Civil Engineering Reference
In-Depth Information
Robinson [ROB 91a and ROB 91b] was the first to carry
out a rigorous and methodical examination of the DNS
performed by Spallart [SPA 88]. He essentially based that
examination on the low-pressure zones to identify the
structures (see Figure 4.1). This approach is obviously
questionable, in view of our discussions from the previous
chapter. Various structures, such as quasi-streamwise
vortices (QSVs), HPVs or arc structures, were observed (as
Figure 4.2 illustrates). Yet HPVs represent only 9% of the
structures detected (see Figure 4.3). The arc structures are
most common. QSVs, for their part, account for around one-
third of the vortices detected.
Figure 4.2. Different structures identified by Robinson [ROB 91b]
and the quadrant events associated therewith
Jeong et al. [JEO 97] estimated that no vortices exist at
. They used the lambda-2 technique to detect the
structures. First, they determined the distribution of the
y +
<
10
(
)
1/ 2
()
2
mean value
and the RMS value
λλλ
'
=−
2
in
λ
2
2
2
2
the inner lay er . Their results are shown in Figure 4.4. We
can see that
at
y +
and that it is also comparable
λ 2 >
0
<
10
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