Characteristic Angles in the Wetting of an Angular Region: Deposit Growth
arXiv:cond-mat/0301336 · doi:10.1103/PhysRevE.68.036306
Abstract
As was shown in an earlier paper [1], solids dispersed in a drying drop migrate to the (pinned) contact line. This migration is caused by outward flows driven by the loss of the solvent due to evaporation and by geometrical constraint that the drop maintains an equilibrium surface shape with a fixed boundary. Here, in continuation of our earlier paper [2], we theoretically investigate the evaporation rate, the flow field and the rate of growth of the deposit patterns in a drop over an angular sector on a plane substrate. Asymptotic power laws near the vertex (as distance to the vertex goes to zero) are obtained. A hydrodynamic model of fluid flow near the singularity of the vertex is developed and the velocity field is obtained. The rate of the deposit growth near the contact line is found in two time regimes. The deposited mass falls off as a weak power Gamma of distance close to the vertex and as a stronger power Beta of distance further from the vertex. The power Gamma depends only slightly on the opening angle Alpha and stays between roughly -1/3 and 0. The power Beta varies from -1 to 0 as the opening angle increases from 0 to 180 degrees. At a given distance from the vertex, the deposited mass grows faster and faster with time, with the greatest increase in the growth rate occurring at the early stages of the drying process.
arXiv commentv1: 36 pages, 21 figures, LaTeX; submitted to Physical Review E; v2: minor additions to Abstract and Introduction
References in corpus (1)
Cited by in corpus (6)
- Evaporative Deposition Patterns Revisited: Spatial Dimensions of the Deposit
- Evaporation and fluid dynamics of a sessile drop of capillary size
- Deposit Growth in the Wetting of an Angular Region with Uniform Evaporation
- Evaporation of non-circular droplets
- The nascent coffee ring with arbitrary droplet contact set: an asymptotic analysis
- Influence of gravitational forces and fluid flows on a shape of surfaces of a viscous fluid of capillary size