Abstract
To investigate the validity of
Kolmogoroff's theory of local isotropy, a series of turbulence measurements
have been made in the wake of a circular cylinder, and the results have been
compared with the predictions of the theory. Using a cylinder of 0.953 cm.
diameter in an air-stream of velocity 1,280 cm. sec.-1, measurements
have been made of the mean squares of the spatial derivatives in the
mean-stream direction of the three components of the turbulent velocity
fluctuation, and also of the skewness and flattening factors of the statistical
distributions of these derivatives. Observations were taken at three traverses
across the wake, respectively at 80, 120, and 160 cylinder diameters
down-stream from the cylinder. Except in the immediate neighbourhood of the
wake centre, the turbulent flow is observed to be intermittent, consisting of
regions of fully developed turbulent flow separated by comparatively sharp
boundaries from regions of almost completely laminar motion. If an
"intermittency factor " is introduced to describe this phenomenon,
and if inside each turbulent region local isotropy exists, then all the
experimental results are consistent with the theory of local isotropy, and in
agreement with previous measurements in flows possessing ordinary isotropy. It
is concluded that, within the boundaries of the turbulent regions, local
isotropy in the sense used by Kolmogoroff exists, and that the theory is
applicable to this example of shear flow. The general applicability of the
theory to turbulent shear flow at high Reynolds numbers must be considered very
probable.
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