根据二维核磁共振测量结果评估具有复杂矿物学和孔隙结构的地层中的流体成分和孔隙体积的新工作流程

Artur Posenato Garcia, R. Mallan, Boquin Sun
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引用次数: 0

摘要

在具有复杂岩性、复杂孔隙结构或不同润湿性条件的地层中,可靠地识别流体组分并估计其饱和度是一项挑战。评估流体饱和度的常用方法依赖于电阻率测量的解释。这些技术需要模型校准,这既耗时又昂贵,而且只能区分导电和非导电流体。二维核磁共振图的解释为确定流体成分和流体体积提供了一种可行的替代方法。然而,传统的二维核磁共振解释技术依赖于T1-T2或D-T2图的截止点。当流体分量松弛响应重叠时,截止点的应用容易产生不准确性。为了解决这些缺点,我们引入了一种新的工作流程,用于识别/跟踪流体成分,并从二维核磁共振测量的解释中估计其体积。我们开发了一个近似二维核磁共振图与二维高斯分布叠加的工作流程。该算法自动确定高斯分布的最佳数量及其相应的属性(即振幅、方差和均值)。其次,对包含整个日志间隔的高斯分布参数的数据空间实现聚类技术。每个高斯分布被分配到对应于不同孔隙/流体成分的簇。然后,我们在高斯分布下计算每个深度对应的每个簇的体积。与每个簇相关的体积直接转化为每个深度不同流体成分(例如,重烃/轻烃,束缚水/自由水)对应的孔隙体积。这项工作的一个突出贡献是,与流体表征的其他岩石物理解释技术相比,引入的工作流程不需要校准工作、用户定义的截止值或专有数据集。此外,用高斯分布的叠加来近似二维核磁共振数据,可以提高具有重叠核磁共振响应的流体组分孔隙体积估计的准确性。使用高斯分布参数作为输入的聚类可以在不使用用户定义的2D截止点的情况下对不同流体成分进行深度跟踪。最后,引入的聚类的多维性提供了识别不同流体成分的独特能力,这些流体成分具有位于T1-T2图中相同坐标范围内的二维NMR响应。在两个具有复杂矿物学和孔隙结构的富有机质泥岩地层中,成功验证了新工作流程的可靠性和鲁棒性。
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A New Workflow for Assessment of Fluid Components and Pore Volumes From 2D NMR Measurements in Formations With Complex Mineralogy and Pore Structure
It is challenging to reliably identify fluid components and estimate their saturations in formations with complex lithology, complex pore structure, or varying wettability conditions. Common practices for assessing fluid saturations rely on the interpretation of resistivity measurements. These techniques require model calibration, which is time consuming/expensive and can only differentiate conductive and nonconductive fluids. Interpretation of 2D NMR maps provides a viable alternative for identifying fluid components and fluid volumes. However, conventional techniques for the interpretation of 2D NMR rely on cutoffs in the T1-T2 or D-T2 maps. The application of cutoffs is prone to inaccuracies when fluid-component relaxation responses overlap. To address these shortcomings, we introduce a new workflow for identifying/tracking fluid components and estimating their volumes from the interpretation of 2D NMR measurements. We developed a workflow that approximates 2D NMR maps with a superposition of 2D Gaussian distributions. The algorithm automatically determines the optimum number of Gaussian distributions and their corresponding properties (i.e., amplitudes, variances, and means). Next, a clustering technique is implemented to the dataspace containing the Gaussian distribution parameters obtained for the entire logged interval. Each Gaussian is assigned to a cluster corresponding to different pore/fluid components. We then calculate the volumes under the Gaussian distributions corresponding to each cluster at each depth. The volumes associated with each cluster translate directly into the pore volumes corresponding to the different fluid components (e.g., heavy/light hydrocarbon, bound/free water) at each depth. A highlighted contribution of this work is that, in contrast to the alternative petrophysical interpretation techniques for fluid characterization, the introduced workflow does not require calibration efforts, user-defined cutoffs, or proprietary data sets. Furthermore, approximating 2D NMR data with a superposition of Gaussian distributions improves the accuracy of estimated pore volumes of fluid components with overlapping NMR responses. The clustering using the Gaussian distribution parameters as inputs enables depth tracking of different fluid components without making use of user-defined 2D cutoffs. Finally, the multidimensional nature of the introduced clustering provides the unique capability of identifying different fluid components with 2D NMR response located in the same range of coordinates in a T1-T2 map. We successfully verified the reliability and robustness of the new workflow for enhancing petrophysical interpretation in two organic-rich mudrock formations with complex mineralogy and pore structure.
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