陆相页岩储层核磁共振T2谱孔径转化与应用——以渤海湾盆地东营凹陷基质型页岩为例

Pore size conversion of nuclear magnetic resonance T2 spectrum in continental shale reservoirs and its application: a case study of matrix-type shale in Dongying Sag, Bohai Bay Basin

  • 摘要: 为精准表征页岩复杂孔隙结构,解决核磁共振技术在页岩储层孔径表征中因岩相差异导致的转换系数不确定问题,选取渤海湾盆地东营凹陷古近系沙河街组典型基质型陆相页岩样品,在岩心观察、薄片及扫描电镜分析基础上,系统对比了不同岩相页岩在原始、洗油、饱和油及去基底状态下的核磁共振T2谱分布特征,并采用高压压汞—气体吸附联合表征的全孔径分布数据标定核磁共振T2谱孔径,明确了不同岩相的孔径转换系数范围与多尺度孔隙结构特征。陆相基质型页岩的核磁共振半径转换系数并非定值,其范围介于4~35 nm/ms;转换系数与页岩矿物组成、结构特征及沉积构造密切相关,通常纹层越发育、结构越复杂,其值越大。页岩储层孔隙以2~500 nm孔径的中孔和宏孔为主,其中纹层状页岩因大孔和微裂缝更发育而表现出最优的储集性能。孔隙结构差异及储集品质受“沉积构造—成岩结晶”机制协同控制,纹层越发育、矿物结构越复杂,孔隙结构越优,从而具有更大的流体赋存空间和更有效的渗流通道。研究为核磁共振技术精准刻画页岩复杂孔隙结构提供了关键参数与方法,对页岩储层精细评价与“甜点”预测具有重要意义。

     

    Abstract: To accurately characterize the complex pore structure of shale and address the uncertainty of conversion coefficients in shale reservoir pore size characterization using nuclear magnetic resonance (NMR) technology due to lithofacies differences, typical matrix-type continental shale samples from Paleogene Shahejie Formation in Dongying Sag of Bohai Bay Basin were selected. Based on observations of cores, thin sections, and scanning electron microscopy analysis, the NMR T2 spectrum distribution characteristics of shale in different lithofacies in original, washed-oil, saturated-oil, and base-removed states were systematically compared. The pore size of NMR T2 spectrum was calibrated using full pore size distribution data obtained from combined high-pressure mercury injection-gas adsorption characterization, clarifying the range of pore size conversion coefficients for different lithofacies and multi-scale pore structure characteristics. The NMR radius conversion coefficient of continental matrix-type shale was not a fixed value, ranging from 4 to 35 nm/ms. The conversion coefficient was closely related to shale mineral composition, structural characteristics, and sedimentary structures. Generally, the more developed the laminae and the more complex the structure, the higher the coefficient value. Shale reservoir pores were mainly mesopores and macropores with pore size of 2-500 nm. Among them, laminated shale exhibited the best storage performance due to more developed macropores and microfractures. The differences in pore structure and reservoir quality were controlled by the synergistic mechanism of "sedimentary structure and diagenetic crystallization". The more developed the laminae and the more complex the mineral structure, the better the pore structure, resulting in larger fluid storage space and more effective seepage channels. This study provides key parameters and methods for accurately characterizing the complex pore structure of shale using NMR technology, which is of great significance for the precise evaluation and "sweet spot" prediction of shale reservoirs.

     

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