SearcharxivSearch

arXiv subjects

O. Ozsun

Publications and source records attributed to O. Ozsun.

2 recordsLinked to original sources

Noninvasive Measurement of the Pressure Distribution in a Deformable Micro-Channel

Direct and noninvasive measurement of the pressure distribution in test sections of a micro-channel is a challenging, if not an impossible, task. Here, we present an analytical method for extracting the pressure distribution in a deformable micro-channel under flow. Our method is based on a measurement of the channel deflection profile as a function of applied \emph{hydrostatic} pressure; this initial measurement generates "constitutive curves" for the deformable channel. The deflection profile under flow is then matched to the constitutive curves, providing the \emph{hydrodynamic} pressure distribution. The method is validated by measurements on planar micro-fluidic channels against analytic and numerical models. The accuracy here is independent of the nature of the wall deformations and is not degraded even in the limit of large deflections, $ζ_{\rm{max}}/2h_{0}= {\cal{O}}(1)$, with $ζ_{\rm{max}}$ and $2h_0$ being the maximum deflection and the unperturbed height of the channel, respectively. We discuss possible applications of the method in characterizing micro-flows, including those in biological systems.

physics.flu-dyn

Porous Superhydrophobic Membranes: Hydrodynamic Anomaly in Oscillating Flows

We have fabricated and characterized a novel superhydrophobic system, a mesh-like porous superhydrophobic membrane with solid area fraction $Φ_s$, which can maintain intimate contact with outside air and water reservoirs simultaneously. Oscillatory hydrodynamic measurements on porous superhydrophobic membranes as a function of $Φ_s$ reveal surprising effects. The hydrodynamic mass oscillating in-phase with the membranes stays constant for $0.9\leΦ_s\le1$, but drops precipitously for $Φ_s < 0.9$. The viscous friction shows a similar drop after a slow initial decrease proportional to $Φ_s$. We attribute these effects to the percolation of a stable Knudsen layer of air at the interface.

cond-mat.soft