Cole, DJ and Payne, MC and Csányi, G and Spearing, SM and Colombi Ciacchi, L (2007) Development of a classical force field for the oxidized Si surface: application to hydrophilic wafer bonding. J Chem Phys, 127. 204704-. ISSN 0021-9606Full text not available from this repository.
We have developed a classical two- and three-body interaction potential to simulate the hydroxylated, natively oxidized Si surface in contact with water solutions, based on the combination and extension of the Stillinger-Weber potential and of a potential originally developed to simulate SiO(2) polymorphs. The potential parameters are chosen to reproduce the structure, charge distribution, tensile surface stress, and interactions with single water molecules of a natively oxidized Si surface model previously obtained by means of accurate density functional theory simulations. We have applied the potential to the case of hydrophilic silicon wafer bonding at room temperature, revealing maximum room temperature work of adhesion values for natively oxidized and amorphous silica surfaces of 97 and 90 mJm(2), respectively, at a water adsorption coverage of approximately 1 ML. The difference arises from the stronger interaction of the natively oxidized surface with liquid water, resulting in a higher heat of immersion (203 vs 166 mJm(2)), and may be explained in terms of the more pronounced water structuring close to the surface in alternating layers of larger and smaller densities with respect to the liquid bulk. The computed force-displacement bonding curves may be a useful input for cohesive zone models where both the topographic details of the surfaces and the dependence of the attractive force on the initial surface separation and wetting can be taken into account.
|Uncontrolled Keywords:||Computer Simulation Models, Chemical Oxidation-Reduction Quantum Theory Silicon Dioxide Solutions Surface Properties Water Wettability|
|Divisions:||Div C > Applied Mechanics|
|Depositing User:||Cron Job|
|Date Deposited:||09 Dec 2016 17:15|
|Last Modified:||25 Mar 2017 01:00|