Abstract
A theory is developed to account for the variable nature of the specific heat C and the transport coefficients of thermal and mass diffusion, λ and D, for the quasi-steady equilibrium vaporization of a droplet in an unbounded, stagnant atmosphere. In the theory C, λ, and D are all temperature dependent whereas C and λ are further concentration weighted. Results from the present theory are found to agree within 15% with existing numerical solutions.
Original language | English (US) |
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Pages (from-to) | 1426-1432 |
Number of pages | 7 |
Journal | Physics of Fluids |
Volume | 18 |
Issue number | 11 |
DOIs | |
State | Published - 1975 |
All Science Journal Classification (ASJC) codes
- Condensed Matter Physics
- Mechanics of Materials
- Mechanical Engineering
- Fluid Flow and Transfer Processes
- Computational Mechanics