Optimization of NMR Permeability Transform and Application to a Source Rock Reservoir

Jin-Hong Chen, Stacey M Althaus, M. Boudjatit
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Abstract

Permeability is a fundamentally important property of reservoir rocks that governs the flow of the reservoir fluids and production rates. Many methods have been developed to estimate permeability, including well established and documented laboratory measurements on whole core and plugs, analysis of formation test data, and analysis of production. Obtaining permeability from nuclear magnetic resonance (NMR) T1 or T2 has proven to be a cost effective method that can provide continuous permeability along a wellbore. This method uses a transform function on NMR well log data to calculate permeability. An accurate NMR permeability transform requires calibration to fit local data of a specific field based on measured data from representative cores from the field. The general form of the permeability transform developed for conventional sandstone and carbonate reservoirs does not work well for extremely tight reservoirs such as source rocks. Here we show a generic optimization method to find the optimal permeability transform for any tight reservoirs using NMR log data and laboratory measured permeability data from samples at selected depth of the logged well. This optimization method is applied to a source rock well and a permeability transform was obtained. The transform is a function of the movable fluid in the rock and logarithm mean of the NMR relaxation time. The permeability calculated from the transform is comparable to measured permeability from core samples.
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某烃源岩储层核磁共振渗透率变换优化及应用
渗透率是储层岩石的一项重要性质,它决定着储层流体的流动和产量。目前已经开发了许多估算渗透率的方法,包括对整个岩心和桥塞的实验室测量、地层测试数据分析和生产分析。通过核磁共振(NMR) T1或T2获得渗透率已被证明是一种经济有效的方法,可以沿井筒提供连续的渗透率。该方法利用核磁共振测井资料的变换函数计算渗透率。一个精确的核磁共振渗透率变换需要标定以拟合特定区域的局部数据,该数据是基于该区域代表性岩心的实测数据。常规砂岩和碳酸盐岩储层渗透率转化的一般形式不适用于烃源岩等极致密储层。在这里,我们展示了一种通用的优化方法,利用核磁共振测井数据和实验室测量的渗透率数据,在选定的测井井深度找到任何致密储层的最佳渗透率变换。将该优化方法应用于某烃源岩井,得到了渗透率的变换。该变换是岩石中可动流体和核磁共振弛豫时间的对数平均值的函数。通过变换计算的渗透率与岩心样品的实测渗透率相当。
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