different sample sizes (500-841 μm GRI fractions, 1 cm-sized cubes, and 2.54 cm in diameter and 2-3 cm in height core plugs) and approaches (low-pressure N2gas physisorption, GRI matrix permeability, MICP, helium pycnometry, and pulse decay permeameter) were used to measure pore size distribution, porosity and permeability. The average porosity and matrix permeability determined from MICP are (6.31±1.64)% and (27.4±31.1)×10-9μm2, the pore throat diameter of pores is mainly around 5 nm, and the median pore throat diameter based on 50% of final cumulative volume is (8.20±3.01) nm in shale. The pore-throat ratios decrease with a decrease of pore size diameter. Moreover, the permeability of shale samples with lamination is nearly 20 times larger than matrix permeability. The geometrical tortuosity of the nano-scale 2.8?10.0 nm pore networks is 8.44 in these shales, which indicates a poor connectivity of matrix pore network and low flow capability. Overall, the variable and limited pore connectivity of shale samples will affect hydrocarbon preservation and recovery.
机译:摘要对于渤海湾盆地东营凹陷古近系沙河街组典型的块状,层状和层状泥岩样品,这项工作系统地集中于多个微纳孔隙网络的结构表征。使用汞注入毛细管压力(MICP)记录了多个μm-nm孔隙网络的存在,并获得了它们各自的孔隙率,渗透率和曲折度。不同的样品尺寸(500-841μmGRI分数,1 cm大小的立方体,直径2.54 cm和高度2-3 cm的岩心塞)和方法(低压N2气体物理吸附,GRI基质渗透性,MICP,氦比重瓶,和脉冲衰减渗透仪)来测量孔径分布,孔隙率和渗透率。由MICP测定的平均孔隙率和基体渗透率分别为(6.31±1.64)%和(27.4±31.1)×10-9μm2,孔的孔喉直径主要在5 nm左右,中值的孔喉直径基于50%的页岩的最终累积体积为(8.20±3.01)nm。孔喉比随着孔径直径的减小而减小。此外,层状页岩样品的渗透率几乎比基质渗透率大20倍。在这些页岩中,纳米级2.8?10.0 nm孔网的几何曲折度为8.44,这表明基质孔网的连通性差且流动能力低。总体而言,页岩样品孔隙连通性的变化和局限性将影响油气的保存和采收。

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