On viscoelastic eddy viscosity for flow
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John Miles
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Article
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1996
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Springer
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English
โ 150 KB
adopts a gradient-diffusion form for Z, whilst Bradshaw et al. (1967) argue against such a form; however, the modifications of the present (Z = 0) results implied by either Townsend's Z or that of Bradshaw et al. are relatively small.