If angular velocity is independent of height, integrating the viscous stress ρνrΩ′ gives ΣνˉrΩ′. Thus the surface density weighted average, rather than an unweighted height average, enters vertically averaged viscous disk equations.
The viscous stress tensor records momentum flux caused by velocity gradients. For a Newtonian compressible fluid it separates into shear and bulk contributions.
The Reynolds number Re=UL/ν compares inertial and viscous effects.
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- Buoyancy-modified Darcy fingering dispersion relation
- Clean-bubble Stokes drag
- Constant gas-radiation ratio vertical disc structure
- Constant-pressure-ratio vertical disk model
- Constant viscosity in radiation-supported vertical balance
- Darcy law
- Einstein viscosity formula for a dilute suspension
- Energy dissipation identity for Model H
- Friction-dominated grounding-line evolution law
- Hydrodynamic coarsening crossover scales
- Magma
- Newtonian fluid stress tensor
- Newtonian till lubrication
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- Phase mobility
- Planar viscous-fingering dispersion relation
- Pointwise alpha-prescription obstruction in a radiation-supported layer
- Porous gravity current with background flow
- Two-layer Couette flow
- Vertically averaged alpha closure for a mixed-pressure layer
- Viscous mountain spreading over an underthrust plate
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