Abstract
The small-scale structure of grid turbulence is studied primarily using data obtained
with a transverse vorticity (ω3) probe for values of the Taylor-microscale Reynolds
number Rλ in the range 27–100. The measured spectra of the transverse vorticity
component agree within ±10% with those calculated using the isotropic relation over
nearly all wavenumbers. Scaling-range exponents of transverse velocity increments are
appreciably smaller than exponents of longitudinal velocity increments. Only a small
fraction of this difference can be attributed to the difference in intermittency between
the locally averaged energy dissipation rate and enstrophy fluctuations. The anisotropy
of turbulence structures in the scaling range, which reflects the small values of Rλ,
is more likely to account for most of the difference. All four fourth-order rotational
invariants Iα (α = 1 to 4) proposed by Siggia (1981) were evaluated. For any particular
value of α, the magnitude of the ratio Iα / I1 is approximately constant, independently
of Rλ. The implication is that the invariants are interdependent, at least in isotropic
and quasi-Gaussian turbulence, so that only one power-law exponent may be sufficient
to describe the Rλ dependence of all fourth-order velocity derivative moments in this
type of flow. This contrasts with previous suggestions that at least two power-law
exponents are needed, one for the rate of strain and the other for vorticity.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Cited by
98 articles.
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