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Imparting Directional Dependence on Log-Derived Permeability

机译:赋予对数导数渗透率的方向依赖性

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Cost-effective, efficient production of hydrocarbons depends on accurate reserves estimates, reservoir architecture, and hydrocarbon distribution. In addition, a complete reservoir description, including both horizontal and vertical permeability, is critical to efficient development strategy. Hydrocarbon recovery efficiency depends on many factors, but one key parameter is the ratio of vertical to horizontal permeability. There are numerous ways to estimate permeability. It is now possible to estimate permeability from continuous formation evaluation measurements. However, it remains difficult to determine directional permeability. Nuclear magnetic resonance (NMR) logs are used routinely to estimate permeability, but NMR-derived permeability is based on scalar properties (e.g., φ, T_2 distributions from NMR, and bulk volume irreducible water) and is inherently a scalar property itself. Few formation evaluation measurements provide directional information. Dip and image logs provide bed thickness and layer dip information, while the multieomponent induction instrument (3DEX) and crossed-dipole shear-wave acoustic tools provide direct measurements of macroscopic formation anisotropy. In this paper, we explore theoretically and with real data the computation of permeability anisotropy. We use laminated sand models as well as macroscopic models based on the resistivity anisotropy measurements to estimate k_v:k_H ratios. In addition to multieomponent induction data, we explore stand-alone and joint interpretation of NMR property variations to predict the macroscopic reservoir permeability anisotropy.
机译:具有成本效益的,有效的碳氢化合物生产取决于准确的储量估算,储层构造和碳氢化合物分布。此外,完整的储层描述(包括水平和垂直渗透率)对于有效的开发策略至关重要。碳氢化合物的回收效率取决于许多因素,但是一个关键参数是垂直渗透率与水平渗透率之比。有许多估算渗透率的方法。现在可以从连续地层评估测量中估算渗透率。然而,仍然难以确定方向渗透率。常规使用核磁共振(NMR)测井来估算磁导率,但是NMR衍生的磁导率是基于标量性质(例如NMR的φ,T_2分布以及不可压缩的水体积),并且本身就是标量性质。很少有地层评价测量提供方向信息。倾角和图像测井记录可提供层厚和层倾角信息,而多元素感应仪(3DEX)和交叉偶极横波声波测井仪可直接测量宏观地层各向异性。在本文中,我们从理论上和实际数据上探索了渗透率各向异性的计算方法。我们使用层压砂模型以及基于电阻率各向异性测量的宏观模型来估计k_v:k_H比。除了多元素诱导数据外,我们还探索了NMR特性变化的独立解释和联合解释,以预测宏观储层渗透率各向异性。

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