首页> 外文会议>SPE Middle East Unconventional Resources Conference >Petrophysical and Fluid Flow Properties of a Tight Carbonate Source Rock Using Digital Rock Physics
【24h】

Petrophysical and Fluid Flow Properties of a Tight Carbonate Source Rock Using Digital Rock Physics

机译:使用数字岩石物理学的岩石物理和流体流动性能

获取原文

摘要

The evaluation of shale is complicated by the structurally heterogeneous nature of fine-grained strata and their intricate pore networks,which are interdependent on many geologic factors including total organic carbon(TOC)content,mineralogy,maturity and grain-size.The ultra-low permeability of the shale rock requires massive hydraulic fracturing to enhance connectivity and increase permeability for the flow.To design an effective fracturing technique,it is necessary to have a good understanding of the reservoir characteristics and fluid flow properties at multiple scales. In this work,representative core plug samples from a tight carbonate source rock in the Middle East were characterized at the core-and pore-scale levels using a Digital Rock Physics(DRP)workflow.The tight nature of the carbonate rocks prevented the use of conventional methods in measuring special core analysis(SCAL)data.Two-dimensional Scanning Electron Microscopy(SEM)and three-dimensional Focused Ion Beam(FIB)-SEM analysis were studied to characterize the organic matter content in the samples together with(organic and inorganic)porosity and matrix permeability.The FIB-SEM images in 3D were also used to determine petrophysical and fluid flow(SCAL)properties in primary drainage and imbibition modes. A clear trend was observed between porosity and permeability related to identified rock fabrics and organic matter in the core.The organic matter was found to have an effect on the imbibition two-phase flow relative permeability and capillary pressure behavior and hysteresis trends among the analyzed samples.The data obtained from DRP provided information that can enhance the understanding of the pore systems and fluid flow properties in tight formations,which cannot be derived accurately using conventional methods.
机译:SALE的评估因细粒色谱层的结构性异质性和其复杂的孔隙网络而异,这在许多地质因子中是相互依存的,包括总有机碳(TOC)含量,矿物学,成熟度和晶粒尺寸。超低页岩岩石的渗透性需要大量的液压压裂,以提高连通性并提高流动的渗透性。设计有效的压裂技术,有必要在多种尺度处具有良好的理解储存器特性和流体流动性质。在这项工作中,从在中东致密碳酸盐源岩代表芯插头样品进行表征在使用数字岩石物理(DRP)工作流程。紧碳酸盐岩的性质芯和孔隙尺度水平防止使用测量特殊核心分析(SCAS)DATA.TWO维扫描电子显微镜(SEM)和三维聚焦离子束(FIB)-SEM分析的常规方法进行了研究,以表征样品中的有机物质含量(有机和无机)孔隙率和基质渗透率。3D中的FIB-SEM图像还用于确定初级排水和吸入模式下的岩浆物和流体流动(SCAL)性质。孔隙率和渗透性之间观察到核心和核心相关的渗透性之间的明显趋势。发现有机物对分析的样品中的增生两相流动相对渗透性和毛细管压力行为以及滞后趋势产生影响。从DRP获得的数据提供了可以增强对孔系统的理解和在紧密地层中的流体流动性质的信息,这不能使用常规方法准确地推导。

著录项

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