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Hydration structure of water confined between mica surfaces

机译:云母表面间水的水合结构

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We report further molecular dynamics simulations on the structure of bound hydration layers under extreme confinement between mica surfaces. We find that the liquid phase of water is maintained down to 2 monolayer (ML) thick, whereas the structure of the K+ ion hydration shell is close to the bulk structure even under D=0.92 nm confinement. Unexpectedly, the density of confined water remains approximately the bulk value or less, whereas the diffusion of water molecules decreases dramatically. Further increase in confinement leads to a transition to a bilayer ice, whose density is much less than that of ice Ih due to the formation of a specific hydrogen-bonding network.
机译:我们报告云母表面之间的极端限制下绑定水化层的结构的进一步的分子动力学模拟。我们发现水的液相保持低至2个单层(ML)厚度,而K +离子水化壳的结构即使在D = 0.92 nm限制下也接近于本体结构。出乎意料的是,承压水的密度大约保持在体积值以下,而水分子的扩散却急剧下降。限制的进一步增加导致向双层冰的过渡,由于形成了特定的氢键网络,其密度比冰的密度Ih小得多。

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