Vugmeyster Liliya, Frazier Bailey, Fu Riqiang, Ostrovsky Dmitry
Department of Chemistry, University of Colorado at Denver, Denver, Colorado 80204, USA.
National High Magnetic Field Laboratory, Tallahassee, Florida 32310, USA.
J Chem Phys. 2025 Jul 14;163(2). doi: 10.1063/5.0279081.
Hydration shell properties in proteins remain an active topic of investigation due to their complexity and importance for biological processes. We focused on hydration shell dynamics in the solid state of the globular villin headpiece subdomain (HP36). We utilized 2H (D2O hydration) and 17O (H217O hydration) solid-state NMR spectroscopy in combination with computational modeling to obtain a comprehensive picture of water motions, starting from high-amplitude modes such as diffusion and large-angle tetrahedral jumps and progressing to lower-amplitude modes such as 2-site deuteron flips and small-angle fluctuations. The measurements consisted of NMR line shapes as well as laboratory and rotating frame relaxation rates using novel approaches, conducted in the 300-170 K temperature range and at multiple values of magnetic field strengths. They permitted the precise determination of motional parameters such as fractions of different water layers, rate constants, and activation energies. Below about 250 K, both 2H and 17O longitudinal relaxation show clear non-exponential behaviors, with at least two components whose T1 times differ by orders of magnitude. The water layer immediately adjacent to the protein surface remains mobile, as probed by the hydration dependence of NMR relaxation in the 20%-70% w/w water content range. Further, the observed non-exponentiality of 17O T1ρ relaxation at low temperatures suggests an exchange process between the layer adjacent to the protein and loosely bound shells. Based on prior results, we discuss correlations with dynamical changes in the hydrophobic core of HP36, thus obtaining insights into the interconnection of protein and water dynamics.
由于其复杂性以及对生物过程的重要性,蛋白质中的水化层性质仍是一个活跃的研究课题。我们聚焦于球状绒毛蛋白头部亚结构域(HP36)固态下的水化层动力学。我们利用2H(D2O水化)和17O(H217O水化)固态核磁共振光谱结合计算模型,从扩散和大角度四面体跳跃等高振幅模式开始,逐步深入到2位点氘核翻转和小角度波动等低振幅模式,以全面了解水的运动情况。测量包括核磁共振线形以及采用新方法的实验室和旋转坐标系弛豫率,在300 - 170 K温度范围内以及多个磁场强度值下进行。这些测量能够精确确定运动参数,如不同水层的分数、速率常数和活化能。在约250 K以下,2H和17O纵向弛豫均呈现明显的非指数行为,至少有两个成分,其T1时间相差几个数量级。在20% - 70% w/w含水量范围内,通过核磁共振弛豫的水化依赖性探测发现,紧邻蛋白质表面的水层保持可移动性。此外,在低温下观察到的17O T1ρ弛豫的非指数性表明,紧邻蛋白质的层与松散结合的壳层之间存在交换过程。基于先前的结果,我们讨论了与HP36疏水核心动态变化的相关性,从而深入了解蛋白质与水动力学的相互联系。