首页> 外文期刊>Fuel >Pore-scale characterization of tight sandstone in Yanchang Formation Ordos Basin China using micro-CT and SEM imaging from nm- to cm-scale
【24h】

Pore-scale characterization of tight sandstone in Yanchang Formation Ordos Basin China using micro-CT and SEM imaging from nm- to cm-scale

机译:鄂尔多斯盆地延长组致密砂岩孔隙尺度特征的微CT和SEM成像

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

In this work, we measured the porosity, permeability, electrical resistivity and NMR T-2 spectrum of the tight sandstone samples from Yanchang Formation Ordos Basin China. The experimental results indicate weak correlation between porosity and other bulk properties. A workflow of multi-scale digital rock technique is proposed to characterize pore geometry and connectivity in order to understand the ability of fluid flow or electric conduct of tight sandstones. A series of SEM images tiles (MAPS technique) with a resolution of 100 nm in a large field of view (FOV) are first recorded on one end surface of sample and then stitched together to reveal fine pore structure, pore type and pore size distribution. Energy-Dispersive SEM (EDS-SEM) is performed on one the same end of the samples to obtain a mineralogy mapping which will be further used to identify mineralogy. The samples with the diameter of 25.4 mm are scanned by X-ray Micro Computed Tomography (CT) to obtain 3D grayscale images, on which image registration, segmentation and cluster-labelling algorithms are applied to generate multi-mineral digital rock and investigate pore connectivity in 3D. The results of digital rock analysis demonstrate that the pore space of tight sandstone is classified into three types, residual intergranular pore, dissolved pore and micro pore in clay mineral. The results of pore size distribution for each type of pore indicate that the micro pore in clay dominates pore space in tight sandstone. The original intergranular pores are partly filled by clay minerals, where the micro pores contained in form percolation pathway and control the fluid flow through pore pace. The permeability and electrical properties of tight sandstones are dominated by micro pore and have higher dependence of the pore structure than only on porosity. The multimineral digital rock proposed in the study can be further applied in numerical simulation of bulk properties and quantitate analysis in nano-geoscience. (C) 2017 Elsevier Ltd. All rights reserved.
机译:在这项工作中,我们测量了中国鄂尔多斯盆地延长组致密砂岩样品的孔隙度,渗透率,电阻率和NMR T-2谱。实验结果表明,孔隙度与其他体积性质之间的相关性较弱。提出了一种多尺度数字岩石技术的工作流程来表征孔隙的几何形状和连通性,以了解致密砂岩的流体流动或导电能力。首先在样品的一个端面上记录一系列在大视野(FOV)中具有100 nm分辨率的SEM图像切片(MAPS技术),然后将它们缝合在一起以显示精细的孔结构,孔类型和孔径分布。在样品的同一端进行能量分散SEM(EDS-SEM),以获得矿物学图谱,该图将进一步用于鉴定矿物学。通过X射线微计算机断层扫描(CT)扫描直径为25.4 mm的样品,以获得3D灰度图像,在该图像上应用图像配准,分割和簇标记算法生成多矿物数字岩石并研究孔隙连通性在3D中。数字岩石分析结果表明,致密砂岩的孔隙空间可分为粘土矿物中的残余粒间孔隙,溶解孔隙和微孔隙三种类型。每种孔隙类型的孔径分布结果表明,粘土中的微孔占致密砂岩孔隙空间的主导。原始的粒间孔被粘土矿物部分填充,其中的微孔形成渗流路径,并控制流体通过孔道的流动。致密砂岩的渗透性和电学性质主要由微孔构成,并且对孔隙结构的依赖性高于对孔隙度的依赖性。研究中提出的多矿物数字岩石可进一步应用于纳米地球科学的块体性质数值模拟和定量分析。 (C)2017 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Fuel》 |2017年第1期|254-264|共11页
  • 作者单位

    China Univ Petr East China, Coll Sci, Qingdao 266580, Peoples R China;

    China Univ Petr East China, Coll Sci, Qingdao 266580, Peoples R China;

    China Univ Petr East China, Coll Sci, Qingdao 266580, Peoples R China;

    PetroChina Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    PetroChina Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    PetroChina Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    PetroChina Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    PetroChina Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    China Univ Petr East China, Res Inst Unconvent Oil & Gas & Renewable Energy, Qingdao 266580, Peoples R China;

    China Univ Petr East China, State Key Lab Heavy Oil Proc, Qingdao 266580, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Tight sandstone; Pore scale; Pore size distribution; Pore connectivity; Digital rock physics;

    机译:致密砂岩;孔隙尺度;孔隙大小分布;孔隙连通性;数字岩石物理学;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号