2006
DOI: 10.1017/s0022112005007688
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Numerical experiments on the intermediate asymptotics of shear-free turbulent transport and diffusion

Abstract: A numerical experiment on the interaction between different decaying homogeneous and isotropic turbulence is described. In the absence of kinetic energy production, the intermediate asymptotics of the turbulent shear-free mixing layer can be observed. The first aim of the experiment is to verify the existence of the intermittency or of the Gaussian asymptotic state in the case of the absence, or weak presence, of a lengthscale gradient. The second aim is to analyse the effects that are due to the difference be… Show more

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Cited by 33 publications
(51 citation statements)
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“…In all flow configurations, the velocity mixing layer was observed to be highly intermittent and the velocity fluctuations in the x-direction have large skewness and kurtosis, see [13,14,24]. Across the mixing layer, the second, the third, and the fourth velocity moments collapse using a single lengthscale; the mixing width E , conventionally defined as the distance between the points with normalised energy (E(x, t) − E 2 (t))/(E 1 (t) − E 2 (t)) equal to 0.75 and 0.25.…”
Section: Passive Scalar Transport Across the Interfacementioning
confidence: 89%
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“…In all flow configurations, the velocity mixing layer was observed to be highly intermittent and the velocity fluctuations in the x-direction have large skewness and kurtosis, see [13,14,24]. Across the mixing layer, the second, the third, and the fourth velocity moments collapse using a single lengthscale; the mixing width E , conventionally defined as the distance between the points with normalised energy (E(x, t) − E 2 (t))/(E 1 (t) − E 2 (t)) equal to 0.75 and 0.25.…”
Section: Passive Scalar Transport Across the Interfacementioning
confidence: 89%
“…The coordinate Downloaded by [Heriot-Watt University] at 13:01 02 January 2015 system is chosen with the x-axis along the direction of the kinetic energy gradient, axes y 1 and y 2 along the homogeneous directions. The initial condition is obtained by matching two homogeneous and isotropic fields with the same integral scale but each with different turbulent kinetic energy as in [13,14]. In practice, the initial condition is generated as…”
Section: Methodsmentioning
confidence: 99%
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