论文标题
石墨下2D禁令的润湿性
Wettability of graphite under 2D confinement
论文作者
论文摘要
纳米限制下固体/液体界面的热力学对液体传输特性具有巨大的影响。在这里,我们使用分子动力学研究了石墨纳米缝隙,并研究了水/石墨界面张力如何随限制程度而变化。我们发现,对于0.7nm至2.6nm之间的纳米通道高度,石墨比散装更疏水,并且表面张力的值振荡,然后最终朝着较大缝隙的恒定值收敛。表面张力的值与流体的滑动长度相关,并用有效和界面密度,水合压力和摩擦系数进行解释。该研究清楚地表明,临界通道高度为0.9nm(可实现的实验性1),表面张力达到其最高值,但整个通道的水扩散为最小。结构分析表明,对于此孔径,2D和3D氢键网络之间的过渡伴随着构象熵的突然增加。我们的结果表明,固体表面的润湿性在纳米填充下可能会发生变化,并且数据可用于解释实验性渗透性数据。
The thermodynamics of solid/liquid interfaces under nanoconfinement has tremendous implications for liquid transport properties. Here using molecular dynamics, we investigate graphite nanoslits and study how the water/graphite interfacial tension changes with the degree of confinement. We found that, for nanochannel heights between 0.7nm and 2.6nm, graphite becomes more hydrophobic than in bulk, and that the value of the surface tension oscillates before eventually converging towards a constant value for larger slits. The value of the surface tension is correlated with the slip length of the fluid and explained in terms of the effective and interfacial density, hydration pressure and friction coefficient. The study clearly indicates that there is a critical channel height of 0.9nm (achievable experimentally1) at which the surface tension reaches its highest value, but the water diffusion across the channel is at its minimum. The structural analysis shows that for this pore size a transition between a 2D and 3D hydrogen bond network is accompanied by an abrupt increase in conformational entropy. Our results show that the wettability of solid surfaces can change under nanoconfinement and the data can be used to interpret the experimental permeability data.