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Attributes of the large-scale coherent motions in a shear layer

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Abstract

PIV observations in a shear layer have been used to identify and characterize the discrete large-scale coherent motions (LSCMs) in the nominally self-preserving region: xo ≈ 450–610, of a shear layer. The LSCMs are given an objective definition wherein their centers are the (swirling flow pattern) nodes of the velocity-vector field as seen by an observer in the Galilean reference frame translating at an appropriately defined reference velocity. The statistical attributes of size, lateral location, and separation between these coherent motions (that exist in a single image) as well as their characteristic vorticity magnitude 〈ωmax〉 are reported.

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Notes

  1. One can imagine a collapsed sphere as a deflated balloon. The associated vector field that is imprinted on the deflated balloon surface must be the same on the two flattened sides; hence, the vector field must be tangent at the perimeter except for the portion of the perimeter at which a hole is present. The balloon’s stem demonstrates the presence of a hole. An important constraint on the topological definition of a hole is that the components of the vector field that exist at and that are normal to the opening are uniformly directed onto or away from the subject sphere.

  2. Stokes theorem: \( \oint_{\text{c}} {\vec{V} \cdot d\vec{S}} = \iint_{A} {(\nabla \times \vec{V}) \cdot \hat{n}dA} \).

  3. The term transverse is used to indicate the “z” direction for the x-streamwise, y-spanwise coordinate system associated with the xy plane PIV images.

  4. θ(x m) = 20 mm at the mid-point of the observational domain.

Abbreviations

C′:

Circulation contour limits (see Fig. 11)

L:

Data domain length (x − x u) (see Fig. 16)

N:

Topologically defined node (see Fig. 9a)

N′:

Topologically defined half-node

S:

Topologically defined saddle (see Fig. 9a)

S′:

Topologically defined half-saddle (see Fig. 9b)

\( \bar{u}(x,y) \) :

Average velocity at location (x, y) (see Fig. 5)

\( \tilde{u}(x,y) \) :

RMS velocity at location (x, y) (see Fig. 5)

U o :

Free stream streamwise velocity (see Fig. 5)

U c :

Convection velocity (see Eq. 4)

V e :

Entrainment flow velocity

x:

Streamwise (downstream) flow direction (see Fig. 2)

y:

Spanwise direction (see Fig. 2)

z:

Out-of-plane direction

δ:

Edge length of PIV data domain (see Fig. 11)

δ(x):

Displacement thickness

δy c :

Distance from y c to the 0.5 Isotach at x = x c (see Figs. 11 and 6)

\( \mathcal{L} \) :

Circulation contour (square) side length (see Fig. 11)

\( \mathcal{L}^{*} \) :

Circulation side length where the data domain edge is reached

θ(x):

Momentum thickness (see Eq. 1a)

θ0 :

Momentum Thickness at the separation lip (backstep)

\( \Upgamma (\mathcal{L}) \) :

Circulation contour value for a surface (square) of side length \( (\mathcal{L}) \) (see Eq. 9)

〈ω〉:

Spatially averaged z–component vorticity magnitude (see Eq. 10)

χsurface :

Topologically defined surface characteristic number (see Eqs. 3a, 3b)

0.13:

Isotach 13 (see Fig. 6)

1.0:

Isotach 100 (see Fig. 6)

c:

Circulation contour center location (see Fig. 11)

d:

Downstream (x-direction) data domain boundary (see Sect. 5.3)

m:

Mid-location (x-direction) of the data domain (see Sect. 5.3)

max:

Associated with the maximum value of 〈ω〉; see Sect. 5.3

min:

2δ × 2δ area “patches” of 3 × 3 discrete velocity field vectors (see Sect. 5.5)

o:

Free stream regions

u:

Upstream (x-direction) data domain boundary (see Sect. 5.3)

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Bade, K.M., Foss, J.F. Attributes of the large-scale coherent motions in a shear layer. Exp Fluids 49, 225–239 (2010). https://doi.org/10.1007/s00348-010-0842-z

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