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Characterization of Single-Phase Flow Through Carbonate Rocks: Quantitative Comparison of NMR Flow Propagator Measurements with a Realistic Pore Network Model

机译:穿过碳酸盐岩的单相流的表征:使用实际孔网络模型的NMR流动传播剂测量结果的定量比较

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We report here the quantitative comparisons between the measured NMR flow propagator of a carbonate rock and the flow propagator calculated with a porous network extracted from the micro-CT image of the twin plug. We developed a numerical model based on a particle tracking algorithm in pore space. The particle tracking in throats is described using the first arrival time distribution. As pores have an important volume fraction in the sample considered, we implemented a time-delay mechanism for particle transport in the pores. We consider that the nodes have volume and there is a transport of the tracking particles inside the nodes, which leads to an "apparent" time-delay. Simulations of flow propagator show good agreement with low field NMR experiments performed on the twin plug of the sample used for pore network extraction with a single adjustable parameter (that describes the dynamics in the pores). These results lead us to a better understanding of the connection between pore structure and the behavior of NMR flow propagator in fluid-saturated rocks and are essential in interpreting the experimental data and correlating NMR parameters to petrophysical properties.
机译:我们在这里报告了碳酸盐岩的NMR测流仪与用从双塞子的微CT图像中提取的多孔网络计算得到的测流仪之间的定量比较。我们基于孔隙空间中的粒子跟踪算法开发了一个数值模型。使用第一到达时间分布描述了喉咙中的粒子跟踪。由于孔在所考虑的样品中具有重要的体积分数,因此我们对颗粒在孔中的传输实施了延时机制。我们认为节点具有体积,并且在节点内部存在跟踪粒子的传输,这导致“明显”时间延迟。流动传播器的仿真显示,与用于双孔插塞样品的双塞子以单个可调参数(描述了孔中的动力学)进行的低场NMR实验相吻合。这些结果使我们对流体饱和岩石中孔隙结构与NMR流动传播剂行为之间的联系有了更好的了解,对于解释实验数据以及将NMR参数与岩石物理特性相关至关重要。

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