Eulerian-Lagrangian aspects of a steady multiscale laminar flow
One key feature for the understanding and control of turbulent flows is the relation between Eulerian and Lagrangian statistics. This Brief Communication investigates such a relation for a laminar quasi-two-dimensional multiscale flow generated by a multiscale (fractal) forcing, which reproduces som...
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Veröffentlicht in: | Physics of fluids (1994) 2007-07, Vol.19 (7), p.078108-078108-4 |
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Zusammenfassung: | One key feature for the understanding and control of turbulent flows is the relation between Eulerian and Lagrangian statistics. This Brief Communication investigates such a relation for a laminar quasi-two-dimensional multiscale flow generated by a multiscale (fractal) forcing, which reproduces some aspects of turbulent flows in the laboratory, e.g., broadband power-law energy spectrum and Richardson’s diffusion. We show that these multiscale flows abide with Corrsin’s estimation of the Lagrangian integral time scale,
T
L
, as proportional to the Eulerian (integral) time scale,
L
E
∕
u
rms
, even though Corrsin’s approach was originally constructed for high Reynolds number turbulence. We check and explain why this relation is verified in our flows. The Lagrangian energy spectrum,
Φ
(
w
)
, presents a plateau at low frequencies followed by a power-law energy spectrum
Φ
(
w
)
∼
w
−
α
at higher ones, similarly to turbulent flows. Furthermore,
Φ
(
ω
)
scales with
L
E
and
u
rms
with
α
>
1
. These are the key elements to obtain such a relation [
Φ
(
w
)
∼
ϵ
w
−
2
is not necessary] as in our flows the dissipation rate varies as
ϵ
∼
u
rms
3
∕
L
E
Re
λ
−
1
. To complete our analysis, we investigate a recently proposed relation [M. A. I. Khan and J. C. Vassilicos, Phys. Fluids
16, 216 (2004)] between Eulerian and Lagrangian structure functions, which uses pair-diffusion statistics and the implications of this relation on
Φ
(
ω
)
. Our results support this relation,
⟨
[
u
L
(
t
)
−
u
L
(
t
+
τ
)
]
2
⟩
=
⟨
[
u
E
(
x
)
−
u
E
(
x
+
Δ
2
¯
(
τ
)
e
)
]
2
⟩
, which leads to
α
=
γ
∕
2
(
p
−
1
)
+
1
. This Eulerian-Lagrangian relation is striking as in the present flows it is imposed by the multiscale distribution of stagnation points, which are an Eulerian property. |
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ISSN: | 1070-6631 1089-7666 |
DOI: | 10.1063/1.2754348 |