Division of Biophysical Chemistry, Department of Chemistry, Lund University, P.O. Box 124, SE-22100 Lund, Sweden.
J Chem Phys. 2018 Jun 7;148(21):215103. doi: 10.1063/1.5026861.
Much of biology happens at the protein-water interface, so all dynamical processes in this region are of fundamental importance. Local structural fluctuations in the hydration layer can be probed by O magnetic relaxation dispersion (MRD), which, at high frequencies, measures the integral of a biaxial rotational time correlation function (TCF)-the integral rotational correlation time. Numerous O MRD studies have demonstrated that this correlation time, when averaged over the first hydration shell, is longer than in bulk water by a factor 3-5. This rotational perturbation factor (RPF) has been corroborated by molecular dynamics simulations, which can also reveal the underlying molecular mechanisms. Here, we address several outstanding problems in this area by analyzing an extensive set of molecular dynamics data, including four globular proteins and three water models. The vexed issue of polarity versus topography as the primary determinant of hydration water dynamics is resolved by establishing a protein-invariant exponential dependence of the RPF on a simple confinement index. We conclude that the previously observed correlation of the RPF with surface polarity is a secondary effect of the correlation between polarity and confinement. Water rotation interpolates between a perturbed but bulk-like collective mechanism at low confinement and an exchange-mediated orientational randomization (EMOR) mechanism at high confinement. The EMOR process, which accounts for about half of the RPF, was not recognized in previous simulation studies, where only the early part of the TCF was examined. Based on the analysis of the experimentally relevant TCF over its full time course, we compare simulated and measured RPFs, finding a 30% discrepancy attributable to force field imperfections. We also compute the full O MRD profile, including the low-frequency dispersion produced by buried water molecules. Computing a local RPF for each hydration shell, we find that the perturbation decays exponentially with a decay "length" of 0.3 shells and that the second and higher shells account for a mere 3% of the total perturbation measured by O MRD. The only long-range effect is a weak water alignment in the electric field produced by an electroneutral protein (not screened by counterions), but this effect is negligibly small for O MRD. By contrast, we find that the O TCF is significantly more sensitive to the important short-range perturbations than the other two TCFs examined here.
许多生物学过程都发生在蛋白质-水界面,因此该区域的所有动力学过程都具有重要意义。水合层中的局部结构波动可以通过 O 磁共振弛豫分散(MRD)来探测,在高频下,它测量双轴旋转时间相关函数(TCF)的积分——整体旋转相关时间。许多 O MRD 研究表明,在第一水合壳层中平均时,这个相关时间比在体相水中长 3-5 倍。这个旋转扰动因子(RPF)得到了分子动力学模拟的证实,这些模拟也可以揭示潜在的分子机制。在这里,我们通过分析大量的分子动力学数据,包括四个球状蛋白质和三个水模型,解决了该领域的几个悬而未决的问题。通过建立一个简单的约束指数与 RPF 的蛋白质不变指数关系,解决了极性与形貌作为水合动力学主要决定因素的棘手问题。我们得出的结论是,以前观察到的 RPF 与表面极性的相关性是极性与约束之间相关性的次要影响。水的旋转在低约束下介于受扰但类似于体相的集体机制和高约束下的交换介导的取向随机化(EMOR)机制之间。EMOR 过程占 RPF 的约一半,但在以前的模拟研究中并未被识别,这些研究只检查了 TCF 的早期部分。基于对实验相关 TCF 整个时间过程的分析,我们比较了模拟和测量的 RPF,发现 30%的差异归因于力场缺陷。我们还计算了完整的 O MRD 谱,包括由埋藏水分子产生的低频分散。为每个水合壳计算局部 RPF,我们发现扰动随时间呈指数衰减,衰减“长度”为 0.3 个壳层,第二和更高壳层仅占 O MRD 测量的总扰动的 3%。唯一的长程效应是由电中性蛋白质产生的电场中的水分子的弱取向(不由抗衡离子屏蔽),但对 O MRD 来说,这种效应可以忽略不计。相比之下,我们发现 O TCF 比这里检查的其他两个 TCF 对重要的短程扰动更为敏感。