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Quantitative cw Overhauser Dynamic Nuclear Polarization for the Analysis of Local Water Dynamics

机译:定量cw Overhauser动态核极化分析局部水动力学

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摘要

Liquid state Overhauser Effect Dynamic Nuclear Polarization (ODNP) has experienced a recent resurgence of interest. The ODNP technique described here relies on the double resonance of electron spin resonance (ESR) at the most common, i.e. X-band (~ 10 GHz), frequency and 1H nuclear magnetic resonance (NMR) at ~ 15 MHz. It requires only a standard continuous wave (cw) ESR spectrometer with an NMR probe inserted or built into an X-band cavity. Our focus lies on reviewing a new and powerful manifestation of ODNP as a high frequency NMR relaxometry tool that probes dipolar cross relaxation between the electron spins and the 1H nuclear spins at X-band frequencies. This technique selectively measures the translational mobility of water within a volume extending 0.5–1.5 nm outward from a nitroxide radical spin probe that is attached to a targeted site of a macromolecule. This method has been applied to study the dynamics of water that hydrates or permeates the surface or interior of proteins, polymers, and lipid membrane vesicles.We begin by reviewing the recent advances that have helped develop ODNP into a tool for mapping the dynamic landscape of hydration water with sub-nanometer locality. In order to bind this work coherently together, and to place it in the context of the extensive body of research in the field of NMR relaxometry, we then rephrase the analytical model and extend the description of the ODNP-derived NMR signal enhancements. This extended model highlights several aspects of ODNP data analysis, including the importance of considering all possible effects of microwave sample heating, the need to consider the error associated with various relaxation rates, and the unique ability of ODNP to probe the electron–1H cross-relaxation process, which is uniquely sensitive to fast (tens of ps) dynamical processes. By implementing the relevant corrections in a stepwise fashion, this paper draws a consensus result from previous ODNP procedures, and then shows how such data can be further corrected to yield clear and reproducible saturation of the NMR hyperpolarization process. Finally, drawing on these results, we broadly survey the previous ODNP dynamics literature. We find that the vast number of published, empirical hydration dynamics data can be reproducibly classified into regimes of surface, interfacial, vs buried water dynamics.
机译:液相奥豪瑟效应动态核极化(ODNP)最近引起了人们的兴趣。这里描述的ODNP技术依赖于最常见的电子自旋共振(ESR)的双共振,即X波段(〜10 GHz),频率和1s H核磁共振(NMR)。 〜15 MHz。它只需要一个标准的连续波(ESW)ESR光谱仪,并在X波段腔中插入或内置一个NMR探针。我们的重点在于回顾ODNP的新的有力表现,它是一种高频NMR弛豫测量工具,可探测X波段频率下电子自旋与 1 H核自旋之间的偶极交叉弛豫。这项技术选择性地测量了从附着于大分子目标部位的氮氧自由基旋转探针向外延伸0.5-1.5 nm范围内的水的平移迁移率。该方法已被用于研究水的动态变化,这些动态水分使蛋白质,聚合物和脂质膜囊泡的表面或内部水合或渗透,我们首先回顾了最近的进展,这些进展已帮助将ODNP开发为用于绘制OD动态图的工具。水化亚纳米级的水。为了将这项工作连贯地绑定在一起,并将其置于NMR弛豫测量领域的广泛研究范围内,我们将重新定义分析模型并扩展对ODNP衍生的NMR信号增强的描述。这个扩展的模型突出了ODNP数据分析的几个方面,包括考虑微波样品加热的所有可能影响的重要性,需要考虑与各种弛豫率相关的误差以及ODNP探测电子– 的独特能力的重要性。 1 H交叉松弛过程,对快速(数十ps)动态过程非常敏感。通过逐步实施相关校正,本文从以前的ODNP程序中得出了共识结果,然后说明了如何进一步校正此类数据以产生清晰且可再现的NMR超极化过程饱和度。最后,利用这些结果,我们广泛地调查了以前的ODNP动力学文献。我们发现,大量已发布的经验水化动力学数据可以可重现地分类为地表,界面和地下水动力学模型。

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