2018
DOI: 10.20944/preprints201807.0327.v1
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Evaporation Boundary Conditions for the Linear R13 Equations Based on the Onsager Theory

Abstract: Due to failure of the continuum hypothesis for higher Knudsen numbers, rarefied gases and microflows of gases are particularly difficult to model. Macroscopic transport equations compete with particle methods, such as DSMC to find accurate solutions in the rarefied gas regime. Due to growing interest in micro flow applications, such as micro fuel cells, it is important to model and understand evaporation in this flow r egime. H ere, e vaporation b oundary c onditions f or t he R 13 equations, which are macrosc… Show more

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Cited by 3 publications
(18 citation statements)
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“…Similar computations confirm that the fields due to a point heat source placed in a isobaric stationary-state rarefied gas flow close to a no-temperature jump surface (Eqs. (27), solutions (28) and boundary condition (18)) are equivalent to the ones obtained in (43a) and (43b).…”
Section: The Solution To This Differential Equation Iŝmentioning
confidence: 74%
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“…Similar computations confirm that the fields due to a point heat source placed in a isobaric stationary-state rarefied gas flow close to a no-temperature jump surface (Eqs. (27), solutions (28) and boundary condition (18)) are equivalent to the ones obtained in (43a) and (43b).…”
Section: The Solution To This Differential Equation Iŝmentioning
confidence: 74%
“…We start with the case of a point heat source (thermal Gradlet) placed in a heat flow close to a temperature jump surface (Eqs. (26), solutions (28) and boundary condition (30)). The Fourier transformed temperature jump boundary condition is now quite complicated:…”
Section: Solutions For Rarefied Gas Flows Close To Boundariesmentioning
confidence: 99%
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