Related Experiment Video
Updated: Nov 27, 2025

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Evaporation Boundary Conditions for the Linear R13 Equations Based on the Onsager Theory.
Alexander Felix Beckmann1, Anirudh Singh Rana2, Manuel Torrilhon3
1Department of Mechanical Engineering, University of Victoria, Victoria, BC V8W 3P6, Canada.
New R13 evaporation boundary conditions improve rarefied gas modeling, showing better agreement with Direct Simulation Monte Carlo (DSMC) data than existing methods for microflow applications.
Area of Science:
- Fluid dynamics
- Rarefied gas dynamics
- Computational physics
Background:
- Modeling rarefied gases and microflows is challenging due to continuum hypothesis limitations at higher Knudsen numbers.
- Macroscopic transport equations and particle methods like Direct Simulation Monte Carlo (DSMC) are used for accurate solutions.
- Understanding evaporation in microflows is crucial for applications like micro fuel cells.
Purpose of the Study:
- Derive novel evaporation boundary conditions for the R13 equations, suitable for rarefied gas regimes.
- Enhance the accuracy of macroscopic transport models in microflow simulations.
- Investigate evaporation phenomena in microfluidic devices.
Main Methods:
- Derived new evaporation boundary conditions for R13 equations using Onsager relations.
- Fitted derived boundary conditions to DSMC data for coefficient determination.
- Compared new R13 boundary conditions against kinetic theory and Navier-Stokes-Fourier (NSF) solutions.
- Implemented and tested new R13 boundary conditions in a 2D numerical code.
Main Results:
- The new phenomenological R13 boundary conditions demonstrated superior agreement with DSMC data compared to existing kinetic theory R13 boundary conditions.
- Numerical simulations in 2D geometries revealed distinct flow patterns between R13 and NSF models at higher Knudsen numbers.
- The derived conditions offer improved modeling capabilities for rarefied gas microflows.
Conclusions:
- The developed R13 evaporation boundary conditions provide a more accurate macroscopic approach for rarefied gas microflows.
- The findings highlight the importance of appropriate boundary conditions for capturing complex flow physics.
- This work advances the modeling of evaporation in microfluidic systems relevant to energy applications.
More Related Videos
Related Concept Videos
Boundary Layer Characteristics
Boundary Conditions for Current Density
Electrostatic Boundary Conditions
The surface integral of an electric field is given by Gauss's law in integral form and is related to...
Magnetostatic Boundary Conditions
Boundary Conditions: Lossless Lines
At the receiving end, the boundary condition states that the voltage equals the product of the receiving-end impedance and current. This relationship is expressed as a function of the incident and...
Electrostatic Boundary Conditions in Dielectrics
Consider a case where both the mediums across a boundary are two different dielectric materials. Recall that the electric field and electric displacement are proportional and related through the material's permittivity....

