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Updated: May 24, 2025

Controlling Flow Speeds of Microtubule-Based 3D Active Fluids Using Temperature
Published on: November 26, 2019
Temperature-driven flows in nanochannels: Theory and simulations
Pietro Anzini1,2, Zeno Filiberti1, Alberto Parola1,2
1Dipartimento di Scienza e Alta Tecnologia, Università degli Studi dell'Insubria, Via Valleggio 11, 22100 Como, Italy.
Thermo-osmosis, fluid motion driven by temperature gradients near surfaces, is explained by pressure gradients. This study provides a theoretical solution and validates it with molecular dynamics simulations.
Area of Science:
- Fluid Dynamics
- Thermodynamics
- Statistical Mechanics
Background:
- Thermo-osmosis describes fluid motion driven by thermal gradients without external forces.
- The phenomenon arises from tangential pressure gradients near confining surfaces.
- Previous work elucidated its microscopic origins using linear response theory.
Purpose of the Study:
- To provide an explicit theoretical solution for thermo-osmotic fluid flow in slab geometry.
- To derive a simple expression for the pressure gradient using equilibrium properties.
- To validate theoretical predictions through extensive nonequilibrium molecular dynamics simulations.
Main Methods:
- Utilized conservation laws to solve stationary fluid flow equations.
- Expressed the thermo-osmotic coefficient as a mass-heat current correlation function.
- Performed 2D nonequilibrium molecular dynamics simulations with varying wall-particle interactions.
Main Results:
- Derived an explicit solution for the thermo-osmotic coefficient.
- Obtained a simple expression for the pressure gradient in terms of equilibrium properties.
- Simulations showed good agreement with theoretical predictions for pressure drop and velocity profiles in both liquid and gas regimes.
Conclusions:
- The theoretical framework accurately describes thermo-osmotic phenomena.
- The derived correlation function provides a microscopic link to macroscopic transport coefficients.
- Molecular dynamics simulations confirm the validity of the theoretical approach across different fluid states.
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