曲折
多孔介质
磁导率
核磁共振
材料科学
地质学
多孔性
物理
化学
岩土工程
膜
生物化学
作者
P. E. Øren,Frank Antonsen,Håkon Rueslåtten,S. Bakke
出处
期刊:SPE Annual Technical Conference and Exhibition
日期:2002-09-29
被引量:35
摘要
Abstract We reconstruct the three-dimensional (3D) microstructure of Fontainebleau sandstone samples of different porosities by a process-based reconstruction method. Permeabilities of the reconstructed media are computed by solving the Stokes equations, while the formation factors are computed by solving a Laplacian equation. Nuclear Magnetic Resonance (NMR) responses are determined by a random walk simulation, and the results are compared with experimental data. Permeabilities estimated from commonly used NMR correlations are compared with the computed permeabilities. The comparison shows that the accuracy of the NMR-derived permeabilities can be improved significantly by accounting for tortuosity effects and variations in surface relaxivity.
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