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2D and 3D nanopore characterization of gas shale in Longmaxi formation based on FIB-SEM

机译:基于FIB-SEM的龙马溪组页岩气页岩的2D和3D纳米孔表征

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摘要

Studying complex pore structures is the key to understanding the mechanism of shale gas accumulation. FIB-SEM (focused ion beam-scanning electron microscope) is the mainstream and effective instrument for imaging nanopores in gas shales. Based on this technology, 2D and 3D characteristics of shale samples from Lower Silurian Longmaxi formation in southern Sichuan Basin were investigated. 2D experimental results show that the pores in shale are nanometer-sized, and the structure of those nanopores can be classified into three types: organic pores, inorganic pores and micro fractures. Among the three types, organic pores are dominantly developed in the OM (organic matter) with three patterns such as continuous distributed OM, OM between clay minerals and OM between pyrite particles, and the size of organic pores range from 5 nm to 200 nm.Inveresly, inorganic pores and micro fractures are less developed in the Longmaxi shales. 3D digital rocks were reconstructed and segmented by 600 continuous images by FIB cutting and SEM imaging simultaneously. The pore size distribution and porosity can be calculated by this 3D digital core, showing that its average value is 32 nm and porosity is 3.62%.The 3D digital porosity is higher than its helium porosity, which can be regarded as one important parameter for evaluation of shale gas reserves. The 2D and 3D characterized results suggest that the nanometer-sized pores in organic matter take up the fundamental storage space for the Longmaxi shale. These characteristics have contributed to the preservation of shale gas in this complex tectonic area. (C) 2016 Elsevier Ltd. All rights reserved.
机译:研究复杂的孔隙结构是理解页岩气成藏机理的关键。 FIB-SEM(聚焦离子束扫描电子显微镜)是对天然气页岩中的纳米孔成像的主流且有效的仪器。基于这项技术,研究了四川盆地南部下志留统龙马溪组页岩样品的二维和三维特征。二维实验结果表明,页岩中的孔隙为纳米级,这些纳米孔的结构可分为有机孔隙,无机孔隙和微裂缝三种类型。在这三种类型中,有机孔隙主要以OM(有机物)的连续分布,黏土矿物之间的OM和黄铁矿颗粒之间的OM三种模式出现,有机孔隙的大小范围为5 nm至200 nm。在龙马溪页岩中,无机孔隙和微裂缝很少出现。通过FIB切割和SEM成像,同时重建3D数字岩石并通过600个连续图像进行分割。利用该3D数字核心可以计算出孔径分布和孔隙率,表明其平均值为32 nm,孔隙率为3.62%.3D数字孔隙率高于其氦气孔隙率,这可以作为评价的重要参数之一页岩气储量。 2D和3D表征结果表明,有机质中的纳米级孔隙占据了Longmaxi页岩的基本储藏空间。这些特征有助于在这个复杂的构造区域保存页岩气。 (C)2016 Elsevier Ltd.保留所有权利。

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