Civil Engineering Reference
In-Depth Information
be related to the viscous effects by a model worked out by Stinson (1991). The simplified
linear equations that satisfy the velocity υ , the pressure p , and the acoustic temperature
τ
of the fluid in a pore, i.e. the variation of the temperature in an acoustic field, are
ρ 0
∂t =−∇
p
+
η
υ
(4.1)
ρ 0 c p ∂t = κ
∂p
∂t
2
τ +
(4.2)
where
is the shear viscosity (the volume viscosity is neglected), κ is the thermal con-
ductivity, c p is the specific heat per unit mass at constant pressure. For air in standard
conditions,
η
2 . 610 2 wm 1 k 1 . The pressure is consid-
ered constant on a cross- section of the tube. The boundary conditions at the air - frame
interface are
1 . 84 10 5 kg m 1 s 1 ,
η =
κ =
υ = 0
(4.3)
τ = 0
(4.4)
( 0 , 0 3 ) parallel to the
x 3 axis and whose magnitude only depends on x 1 . The variation of this velocity with x 1
produces viscous stress. Due to the viscosity, the air is subjected to a shear force parallel
to the x 3 axis, and proportional to ∂υ 3 /∂x 1 . More precisely, the right-hand side of plane
is subjected from the left-hand side of to a stress T parallel to X 3 . The projection
of T on the x 3 axis is
A volume of air is represented in Figure 4.1, with a velocity υ
η ∂υ 3 (x 1 )
∂x 1
T 3 (x 1 )
=−
(4.5)
The resulting force due to the stresses at and for a layer of unit lateral area is
d F parallel to the x 3 axis such that
η ∂υ 3 (x 1 )
∂x 1
η ∂υ 3 (x 1 + x 1 )
∂x 1
d F 3
=−
+
(4.6)
Per unit volume of air, this force is equal to
η 2 υ 3
∂x 1
X 3 =
(4.7)
Π
Π′
X 3
v(x 1 )
+∆
v
v(x 1 )
x 1
x 1
X 1
X 2
Figure 4.1
A simple velocity field in a viscous fluid.
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