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Squeeze-Flow in the Presence of a Temperature Gradient: Effective Attraction between Asperites in the Friction Zone of Two Solids
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Published/Copyright:
June 1, 2005
Abstract
The equations of hydrodynamics are solved for a slow squeeze-Oow in the presence of a gradient of the viscosity which, in turn, is caused by a temperature gradient. The gradient induces an asymmetry of the spreading velocity and a drift of the center of mass towards the direction where the viscosity is decreasing. Due to this phenomenon, adjacent asperites in the friction zone between two solids sliding over each other experience an effective attraction.
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Published Online: 2005-06-01
Published in Print: 2002-06-12
Copyright © 2002 by Walter de Gruyter GmbH & Co. KG
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Articles in the same Issue
- GENERIC Projection-Operator Derivation of Boltzmanns Kinetic Equation
- Squeeze-Flow in the Presence of a Temperature Gradient: Effective Attraction between Asperites in the Friction Zone of Two Solids
- Black Hole Thermodynamics. A Classical Non-Equilibrium Approach
- Phenomenological Kinetics of Real Gas-Adsorption-Systems: Isothermal Adsorption
Articles in the same Issue
- GENERIC Projection-Operator Derivation of Boltzmanns Kinetic Equation
- Squeeze-Flow in the Presence of a Temperature Gradient: Effective Attraction between Asperites in the Friction Zone of Two Solids
- Black Hole Thermodynamics. A Classical Non-Equilibrium Approach
- Phenomenological Kinetics of Real Gas-Adsorption-Systems: Isothermal Adsorption
