A Taylor swimming sheet beneath a finite Brinkman layer is slower than in a Newtonian fluid unless the layer is thin, highly permeable, close to the sheet, or has a positive jump stress.
Lighthill, Flagellar hydrodynamics, SIAM 18, 161 (1976)
1 Pith paper cite this work. Polarity classification is still indexing.
1
Pith paper citing it
citation-role summary
background 1
citation-polarity summary
fields
physics.flu-dyn 1years
2025 1verdicts
CONDITIONAL 1roles
background 1polarities
background 1representative citing papers
citing papers explorer
-
A Taylor swimming sheet under a finite Brinkman layer
A Taylor swimming sheet beneath a finite Brinkman layer is slower than in a Newtonian fluid unless the layer is thin, highly permeable, close to the sheet, or has a positive jump stress.