Jacob Timo, Goddard William A
Materials and Process Simulation Center, Beckman Institute (139-74), California Institute of Technology, Pasadena, California 91125, USA.
J Am Chem Soc. 2004 Aug 4;126(30):9360-8. doi: 10.1021/ja049920y.
Recent quantum mechanical (QM) calculations for a monolayer of H(2)O on Ru(0001) suggested a novel stable structure with half the waters dissociated. However, different studies on Pt(111) suggested an undissociated bilayer structure in which the outer half of the water has the OH bonds toward the surface rather than the O lone pair. Since water layers on Pt are important in many catalytic processes (e.g., the fuel cell cathode), we calculated the energetics and structure of the first monolayer of water on the Pt(111) surface using QM [periodic slab using density functional calculations (DFT) with the PBE-flavor of exchange-correlation functional]. We find that the fully saturated surface ((2)/(3) ML) has half the water almost parallel to the surface (forming a Pt-O Lewis acid-base bond), whereas the other half are perpendicular to the surface, but with the H down toward the surface (forming a Pt-HO agostic bond). This leads to a net bond energy of 0.60 eV/water = 13.8 kcal/mol (the standard ice model with the H up configuration of the water molecules perpendicular to the surface is less stable by 0.092 eV/water = 2.1 kcal/mol). We examined whether the partial dissociation of water proposed for Ru(0001) could occur on Pt(111). For the saturated water layer ((2)/(3) ML) we find a stable structure with half the H(2)O dissociated (forming Pt-OH and Pt-H covalent bonds), which is less favorable by only 0.066 eV/water = 1.51 kcal/mol. These results confirm the interpretation of combined experimental (XAS, XES, XPS) and theoretical (DFT cluster and periodic including spectrum calculations) studies, which find only the H down undissociated case. We find that the undissociated structure leads to a vertical displacement between the two layers of oxygens of approximately 0.42 A (for both H down and H up). In contrast, the partially dissociated system leads to a flat structure with a separation of the oxygen layers of 0.08 A. Among the partially dissociated systems, we find that all subsurface positions for the dissociated hydrogen are less favorable than adsorbing on top of the free Pt surface atom. Our results suggest that for less than (1)/(3) ML, clustering would be observed rather than ordered monolayer structures.
近期针对Ru(0001)表面单层H₂O的量子力学(QM)计算表明,存在一种新型稳定结构,其中一半的水分子发生解离。然而,对Pt(111)的不同研究表明,存在一种未解离的双层结构,其中外层水分子的OH键朝向表面,而非氧孤对电子朝向表面。由于Pt表面的水层在许多催化过程(如燃料电池阴极)中很重要,我们使用QM[采用密度泛函理论(DFT)并结合PBE味的交换关联泛函的周期性平板模型]计算了Pt(111)表面第一层水的能量和结构。我们发现,完全饱和的表面((2)/(3) ML)有一半的水分子几乎与表面平行(形成Pt - O路易斯酸碱键),而另一半垂直于表面,但氢原子朝下朝向表面(形成Pt - HO agostic键)。这导致每个水分子的净键能为0.60 eV/水分子 = 13.8 kcal/mol(水分子垂直于表面且氢原子朝上的标准冰模型稳定性低0.092 eV/水分子 = 2.1 kcal/mol)。我们研究了Ru(0001)上提出的水分子部分解离情况是否会在Pt(111)上发生。对于饱和水层((2)/(3) ML),我们发现一种稳定结构,其中一半的H₂O发生解离(形成Pt - OH和Pt - H共价键),其稳定性仅低0.066 eV/水分子 = 1.51 kcal/mol。这些结果证实了结合实验(XAS、XES、XPS)和理论(DFT团簇及包括光谱计算的周期性模型)研究的解释,该解释仅发现了氢原子朝下的未解离情况。我们发现,未解离结构导致两层氧原子之间的垂直位移约为0.42 Å(氢原子朝下和朝上情况均如此)。相比之下,部分解离体系导致一种扁平结构,氧层间距为0.08 Å。在部分解离体系中,我们发现解离氢原子的所有次表面位置都不如吸附在自由Pt表面原子顶部有利。我们的结果表明,对于小于(1)/(3) ML的情况,会观察到团簇现象,而非有序的单层结构。