Department of Chemistry, University of Massachusetts, Amherst, Massachusetts 01003, United States.
Department of Biochemistry and Molecular Biology, University of Massachusetts, Amherst, Massachusetts 01003, United States.
J Phys Chem B. 2022 Sep 1;126(34):6428-6437. doi: 10.1021/acs.jpcb.2c04157. Epub 2022 Aug 23.
Water confined within hydrophobic spaces can undergo cooperative dewetting transitions due to slight changes in water density and pressure that push water toward the vapor phase. Many transmembrane protein ion channels contain nanoscale hydrophobic pores that could undergo dewetting transitions, sometimes blocking the flow of ions without physical blockages. Standard molecular dynamics simulations have been extensively applied to study the behavior of water in nanoscale pores, but the large free energy barriers of dewetting often prevent direct sampling of both wet and dry states and quantitative studies of the hydration thermodynamics of biologically relevant pores. Here, we describe a metadynamics protocol that uses the number of waters within the pore as the collective variable to drive many reversible transitions between relevant hydration states and calculate well-converged free energy profiles of pore hydration. By creating model nanopore systems and changing their radius and morphology and including various cosolvents, we quantify how these pore properties and cosolvents affect the dewetting transition. The results reveal that the dewetting free energy of nanoscale pores is determined by two key thermodynamic parameters, namely, the effective surface tension coefficients of water-air and water-pore interfaces. Importantly, while the effect of salt can be fully captured in the water activity dependence, amphipathic cosolvents such as alcohols modify both dry and wet states of the pore and dramatically shift the wet-dry equilibrium. The metadynamics approach could be applied to studies of dewetting transitions within nanoscale pores of proteins and provide new insights into why different pore properties evolved in biological systems.
由于水密度和压力的微小变化,会将水推向气相,因此被困在疏水区的水可以发生协同去湿转变。许多跨膜蛋白离子通道包含纳米级疏水性孔道,这些孔道可能会发生去湿转变,有时在没有物理阻塞的情况下阻止离子流动。标准的分子动力学模拟已广泛应用于研究纳米孔道中水分子的行为,但去湿的自由能势垒很大,通常会阻止对湿态和干态的直接采样,以及对生物相关孔道水合热力学的定量研究。在这里,我们描述了一种元动力学方案,该方案使用孔道内的水分子数量作为集体变量,驱动相关水合状态之间的许多可逆转变,并计算出孔水合的收敛良好的自由能分布。通过创建模型纳米孔系统并改变其半径和形态并包括各种共溶剂,我们量化了这些孔特性和共溶剂如何影响去湿转变。结果表明,纳米孔的去湿自由能由两个关键的热力学参数决定,即水-空气和水-孔界面的有效表面张力系数。重要的是,虽然盐的影响可以完全包含在水活度依赖性中,但两亲性共溶剂(如醇)会修饰孔的干态和湿态,并显著改变湿-干平衡。元动力学方法可应用于研究蛋白质纳米孔中的去湿转变,并为深入了解为什么不同的孔特性在生物系统中进化提供了新的见解。