首页> 外文会议>SPWLA Annual Logging Symposium >A NOVEL APPROACH TO NUMERICAL INTEGRATION OF CONVENTIONAL, MULTICOMPONENT INDUCTION, AND MAGNETIC RESONANCE DATA IN SHALY-SAND AND CARBONATE SYSTEMS
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A NOVEL APPROACH TO NUMERICAL INTEGRATION OF CONVENTIONAL, MULTICOMPONENT INDUCTION, AND MAGNETIC RESONANCE DATA IN SHALY-SAND AND CARBONATE SYSTEMS

机译:一种新的植物 - 碳酸盐和碳酸盐系统中常规,多组分诱导和磁共振数据的数控积分方法

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Reconciling petrophysical formation parameters in carbonate and shaly-sand systems represents a challenge log analysts and petrophysicists face in dealing with well log interpretation. The problem becomes especially difficult when data from conventional (e.g., density, neutron, gamma ray) and non-conventional (e.g., NMR, multi-component induction) instruments are available and need to be combined in a consistent interpretation. Also, the use of effective and/or total porosity petrophysical models may lead to confusion and improper use and interpretation of those quantities. The paper presents different petrophysical models for use in the evaluation of carbonate and shaly-sand reservoirs, the latter with emphasis on low-resistivity laminated shaly-sand reservoirs. They allow for an effective and consistent combination of the various measurements leading to an accurate characterization of rock mineralogy, shale distribution, variation shale property, anisotropy, fluid distribution, and permeability. The proposed petrophysical models, which are tailored to integrate conventional with NMR and multi-component induction data, comprise a volumetric description of the rock, representing the fractional volumes of each rock component, and a set of response equations relating rock volumetrics with rock physical properties that are provided by the log measurements. Simultaneous and sequential solutions of the petrophysical models are proposed to facilitate the estimation of the required analyst-provided formation parameters. The paper describes the mathematical formulation of the petrophysical model as well as the applied numerical techniques. Optimal interpretation results are achieved utilizing forward modeling and a constrained, quality-weighted error minimization technique. Synthetic and real field data examples are presented, which show the ability of the proposed interpretation philosophy and methodology to reconcile formation lithology, porosity, fluid type, fluid distribution, and permeability.
机译:协调碳酸盐和Shaly - 砂系统中的岩石物理形成参数代表了挑战日志分析师和岩石物理学家面临的面临良好的日志解释。当来自常规(例如,密度,中子,伽马射线)和非常规(例如,NMR,多组分诱导)器械的数据有并且需要以一致的解释组合时,该问题变得特别困难。而且,使用有效和/或总孔隙率的岩石物理模型可能导致混淆和不当使用和解释这些数量。本文呈现出不同的岩石物理模型,用于评估碳酸盐和雪地砂储层,后者重点是低电阻率层压害材砂储层。它们允许有效且一致的各种测量组合,导致岩石矿物学,页岩分布,变异页岩性能,各向异性,流体分布和渗透性的精确表征。所提出的岩石物理模型,用于与NMR和多组分感应数据集成的常规,包括岩石的容积描述,其代表每个岩石分量的分数体积,以及与岩石物理性质相关的岩石体积的一组响应方程由日志测量提供。提出了岩石物理模型的同时和顺序溶液,以促进所需的分析人提供的形成参数。本文描述了岩石物理模型的数学制定以及应用的数值技术。利用前向建模和受约束的质量加权误差最小化技术实现了最佳解释结果。提出了合成和实场数据示例,其显示了所提出的解释哲学和方法来协调形成岩性,孔隙率,流体型,流体分布和渗透性的能力。

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