Instituto de Física de São Carlos, Universidade de São Paulo, CP 369, 13560-970 São Carlos, São Paulo, Brazil.
Instituto de Física de São Carlos, Universidade de São Paulo, CP 369, 13560-970 São Carlos, São Paulo, Brazil.
J Magn Reson. 2018 Jul;292:16-24. doi: 10.1016/j.jmr.2018.05.001. Epub 2018 May 4.
Nowadays, most of the efforts in NMR applied to porous media are dedicated to studying the molecular fluid dynamics within and among the pores. These analyses have a higher complexity due to morphology and chemical composition of rocks, besides dynamic effects as restricted diffusion, diffusional coupling, and exchange processes. Since the translational nuclear spin diffusion in a confined geometry (e.g. pores and fractures) requires specific boundary conditions, the theoretical solutions are restricted to some special problems and, in many cases, computational methods are required. The Random Walk Method is a classic way to simulate self-diffusion along a Digital Porous Medium. Bergman model considers the magnetic relaxation process of the fluid molecules by including a probability rate of magnetization survival under surface interactions. Here we propose a statistical approach to correlate surface magnetic relaxivity with the computational method applied to the NMR relaxation in order to elucidate the relationship between simulated relaxation time and pore size of the Digital Porous Medium. The proposed computational method simulates one- and two-dimensional NMR techniques reproducing, for example, longitudinal and transverse relaxation times (T and T, respectively), diffusion coefficients (D), as well as their correlations. For a good approximation between the numerical and experimental results, it is necessary to preserve the complexity of translational diffusion through the microstructures in the digital rocks. Therefore, we use Digital Porous Media obtained by 3D X-ray microtomography. To validate the method, relaxation times of ideal spherical pores were obtained and compared with the previous determinations by the Brownstein-Tarr model, as well as the computational approach proposed by Bergman. Furthermore, simulated and experimental results of synthetic porous media are compared. These results make evident the potential of computational physics in the analysis of the NMR data for complex porous materials.
如今,应用于多孔介质的 NMR 研究主要致力于研究分子在孔隙内和孔隙间的流体动力学。这些分析由于岩石的形态和化学成分,以及受限扩散、扩散偶联和交换过程等动态效应而变得更加复杂。由于受限几何形状(例如孔隙和裂缝)中的核自旋扩散需要特定的边界条件,因此理论解仅限于一些特殊问题,并且在许多情况下需要计算方法。随机行走方法是模拟沿数字多孔介质自扩散的经典方法。伯格曼模型通过包括在表面相互作用下磁化生存的概率速率来考虑流体分子的磁弛豫过程。在这里,我们提出了一种统计方法来关联表面磁弛豫率与应用于 NMR 弛豫的计算方法,以便阐明模拟弛豫时间与数字多孔介质孔径之间的关系。所提出的计算方法模拟了一维和二维 NMR 技术,例如,模拟纵向和横向弛豫时间(T 和 T,分别)、扩散系数(D)以及它们的相关性。为了在数值和实验结果之间获得良好的近似,有必要通过数字岩石中的微观结构保留平移扩散的复杂性。因此,我们使用通过 3D X 射线微断层扫描获得的数字多孔介质。为了验证该方法,获得了理想球形孔隙的弛豫时间,并与布朗斯坦-塔尔模型之前的测定值以及伯格曼提出的计算方法进行了比较。此外,还比较了合成多孔介质的模拟和实验结果。这些结果表明了计算物理学在分析复杂多孔材料的 NMR 数据方面的潜力。