Grashof number

From Wikipedia, the free encyclopedia

You have new messages (last change).

The Grashof number is a dimensionless number in fluid dynamics which approximates the ratio of the buoyancy force to the viscous force acting on a fluid. It is named after the German engineer Franz Grashof.

Gr = \frac{g \beta (T_s - T_\infty ) L^3}{\nu ^2}\,

where

g = acceleration due to Earth's gravity
β = volumetric thermal expansion coefficient
Ts = source temperature
T∞ = quiescent temperature
L = characteristic length
ν = kinematic viscosity

The product of the Grashof number and the Prandtl number gives the Rayleigh number, a dimensionless number that characterizes convection problems in heat transfer.

There is an analogous form of the Grashof number used in cases of natural convection mass transfer problems.

Gr_c = \frac{g \beta^* (C_{a,s} - C_{a,a} ) L^3}{\nu^2}

where

\beta^* = -\frac{1}{\rho} \left ( \frac{\partial \rho}{\partial C_a} \right )_{T,p}

and

g = acceleration due to Earth's gravity
Ca,s = concentration of species a at surface
Ca,a = concentration of species a in ambient medium
L = characteristic length
ν = kinematic viscosity
ρ = fluid density
Ca = concentration of species a
T = constant temperature
p = constant pressure

[edit] References

  • Jaluria, Yogesh. Natural Convection Heat and Mass Transfer (New York: Pergamon Press, 1980).
 v • d • e Dimensionless numbers in fluid dynamics
Archimedes • Bagnold • Bond • Brinkman • Capillary • Damköhler • Deborah • Eckert • Ekman • Euler • Froude • Galilei • Grashof • Hagen • Knudsen • Laplace • Lewis • Mach • Marangoni • Nusselt • Ohnesorge • Péclet • Prandtl • Rayleigh • Reynolds • Richardson • Rossby • Schmidt • Sherwood • Stanton • Stokes • Strouhal • Weber • Weissenberg • Womersley
Retrieved from "http://en.wikipedia.org../../../g/r/a/Grashof_number.html"