首页> 外文会议>SPWLA annual logging symposium >Investigation of the impact of diagenesis on the petrophysical properties in the complex porosity systems in carbonates
【24h】

Investigation of the impact of diagenesis on the petrophysical properties in the complex porosity systems in carbonates

机译:碳酸盐岩中复杂孔隙体系中成岩作用对岩石物性影响的研究

获取原文

摘要

The determination of petrophysical properties incarbonate rocks is strongly affected byheterogeneity at different scales. Complexdepositional and diagenetic processes have led tosystems with a very wide range of pore sizesinvolving many decades of length-scales (e.g.,from sub-micron to cm), which cannot be capturedby a single-resolution x-ray CT image.Calculations of flow parameters such aspermeability, relative permeability and capillarypressure do require the representative multiscalepore system to get accurate prediction. Thereforemodels of the pore space that include the full rangeof pore sizes and their connectivity are vital for thisrequirement in petrophysics and reservoirsimulation. Recently a multiscale pore-networksgenerated from statistical models extracted fromimages at different resolutions have shown as animportant tool for multiscale pore description (Wuet al, 2011). In this work we explore the extensionof this multiscale pore-reconstruction and imagestatistical description to include diageneticprocesses. We present a study of the impact ofdiagenetic processes on the evolution of carbonaterock by quantification of pore size andconnectivity, modelling the process of cementationand dissolution using derived information fromcatholuminescent thin section images indicatingvarious stages of diagenesis. The diageneticprocesses includes cementation and dissolution inboth the meteoric and burial diageneticenvironments and are modelled using PoreArchitecture model to dissolve grains in the regionsof the best connectivity estimated fromreconstructed 3D images of carbonate samples. Anintegrated multi-scale pore-network is thengenerated and the petrophysical predictions wouldbe performed on a pore-network flow simulator. Atlast a further study of comprehensive rock typingcombining diagenetic processes on poreconnectivity and petrophysical properties isinvestigated to better understand the diageneticcontrols of the pore system and transportproperties.
机译:岩石中岩石物理性质的测定。 碳酸盐岩受到以下因素的强烈影响 不同规模的异质性。复杂的 沉积和成岩作用导致 孔径范围很广的系统 涉及数十年的长度尺度(例如, (从亚微米到厘米),无法捕获 通过单分辨率X射线CT图像。 流量参数的计算,例如 渗透率,相对渗透率和毛细管 压力确实需要代表多尺度 毛孔系统以获得准确的预测。所以 包含所有范围的毛孔空间模型 孔径的大小及其连通性对此至关重要 岩石物理和储层的需求 模拟。最近有一个多尺度的孔网 从统计模型中提取 不同分辨率的图像显示为 多尺度孔隙描述的重要工具(吴 等人,2011)。在这项工作中,我们探索扩展 多尺度毛孔重建和图像 统计描述,包括成岩作用 流程。我们提出一项对以下方面的影响的研究 碳酸盐演化的成岩过程 岩石通过孔径和数量的量化 连通性,为胶结过程建模 并使用从中获得的信息解散 阴极发光薄层图像指示 成岩的各个阶段。成岩作用 过程包括胶结和溶解 既有成岩的,也有成岩的 环境,并使用毛孔进行建模 溶解区域中的谷物的体系结构模型 估计的最佳连通性 重建碳酸盐样品的3D图像。一个 然后是集成的多尺度孔隙网络 产生的岩石物理预测 在孔网流动模拟器上执行。在 最后对综合岩石分型进行了进一步研究 结合孔隙上的成岩作用 连接性和岩石物理特性是 调查以更好地了解成岩作用 控制毛孔系统和运输 特性。

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