介质色散的核磁共振映射分布

J. Funk, M. Myers, L. Hathon
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引用次数: 0

摘要

核磁共振和介电测量的结合经常解决常规油藏中具有挑战性的饱和度和润湿性测定问题。当考虑孔隙结构效应时,核磁共振(NMR)特征是基于表面弛豫的评价来解释的,并且介电结构响应归因于岩石基质的“纹理”。如果考虑到分子运动和电荷迁移率,这两种孔隙结构描述符都可以得到改进。与Bloembergen, Purcell和Pound (BPP)模型中核磁共振和介电相关时间测量的偶极弛豫等价类似,我们开发了一个假设具有代表性的麦克斯韦-瓦格纳弛豫的弛豫时间相关。Myers证明的碳酸盐基质和孔隙组分的介电色散曲线使用介电弛豫时间(DRT)模型进行了量化。基于与电导率相关的增强Debye屏蔽距离,将模拟的孔隙系统分数光谱映射到核磁共振T1或T2分布。表征的核磁共振分布通过微ct孔径测定和扩散相关性进行了验证。映射的分布为岩石物理学提供了与导电性弯曲度和附加润湿性筛选标准相关的常用阿尔奇指数组合(mn)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
NMR-Mapped Distributions of Dielectric Dispersion
Combinations of NMR and dielectric measurements frequently address challenging saturation and wettability determinations in conventional reservoirs. When pore structure effects are addressed, the nuclear magnetic resonance (NMR) characteristics are interpreted based on the evaluations of surface relaxivity, and the dielectric structural response is attributed to the “texture” of the rock matrix. Both pore structure descriptors can be improved if the molecular motions and charge mobility common to the measurements are considered. Similar to the dipolar relaxation equivalence of NMR and dielectric correlation time measurements in the Bloembergen, Purcell, and Pound (BPP) model, we develop a relaxation time correlation assuming representative Maxwell-Wagner relaxations. Dielectric dispersion curves for the carbonate matrix and vug pore components demonstrated by Myers are quantified using a dielectric relaxation time (DRT) model. The modeled pore system fractions are spectrally mapped to the NMR T1 or T2 distributions based on enhanced Debye shielding distances correlated with the conductivity. The characterized NMR distributions are validated with micro-CT pore-size determinations and diffusion correlations. The mapped distributions provide petrophysical insight into the frequently used Archie exponent combination (mn) associated with conductivity tortuosity and additional wettability screening criteria.
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