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The influence of macropore heterogeneity on the petrophysical properties of carbonates.

机译:大孔异质性对碳酸盐岩岩石物理性质的影响。

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摘要

The objective of this research is to better understand the petrophysical properties of hydrocarbon bearing carbonate rocks. The specific properties that are investigated are: electrical properties, capillary pressure curves, permeability and displacement behavior. The relationship between the petrophysical properties and various geological classification systems is also explored.;A porous plate capillary desaturation cell that can simultaneously measure electrical properties, capillary pressure curves and displacement behavior has been built. Up to 12 cores can be simultaneously desaturated. Both gas and crude oil were used as the non-wetting phase.;In accordance with Lucia's carbonate porosity classification, two oil fields were chosen, one with vuggy porosity and the other with interparticle porosity. Cores from the Dune field and the Yates field in the San Andres-Grayburg formations in west Texas were used as examples of interparticle and vuggy porosity systems. Saturation exponents for the Dune field cores were found to be lie between 1.6 and 2.5, and the cementation exponents were approximately 2.2. Experimental results showed very poor correlation between the geologically defined lithofacies and the measured petrophysical properties.;The effect of vugularity on the petrophysical properties was evident from the Yates core experiments. For a constant porosity, as vugularity increases, m and n increase systematically. The irreducible water saturation, the capillary pressure curves and the displacement behavior are also substantially different.;CAT-scanning was used for characterizing the local heterogeneity of the core. Cores were CAT scanned at 1 mm increments to generate a 3-dimensional porosity map. Three dimensional resistivity maps were generated from these local porosities. A random walk method was used to estimate the resistivity of the core. Simulation results and experimental results showed good agreement.
机译:这项研究的目的是更好地理解含碳酸盐碳酸盐岩的岩石物性。研究的特定特性是:电特性,毛细管压力曲线,渗透率和位移行为。还探讨了岩石物性与各种地质分类体系之间的关系。建立了可同时测量电性能,毛细管压力曲线和位移行为的多孔板毛细管去饱和池。最多可以同时使12个核饱和。天然气和原油都被用作非润湿相。根据卢西亚的碳酸盐岩孔隙度分类,选择了两个油田,一个为松散孔隙度,另一个为颗粒间孔隙度。得克萨斯州西部圣安德列斯-格雷堡地层的沙丘场和耶茨场的岩心被用作粒子间和松散孔隙系统的例子。发现沙丘场岩心的饱和指数在1.6到2.5之间,而胶结指数约为2.2。实验结果表明,地质定义的岩相与测得的岩石物理特性之间的相关性很差。从耶茨岩心实验可以明显看出,孔隙度对岩石物理特性的影响。对于恒定的孔隙率,随着孔隙度的增加,m和n会系统地增加。不可还原的水饱和度,毛细管压力曲线和位移行为也有很大的不同。; CAT扫描用于表征岩心的局部非均质性。以1 mm的增量CAT扫描岩心,以生成三维孔隙率图。从这些局部孔隙率生成三维电阻率图。使用随机游走法估计岩心的电阻率。仿真结果与实验结果吻合良好。

著录项

  • 作者

    Bae, Wisup.;

  • 作者单位

    The University of Texas at Austin.;

  • 授予单位 The University of Texas at Austin.;
  • 学科 Engineering Petroleum.
  • 学位 Ph.D.
  • 年度 1992
  • 页码 254 p.
  • 总页数 254
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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