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Observation of Slip Flow in Thermophoresis

Franz M. Weinert and Dieter Braun
Phys. Rev. Lett. 101, 168301 – Published 13 October 2008
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Abstract

Two differing theories aim to describe fluidic thermophoresis, the movement of particles along a temperature gradient. While thermodynamic approaches rely on local equilibrium, hydrodynamic descriptions assume a quasi-slip-flow boundary condition at the particle’s surface. Evidence for slip flow is presented for the case of thermal gradients exceeding (aST)1 with particle radius a and Soret coefficient ST. Thermophoretic slip flow at spheres near a surface attracts or repels tracer particles perpendicular to the thermal gradient. Moreover, particles mutually attract and form colloidal crystals. Fluid dynamic slip explains the latter quantitatively.

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  • Received 4 September 2007

DOI:https://doi.org/10.1103/PhysRevLett.101.168301

©2008 American Physical Society

Authors & Affiliations

Franz M. Weinert and Dieter Braun*

  • Systems Biophysics, Ludwig Maximilians Universität München, Amalienstrasse 54, 80799 München, Germany

  • *dieter.braun@physik.lmu.de

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Issue

Vol. 101, Iss. 16 — 17 October 2008

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