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A generating mechanism for apparent fluid slip in hydrophobic microchannels

机译:疏水微通道表观流体滑移的产生机理

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Fluid slip has been observed experimentally in micro- and nanoscale flow devices by several investigators [e.g., Tretheway and Meinhart, Phys. Fluids 14, L9 (2002); Zhu and Granik, Phys. Rev. Lett. 87, 096105 (2001); Pit et al., Phys. Rev. Lett. 85, 980 (2000); and Choi et al., Phys. Fluids 15, 2897 (2003)]. This paper examines a possible mechanism for the measured fluid slip, for water flowing over a hydrophobic surface. We extend the work of Lum et al. [J. Phys. Chem. B 103, 4570 (1999)], Zhu and Granick [Phys. Rev. Lett. 87, 096105 (2001)], Granick et al. [Nature Materials 2, 221 (2003)], and de Gennes [Langmuir 18, 3413 (2002)], who suggest slip develops from a depleted water region or vapor layer near a hydrophobic surface. By modeling the presence of either a depleted water layer or nanobubbles as an effective air gap at the wall, we calculate slip lengths for flow between two infinite parallel plates. The calculated slip lengths are consistent with experimental values when the gas layer is modeled as a continuum and significantly higher when rarefied gas conditions are assumed. The results suggest that the apparent fluid slip observed experimentally at hydrophobic surfaces may arise from either the presence of nanobubbles or a layer of low density fluid at the surface. (C) 2004 American Institute of Physics.
机译:几位研究人员已在微米级和纳米级流量装置中通过实验观察到流体滑移[例如Tretheway和Meinhart,Phys。流体14,L9(2002); Zhu和Granik,物理学。牧师87,096105(2001);皮特(Pit)等人,物理学。牧师85,980(2000);和Choi等人,Phys。流体15,2897(2003)。本文研究了一种可能的机制,用于测得的流体滑移,流过疏水表面的水。我们扩展了Lum等的工作。 [J.物理化学B 103,4570(1999)],Zhu and Granick [Phys。牧师87,096105(2001)],Granick等人。 [Nature Materials 2,221(2003)]和de Gennes [Langmuir 18,3413(2002)],他们提出滑移是从疏水表面附近的贫水区域或蒸汽层形成的。通过将枯竭的水层或纳米气泡的存在建模为壁上的有效气隙,我们计算了两个无限平行板之间流动的滑移长度。当将气体层建模为连续体时,计算出的滑动长度与实验值一致,而在假设稀有气体条件下,计算出的滑动长度与实验值一致。结果表明,在疏水表面上实验观察到的表观流体滑移可能是由于纳米气泡或表面上低密度流体层的存在而引起的。 (C)2004美国物理研究所。

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