MacDiarmid Institute for Advanced Materials and Nanotechnology, School of Chemical and Physical Sciences, Victoria University of Wellington, Wellington 6001, New Zealand.
J Magn Reson. 2010 Aug;205(2):209-15. doi: 10.1016/j.jmr.2010.04.020. Epub 2010 May 6.
We present a propagator-resolved 2D exchange spectroscopy technique for observing fluid motion in a porous medium. The susceptibility difference between the matrix and the fluid is exploited to produce an inhomogeneous internal magnetic field, causing the Larmor frequency to change as molecules migrate. We test our method using a randomly packed monodisperse 100 microm diameter glass bead matrix saturated with distilled water. Building upon previous 2D exchange spectroscopy work we add a displacement dimension which allows us to obtain 2D exchange spectra that are defined by both mixing time and spatial displacement rather than by mixing time alone. We also simulate our system using a Monte Carlo process in a random nonpenetrating monodisperse bead pack, finding good agreement with experiment. A simple analytic model is used to interpret the NMR data in terms of a characteristic length scale over which molecules must diffuse to sample the inhomogeneous field distribution.
我们提出了一种传播子分辨的 2D 交换波谱技术,用于观察多孔介质中的流体运动。利用基质和流体之间的磁化率差异产生不均匀的内磁场,导致分子迁移时拉莫尔频率发生变化。我们使用用直径为 100 微米的单分散玻璃珠基质随机填充并饱和蒸馏水的方法对我们的方法进行了测试。在之前的 2D 交换波谱工作的基础上,我们添加了一个位移维度,这使我们能够获得由混合时间和空间位移定义的 2D 交换光谱,而不仅仅是由混合时间定义。我们还使用随机非贯穿单分散珠包中的蒙特卡罗过程对我们的系统进行了模拟,发现与实验吻合较好。我们使用一个简单的分析模型,根据分子必须扩散的特征长度来解释 NMR 数据,以对非均匀磁场分布进行采样。