首页> 外文会议>Pushing Technology Boundaries: Rejuvenating Fields and Skills >Return Permeability Measurements—Proceed With Caution
【24h】

Return Permeability Measurements—Proceed With Caution

机译:回油渗透率测量-谨慎行事

获取原文
获取原文并翻译 | 示例

摘要

Many papers have described different techniques and procedures for core floods that measure permeability “return permeability” to evaluate the magnitude of formation damage caused by fluid(s) used in operations (e.g. drilling muds, completion fluids). Often these measurements of permeability are used to make critical decisions for field development and well construction design. This paper demonstrates with examples, the danger on having used only the permeability measurements to determine the extent of formation damage. Commonly, laboratory core flood tests will have used core cylinders cut to 1.5 inch diameter and short lengths (less then 4 inches) unavoidably limited by core retrieval. Short core samples may be useful if the depth of formation damage was restricted to within the core length, however would have been misleading if any damaging affects extend further than this. Formation damage effects commonly extend further than the length provided by short core samples. The extent of formation damage that occurred would not have been identified by using permeability but requires identification by performing comparative before and after test geological analysis techniques. Subsequently the extent of damage must be scaled from the laboratory to the field by experts in an attempt to extrapolate what those damaging effects have on field injection and/or production. Formation damage that caused alteration(s) to any core sample should be identified by comparing before and after test permeability measurements combined with all other analysis. The nature of any damage mechanism(s) would unlikely to have been identified by just some or any one measurement alone. Scanning Electron Microscopy (Dry and Cryogenic), Energy dispersive x-ray spectrometry (EDS), X-ray Diffraction Analysis and Thin Section Analysis should be incorporated to properly determine the nature and extent of formation damage. The examples in this paper have never previously been published and they represent a continuing evolution in our understanding f formation damage measurements and mechanisms. Examples of mechanisms such as fines migration, fluid retention and mud body damage will be presented and discussed in terms of their potential impact on return permeability measurements.
机译:许多论文描述了用于岩心驱替的不同技术和程序,这些技术和程序测量渗透率“回油渗透率”,以评估由作业中使用的流体(例如钻探泥浆,完井液)引起的地层破坏的程度。通常,这些渗透率的测量结果可用于油田开发和油井施工设计的关键决策。本文通过示例演示了仅使用渗透率测量来确定地层破坏程度的危险。通常,实验室岩心洪水测试将使用切成1.5英寸直径和较短长度(小于4英寸)的岩心圆柱,这不可避免地受到岩心取回的限制。如果将地层破坏的深度限制在岩心长度之内,则短岩心样本可能会有用,但是,如果任何破坏性影响超出此范围,则可能会产生误导。地层破坏效应通常会比短岩心样本所提供的长度更大。发生的地层破坏程度无法通过使用渗透率来识别,但需要通过在测试地质分析技术之前和之后进行比较来识别。随后,必须由专家将损害的程度从实验室扩展到现场,以推断那些对田间注入和/或生产产生的破坏作用。应通过比较测试渗透率测量前后与所有其他分析的对比来识别导致任何岩心样品发生变化的地层损害。仅通过某些或任何一项测量就不可能确定任何损坏机制的性质。应结合使用扫描电子显微镜(干式和低温),能量色散X射线光谱法(EDS),X射线衍射分析和薄层分析,以正确确定地层破坏的性质和程度。本文中的示例以前从未发表过,它们代表了我们对地层损伤测量和机理的理解的不断发展。机理的例子如细粉迁移,流体滞留和泥浆体破坏将在对回油渗透率测量的潜在影响方面进行介绍和讨论。

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