Halle Bertil
Department of Biophysical Chemistry, Lund University, SE-22100 Lund, Sweden.
Philos Trans R Soc Lond B Biol Sci. 2004 Aug 29;359(1448):1207-23; discussion 1223-4, 1323-8. doi: 10.1098/rstb.2004.1499.
The properties of water in biological systems have been studied for well over a century by a wide range of physical techniques, but progress has been slow and erratic. Protein hydration--the perturbation of water structure and dynamics by the protein surface--has been a particularly rich source of controversy and confusion. Our aim here is to critically examine central concepts in the description of protein hydration, and to assess the experimental basis for the current view of protein hydration, with the focus on dynamic aspects. Recent oxygen-17 magnetic relaxation dispersion (MRD) experiments have shown that the vast majority of water molecules in the protein hydration layer suffer a mere twofold dynamic retardation compared with bulk water. The high mobility of hydration water ensures that all thermally activated processes at the protein-water interface, such as binding, recognition and catalysis, can proceed at high rates. The MRD-derived picture of a highly mobile hydration layer is consistent with recent molecular dynamics simulations, but is incompatible with results deduced from intermolecular nuclear Overhauser effect spectroscopy, dielectric relaxation and fluorescence spectroscopy. It is also inconsistent with the common view of hydration effects on protein hydrodynamics. Here, we show how these discrepancies can be resolved.
在超过一个世纪的时间里,人们运用各种各样的物理技术对生物系统中的水的特性进行了研究,但进展缓慢且不稳定。蛋白质水合作用——即蛋白质表面对水的结构和动力学的扰动——一直是争议和困惑的一个特别丰富的来源。我们在此的目的是批判性地审视蛋白质水合作用描述中的核心概念,并评估当前蛋白质水合作用观点的实验基础,重点关注动态方面。最近的氧 - 17 磁弛豫色散(MRD)实验表明,与 bulk 水相比,蛋白质水合层中的绝大多数水分子仅遭受两倍的动态迟缓。水合水的高流动性确保了蛋白质 - 水界面处的所有热激活过程,如结合、识别和催化,都能以高速进行。由 MRD 得出的高度流动的水合层的图景与最近的分子动力学模拟一致,但与从分子间核 Overhauser 效应光谱、介电弛豫和荧光光谱推导的结果不兼容。它也与水合作用对蛋白质流体动力学的普遍观点不一致。在此,我们展示了如何解决这些差异。