Dipartimento di Chimica I.F.M. and Center for Molecular Imaging, Università Degli Studi di Torino, Torino, Italy.
J Magn Reson. 2011 May;210(1):107-12. doi: 10.1016/j.jmr.2011.02.017. Epub 2011 Feb 23.
When a hydrogenation reaction is carried out with gaseous hydrogen enriched in its para- isomer in the earth magnetic field (prior to adiabatic insertion of the sample in the NMR magnet), enhanced proton longitudinal order (represented by 2I(z)(A)I(z)(B)) is created but also difference of enhanced polarizations (I(z)(A)-I(z)(B)). In a first part, it is shown theoretically and experimentally that the longitudinal relaxation time of this polarization difference is roughly twice the ones of individual polarizations. The second part is devoted to a pulse sequence designed for transforming this difference into net hyperpolarization. The evolution of this global hyperpolarization is studied experimentally in a third part and it is observed that a fraction of hyperpolarization possesses an effective longitudinal relaxation time similar to the one of the initial polarization difference. Those experimental results are interpreted by numerical calculations based on Solomon-type equations including the longitudinal order and possibly dipolar-csa cross correlation rates.
当在地球磁场中用富含其顺磁异构体的氢气进行加氢反应时(在绝热插入 NMR 磁铁之前),会产生增强的质子纵向有序(由 2I(z)(A)I(z)(B)表示),但也会产生增强的极化差异(I(z)(A)-I(z)(B))。在第一部分,从理论和实验上证明了这种极化差的纵向弛豫时间大致是单个极化的两倍。第二部分致力于设计一个脉冲序列,将这种差异转化为净超极化。在第三部分中,实验研究了这种整体超极化的演化,观察到超极化的一部分具有类似于初始极化差的有效纵向弛豫时间。这些实验结果通过基于包括纵向有序和可能的偶极-csa 交叉相关率的 Solomon 型方程的数值计算来解释。