2010
DOI: 10.1137/090749748
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Thin Film Evolution over a Thin Porous Layer: Modeling a Tear Film on a Contact Lens

Abstract: Abstract.We examine a mathematical model describing the behavior of the precontact lens tear film of a human eye. Our work examines the effect of contact lens thickness and lens permeability on the film dynamics. Also investigated are gravitational effects and the effects of different slip models at the fluid-lens interface. A mathematical model for the evolution of the tear film is derived using a lubrication approximation applied to the hydrodynamic equations of motion in the fluid film and the porous layer.… Show more

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Cited by 28 publications
(7 citation statements)
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“…Trevelyan et al 53 consider both constant temperature and specified heat flux boundary conditions, and note that specifying the heat flux is more appropriate when modeling flows along a wall that loses heat to both the fluid and the ambient air. However, there are other applications where the constant temperature boundary condition may be more appropriate, such as in the problem considered by Nong et al 68 involving a tear layer flowing over a contact lens. In this case, the eye would be maintained at a constant temperature as a result of the body heating the eye.…”
Section: Governing Equations and Boundary Conditionsmentioning
confidence: 99%
“…Trevelyan et al 53 consider both constant temperature and specified heat flux boundary conditions, and note that specifying the heat flux is more appropriate when modeling flows along a wall that loses heat to both the fluid and the ambient air. However, there are other applications where the constant temperature boundary condition may be more appropriate, such as in the problem considered by Nong et al 68 involving a tear layer flowing over a contact lens. In this case, the eye would be maintained at a constant temperature as a result of the body heating the eye.…”
Section: Governing Equations and Boundary Conditionsmentioning
confidence: 99%
“…Among these are paints [1], contact lens manufacture [2] and microchip fabrication [3]. Gravity-driven thin film flow also occurs throughout nature, including a variety of gravity currents, such as lava flow and glacier flow [4–5].…”
Section: Introductionmentioning
confidence: 99%
“…where α (> 0) is the dimensionless Beavers-Joseph constant (see the original work by Beavers & Joseph (1967), the historical and critical note by Nield (2009), and the many papers using this condition, including, for example, Sherwood (1990), Wu (1972), Prakash & Vij (1974), Lin et al (2001), and Nong & Anderson (2010)). This condition allows for velocity slip on the interface between the fluid layer and the porous bed at z = 0 with slip length l s = k 1/2 /α.…”
Section: Governing Equations and Boundary Conditionsmentioning
confidence: 99%