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Boussinesq Approximation for Buoyancy Formula and Calculator
Fluids Dynamics and Engineering
Boussinesq Approximation for Buoyancy Formula and Calculator
In fluid dynamics, the Boussinesq approximation (pronounced [businɛsk], named for Joseph Valentin Boussinesq) is used in the field of buoyancy-driven flow (also known as natural convection). It ignores density differences except where they appear in terms multiplied by g, the acceleration due to gravity. The essence of the Boussinesq approximation is that the difference in inertia is negligible but gravity is sufficiently strong to make the specific weight appreciably different between the two fluids. Sound waves are impossible/neglected when the Boussinesq approximation is used since sound waves move via density variations.
The advantage of the approximation arises because when considering a flow of, say, warm and cold water of density ρ1 and ρ2 one needs only to consider a single density ρ: the difference Δρ = ρ1− ρ2 is negligible. Dimensional analysis shows that, under these circumstances, the only sensible way that acceleration due to gravity g should enter into the equations of motion is in the reduced gravity g′ where:
Eq. 1
gr = g · ( ρ2 - ρ1 ) . ρ
(Note that the denominator may be either density without affecting the result because the change would be of order g(Δρ/ρ)2 The most generally used dimensionless number would be the Richardson number and Rayleigh number.
The mathematics of the flow is therefore simpler because the density ratio ρ1 / ρ2 , a dimensionless number, does not affect the flow; the Boussinesq approximation states that it may be assumed to be exactly one.
Where:
g = Acceleration due to Earth (m/s2)
ρ2 = Final Density (kg/m3)
ρ1 = Initial Density (kg/m3)
ρ = Single Density (kg/m3)
gr = Reduced Acceleration due to Gravity (m/s2)
Source:
- Wikipedia
- Physical fluid dynamics . New York: Van Nostrand Reinhold Co.
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