Dimensionless Numbers: Difference between revisions

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<div id="Reynolds Number"></div>
<div id="Reynolds Number"></div>
;'''Reynolds Number'''  
;'''Reynolds Number'''  
* Definition: <math> Re = \frac{UL}{\nu} </math>, where <math> U </math> and <math> L </math> are the characteristic velocity and length scales, and <math> \nu </math> is the [[Glossary#Viscosity|dynamic viscosity]].  
* Definition: <math> Re = \frac{UL}{\nu} </math>, where <math> U </math> and <math> L </math> are the characteristic velocity and length scales, and <math> \nu </math> is the [[Glossary#Viscosity|kinematic viscosity]].  
* Interpretation: The ratio of inertia force to viscous force.  
* Interpretation: The ratio of inertia force to viscous force.  
* Analysis: Small Reynolds numbers are often associated with viscous flows, whereas large Reynolds numbers are typically found in turbulent flows.
* Analysis: Small Reynolds numbers are often associated with viscous flows, whereas large Reynolds numbers are typically found in turbulent flows.

Revision as of 11:49, 28 May 2015

Mach Number
  • Definition: , where is the characteristic velocity scale, and is the speed of sound.
  • Interpretation: The ratio of inertia force to compressibility force.
  • Analysis: Compressibility effects can be neglected if Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle M < 0.3 } .
Prandtl Number
  • Definition: Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle Pr = \nu/\kappa } , where Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \nu } is the viscosity, and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \kappa } is the thermal diffusivity.
  • Interpretation: The ratio of momentum diffusivity (i.e. viscosity) to heat diffusivity.
  • Analysis: The typical Prandtl number for water is around 7 for water (At 20 degrees Celsius). See also Schmidt number.
Reynolds Number
  • Definition: Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle Re = \frac{UL}{\nu} } , where Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle U } and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle L } are the characteristic velocity and length scales, and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \nu } is the kinematic viscosity.
  • Interpretation: The ratio of inertia force to viscous force.
  • Analysis: Small Reynolds numbers are often associated with viscous flows, whereas large Reynolds numbers are typically found in turbulent flows.
Richardson Number
  • Definition: Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle Ri = N^2/U_z^2 } , where is the buoyancy frequency, and is the background horizontal velocity.
  • Interpretation: The ratio between the strength of stratification and velocity shear. Also called the gradient Richardson number.
  • Analysis: A sufficient condition for the flow to be linearly stable is that the local Richardson number exceed 0.25 throughout the flow. However, does not mean the flow is necessarily unstable (the criterion is not sufficient). When the flow is not a parallel shear flow, the meaning of is not clear.
Rossby Number
  • Definition: , where is the characteristic velocity, and is the Coriolis frequency, and is the characteristic length scale.
  • Interpretation: The ratio of the advective forces to the Coriolis pseudo-forces.
  • Analysis: When , Coriolis effects dominate and the system approaches geostrophic balance.
Schmidt Number
  • Definition: , where is the viscosity, and is the mass diffusivity.
  • Interpretation: The ratio of momentum diffusivity (i.e. viscosity) to mass diffusivity.
  • Analysis: The typical Schmidt number for water is around 500, depending on the temperature and salinity. For direct numerical simulations, is commonly used in the literature. See also Prandtl number.