Department of Chemistry, Isfahan University of Technology, Isfahan 84156-83111, Iran.
J Chem Phys. 2012 Nov 14;137(18):184703. doi: 10.1063/1.4763984.
We use molecular dynamics simulations to study the structure, dynamics, and transport properties of nano-confined water between parallel graphite plates with separation distances (H) from 7 to 20 Å at different water densities with an emphasis on anisotropies generated by confinement. The behavior of the confined water phase is compared to non-confined bulk water under similar pressure and temperature conditions. Our simulations show anisotropic structure and dynamics of the confined water phase in directions parallel and perpendicular to the graphite plate. The magnitude of these anisotropies depends on the slit width H. Confined water shows "solid-like" structure and slow dynamics for the water layers near the plates. The mean square displacements (MSDs) and velocity autocorrelation functions (VACFs) for directions parallel and perpendicular to the graphite plates are calculated. By increasing the confinement distance from H = 7 Å to H = 20 Å, the MSD increases and the behavior of the VACF indicates that the confined water changes from solid-like to liquid-like dynamics. If the initial density of the water phase is set up using geometric criteria (i.e., distance between the graphite plates), large pressures (in the order of ~10 katm), and large pressure anisotropies are established within the water. By decreasing the density of the water between the confined plates to about 0.9 g cm(-3), bubble formation and restructuring of the water layers are observed.
我们使用分子动力学模拟来研究平行石墨板之间纳米受限水的结构、动力学和输运性质,分离距离(H)从 7 埃到 20 埃不等,重点研究受限产生的各向异性。受限水相的行为与类似压力和温度条件下的非受限体相水进行了比较。我们的模拟表明,受限水相在平行和垂直于石墨板的方向上表现出各向异性的结构和动力学。这些各向异性的大小取决于狭缝宽度 H。受限水在靠近板的水层中表现出“固态”结构和缓慢的动力学。计算了平行和垂直于石墨板方向的均方位移(MSD)和速度自相关函数(VACF)。通过将约束距离从 H = 7 Å 增加到 H = 20 Å,MSD 增加,VACF 的行为表明受限水从固态动力学转变为液态动力学。如果用水相的初始密度根据几何标准(即,石墨板之间的距离)确定,则在水中会建立大的压力(约 10 katm)和大的压力各向异性。通过将受限板之间的水密度降低到约 0.9 g cm(-3),观察到气泡形成和水层的重构。