Abstract
An entrainment model is developed which includes the effect of the buoyancy flux by molecular diffusion across a density interface. This effect is incorporated into the conservation equation for turbulent kinetic energy through a “diffusion parameter” RiPe -1/2, where Ri is the bulk Richardson number and Pe the Peclet number. As RiPRiPe -1/2e increases and approaches a critical limiting value the net entrainment, defined as the rate of deepening of the mixed layer, becomes zero. Based on a numerical study and on results from two experiments of different scales, it is shown that the limiting value of this parameter for entrainment to occur is approximately 10 for a salt-stratified system, though this value may depend on the diffusivity of the stratified component.
| Original language | English |
|---|---|
| Pages (from-to) | 117-130 |
| Number of pages | 14 |
| Journal | Journal of Hydraulic Research/De Recherches Hydrauliques |
| Volume | 26 |
| Issue number | 2 |
| DOIs | |
| State | Published - Mar 1988 |
Fingerprint
Dive into the research topics of 'A diftusive limit tor entrainment'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver