Leroy Frédéric
Eduard-Zintl-Institut für Anorganische und Physikalische Chemie, Technische Universität Darmstadt, Alarich-Weiss-Strasse 8, 64287 Darmstadt, Germany and Institut für Chemie, Universität Kassel, Heinrich-Plett-Strasse 40, 34132 Kassel, Germany.
J Chem Phys. 2016 Oct 28;145(16):164705. doi: 10.1063/1.4966215.
Owing to its peculiar electronic properties, molybdenum disulfide (MoS) has been the subject of a growing number of studies in the recent years. In applications, this material and other transition metal dichalcogenides (TMDs) may have to interact with a liquid or polymer phase as well as solutions of biomolecules. It is therefore of primary importance to understand the wetting and adhesion properties of TMDs. Starting from existing models, we derive Lennard-Jones parameters for the interaction between water and the basal plane of MoS that are consistent with recent wetting experiments. Molecular dynamics simulations indicate that a stack of only two MoS monolayers is necessary to capture the wetting behavior of bulk MoS. It is found that the Coulomb interaction between water and monolayer and bilayer MoS plays no role in the related interfacial thermodynamics. Calculations with the optimized parameters show that the depth of the well of the interaction potential between water and bulk MoS is of the order of 8.2 kJ/mol. Such a value is comparable with what was found for graphite and consistent with the fact that the wetting angles of water on graphite and MoS are almost equal. The derivation of the force-field parameters is performed using a methodology which, contrary to previous studies, makes a consistent use of droplet calculations. The results of our work should find application in further simulation studies on the wetting behavior of TMDs and other dispersive materials.
由于其独特的电子特性,近年来二硫化钼(MoS)一直是越来越多研究的主题。在应用中,这种材料和其他过渡金属二硫属化物(TMDs)可能必须与液相或聚合物相以及生物分子溶液相互作用。因此,了解TMDs的润湿性和粘附性至关重要。从现有模型出发,我们推导出了与最近的润湿性实验一致的水与MoS基面之间相互作用的 Lennard-Jones 参数。分子动力学模拟表明,仅需两层MoS单层堆叠就能捕捉块状MoS的润湿行为。研究发现,水与单层和双层MoS之间的库仑相互作用在相关界面热力学中不起作用。使用优化参数进行的计算表明,水与块状MoS之间相互作用势阱的深度约为8.2 kJ/mol。这个值与石墨的情况相当,并且与水在石墨和MoS上的接触角几乎相等这一事实相符。力场参数的推导采用了一种方法,与之前的研究不同,该方法一致地使用了液滴计算。我们的工作结果应可应用于进一步关于TMDs和其他分散材料润湿行为的模拟研究。