Grashof number

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The Grashof number is a dimensionless number in fluid dynamics and Heat Transfer which approximates the ratio of the buoyancy to 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}\, For Flat Plates
 Gr_D = \frac{g \beta (T_s - T_\infty ) D^3}{\nu ^2}\, For Pipes
 Gr_D = \frac{g \beta (T_s - T_\infty ) D^3}{\nu ^2}\, For Bluff Bodies

where the D subscript indicates the length scale basis for the Grashof Number.

g = acceleration due to Earth's gravity
β = volumetric thermal expansion coefficient = 1/T; T in Kelvin
Ts = source temperature
T = film temperature
L = length
D = diameter
ν = kinematic viscosity

The Transition to turbulant flow occurs for Gr > 109 for flat plates.


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] See also

[edit] References

  • Jaluria, Yogesh. Natural Convection Heat and Mass Transfer (New York: Pergamon Press, 1980).