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contributor authorGrأ©a, Benoأ®t
contributor authorBurlot, Alan
contributor authorGriffond, Jأ©rأ´me
contributor authorLlor, Antoine
date accessioned2017-05-09T01:29:39Z
date available2017-05-09T01:29:39Z
date issued2016
identifier issn0098-2202
identifier otherfe_138_07_070904.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/161384
description abstractThe present work aims at expanding the set of buoyancydriven unstable reference flows—a critical ingredient in the development of turbulence models—by considering the recently introduced “Unstably Stratified Homogeneous Turbulenceâ€‌ (USHT) in both its selfsimilar and transient regimes. The previously established accuracy of an anisotropic EddyDamped QuasiNormal Markovian Model (EDQNM) on the USHT has allowed us to: (i) build a data set of well defined transient flows from Homogeneous Isotropic Turbulence (HIT) to latetime selfsimilar USHT and (ii) on this basis, calibrate, validate, and compare three common ReynoldsAveraged Navier–Stokes (RANS) mixing models (twoequation, Reynolds stress, and twofluid). The model calibrations were performed on the selfsimilar flows constrained by predefined long range correlations (Saffman or Batchelor type). Then, with fixed constants, validations were carried out over the various transients defined by the initial Froude number and mixing intensity. Significant differences between the models are observed, but none of them can accurately capture all of the transient regimes at once. Closer inspection of the various model responses hints at possible routes for their improvement.
publisherThe American Society of Mechanical Engineers (ASME)
titleChallenging Mix Models on Transients to Self Similarity of Unstably Stratified Homogeneous Turbulence
typeJournal Paper
journal volume138
journal issue7
journal titleJournal of Fluids Engineering
identifier doi10.1115/1.4032533
journal fristpage70904
journal lastpage70904
identifier eissn1528-901X
treeJournal of Fluids Engineering:;2016:;volume( 138 ):;issue: 007
contenttypeFulltext


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