首页> 外文OA文献 >Stoneley Wave Propagation In Heterogeneous Permeable Porous Formations
【2h】

Stoneley Wave Propagation In Heterogeneous Permeable Porous Formations

机译:非均质渗透多孔地层中斯通利波的传播

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

The propagation of borehole Stoneley waves is strongly correlated with permeabilityof the formation. Previous studies primarily focused on the situation where the permeability is homogeneously distributed in the formation. In many in-situ situations,however, the permeability distribution of the formation is heterogeneous, due to effectssuch as a damaged zone around the borehole, random variation of the formation permeability, and layering, etc. This study investigates the effects of formation permeability heterogeneity on Stoneley wave propagation. Using the theory of dynamic permeability and a finite difference technique in cylindrical coordinates, dynamic pore fluid flow in an arbitrarily heterogeneous porous medium surrounding the borehole is modeled. The effects of the flow on the borehole Stoneley waves are calculated. The calculations were performed on various types of permeability heterogeneities. For a formation having random permeability variation with various heterogeneity scale lengths (smaller than the scale of the borehole), the Stoneley wave attenuation and dispersion are only slightly higher than those calculated with a constant permeability (mean value of the random distributions). For a formation with permeability linearly increasing or decreasing away from the borehole, the Stoneley wave behaviors are also similar to those calculated with a constant permeability. Significant effects are found for a damaged zone case where the zone has much higher permeability than the virgin formation. The attenuation exhibits a peak and the Stoneley wave velocity is significantly decreased in the frequency range from 0 to 3 kHz. These features, if measured from the data, can be used as a diagnostic of the borehole condition.
机译:井孔斯通利波的传播与地层的渗透率密切相关。先前的研究主要集中在渗透率在地层中均匀分布的情况。但是,在许多现场情况下,由于井眼周围的损坏区域,地层渗透率的随机变化和分层等影响,地层的渗透率分布是不均匀的。本研究调查了地层渗透率非均质性的影响关于斯通利波的传播。使用动态渗透率理论和圆柱坐标系中的有限差分技术,对井眼周围任意非均质多孔介质中的动态孔隙流体流动进行了建模。计算了流动对钻孔斯通利波的影响。对各种类型的渗透率非均质性进行了计算。对于具有各种非均质尺度长度(小于井眼尺度)的随机渗透率变化的地层,斯通利波的衰减和弥散仅略高于采用恒定渗透率(随机分布的均值)计算得到的值。对于渗透率线性远离井眼增加或减少的地层,斯通利波的行为也类似于恒定渗透率计算的那些。在损坏区域的情况下发现了显着效果,在该区域中,该区域的渗透性比原始地层高得多。在0至3 kHz的频率范围内,衰减呈现峰值,斯通利波速度显着降低。如果根据数据进行测量,这些特征可以用作井眼状况的诊断。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

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