Korb J-P, Freiman G, Nicot B, Ligneul P
Physique de la Matière Condensée, Ecole Polytechnique, CNRS, 91128 Palaiseau, France.
Phys Rev E Stat Nonlin Soft Matter Phys. 2009 Dec;80(6 Pt 1):061601. doi: 10.1103/PhysRevE.80.061601. Epub 2009 Dec 1.
We introduce a method for estimating the wettability of rock/oil/brine systems using noninvasive in situ nuclear magnetic relaxation dispersion. This technique scans over a large range of applied magnetic fields and yields unique information about the extent to which a fluid is dynamically correlated with a solid rock surface. Unlike conventional transverse relaxation studies, this approach is a direct probe of the dynamical surface affinity of fluids. To quantify these features we introduce a microscopic dynamical surface affinity index which measures the dynamical correlation (i.e., the microscopic wettability) between the diffusive fluid and the fixed paramagnetic relaxation sources at the pore surfaces. We apply this method to carbonate reservoir rocks which are known to hold about two thirds of the world's oil reserves. Although this nondestructive method concerns here an application to rocks, it could be generalized as an in situ liquid/surface affinity indicator for any multimodal porous medium including porous biological media.
我们介绍了一种利用非侵入性原位核磁共振弛豫色散来估算岩石/油/盐水体系润湿性的方法。该技术在大范围的外加磁场中进行扫描,并能提供有关流体与固体岩石表面动态关联程度的独特信息。与传统的横向弛豫研究不同,这种方法是对流体动态表面亲和力的直接探测。为了量化这些特征,我们引入了一个微观动态表面亲和力指数,该指数用于测量扩散流体与孔隙表面固定顺磁弛豫源之间的动态关联(即微观润湿性)。我们将此方法应用于碳酸盐岩储层岩石,已知这类岩石蕴藏着全球约三分之二的石油储量。尽管这种无损方法在此涉及对岩石的应用,但它可以推广为适用于任何多模态多孔介质(包括多孔生物介质)的原位液体/表面亲和力指标。