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Free Energy Assessment of Water Structures and Their Dissociation on Ru(0001)

机译:Ru(0001)上水结构及其离解的自由能评估

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The free energy landscape of the structures and dissociation degree of the first water and heavy water adlayers on Ru(0001) surface is presented. Thermodynamically favored interconversion routes connecting different experimentally reported structures are: suggested based on free energy CaleUlations. On going from low to high water coverage one-dimensional (1D) periodic Chairi-like structures with small, or zero, water dissociation degree like Chain-4a motifs are found to be very stable intermediates in the formation of dissociated and molecular ice-like bilayers, respectively. The isotopic effects ori the dissociation degree of the hie-like,bilayers are estimated: a preference for the half, dissociated form is found for H2O at temperatures below 275 K followed by energetic degeneration between all bilayers dissociated over that threshold. Instead, for heavy water this temperature is shifted to 225 K. Moreover, the configurational entropy due to the different arrangements of dissociated and molecular flat molecules further contributes to set the energie of all these structures within a small energy Window that make experimental identification difficult.
机译:给出了Ru(0001)表面第一水和重水吸附层的结构自由能态和解离度。基于自由能的CaleUlations,提出了连接不同实验报道的结构的热力学上有利的相互转化途径。从低水覆盖率到高水覆盖率,一维(1D)周期性的类似于小或零解离的椅子状结构,如Chain-4a母题被发现是离解和分子冰状形成中非常稳定的中间产物双层。估计了同位素效应或类Hie双层的解离程度:在低于275 K的温度下,H2O偏向半解离形式,然后在该阈值以上解离的所有双层之间发生了高能变性。取而代之的是,对于重水,该温度转移到225K。此外,由于解离的分子扁平分子的不同排列而导致的结构熵进一步有助于在小的能量窗内设置所有这些结构的能量,这使实验识别变得困难。

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