Civil Engineering Reference
In-Depth Information
determination of the characteristic viscous and thermal lengths. A procedure to do this is
to plot the quantity
⎧
2
⎫
⎛
⎞
⎛
c
⎞
⎪
⎪
1
0
eff
y
=
Re
as a function of
⎜
⎟
,
a linear function given by
⎨
⎜
⎟
⎬
⎜
⎟
c
f
⎪
⎝
⎠
⎪
⎝
⎠
⎩
⎭
⎡
⎤
⎛
⎞
1
μ
1
γ
−
1
yk
≈+
1
+
.
(5.73)
⎢
⎥
⎜
Λ
⎟
s
ρπ
′
f
Pr
Λ
⎢
⎝
⎠
⎥
⎣
⎦
0
1.50
1.45
1.40
1.35
1.30
Helium
1.25
1.20
1.15
Air
1.10
1.05
1.00
0.000
0.001
0.002
0.003
0.004
Square rot of inverse frequency ((1/Hz)
1/2
)
Figure 5.35
The relationship between the real part of (c
0
/c
eff
)
2
and the square root of the inverse frequency for
a porous material having air-filled and helium-filled pores, respectively. The ordinate is normalized by the
tortuosity
k
S
. Material parameters: r − 30000Pa⋅s/m
2
, σ − 0.95, Λ − 50μm, Λ′ − 100μm. Solid lines - complete
model. Dashed lines - approximate model.
The slope of this function gives the possibility of determining the length
L
in the
expression
−
1
−
=+
⎡
1
γ
1
⎤
L
,
⎢
⎥
Λ
′
Pr
Λ
⎣
⎦
whereas
k
S
again is determined by the intercept with the ordinate. Performing this
measurement twice, once by having the pores filled with air and, second, by helium, we
can determine Λ and Λ′ by finding the slopes
b
air
and
b
He
given by