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首页> 外文期刊>The Journal of Chemical Physics >Simulations of structural and dynamic anisotropy in nano-confined water between parallel graphite plates
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Simulations of structural and dynamic anisotropy in nano-confined water between parallel graphite plates

机译:平行石墨板之间纳米约束水中结构和动态各向异性的模拟

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摘要

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 ? 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 ? to H = 20 ?, 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.
机译:我们使用分子动力学模拟来研究纳米约束水在平行石墨板之间的结构、动力学和输运特性,这些石墨板之间的分离距离(H)为7-20?在不同的水密度下,重点是由限制产生的各向异性。将承压水相与非承压散装水在类似压力和温度条件下的行为进行了比较。我们的模拟显示了平行于和垂直于石墨板的方向上承压水相的各向异性结构和动力学。这些各向异性的大小取决于狭缝宽度H.承压水显示出“固体状”结构和板块附近水层的缓慢动力学。计算了平行于和垂直于石墨板的方向的均方位移(MSD)和速度自相关函数(VACF)。通过增加从 H = 7 ?当 H = 20 ?时,MSD 增加,VACF 的行为表明承压水从类固体变为类液体动力学。如果使用几何标准(即石墨板之间的距离)设置水相的初始密度,则在水中建立大压力(大约为 ~10 katm)和大压力各向异性。通过将约束板之间的水密度降低到约0.9 g cm~(?3),观察到水层的气泡形成和重组。

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