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- W2895035144 abstract "The purpose of this research paper is to investigate the third-order moments of velocity fluctuations, turbulent kinetic energy (TKE) fluxes, turbulence dissipation rate, turbulent length scales, and Reynolds stress anisotropy in the wake regions over two artificial upstream-facing bed forms. For the structure having a smaller flow-facing slope (slanting forward-facing structure, named as SFFS), the maximum flow intermittency is 0.6% with a maximum flow reversal frequency of 0.24 Hz, whereas for the greater flow-facing sloped structure (vertical forward-facing structure, named as VFFS), up to 70% flow intermittency is noticed just downstream of the corresponding crest location with a maximum of 28 Hz flow reversal frequency. A strong negative M30 (stream-wise flux of stream-wise normal stress) and a strong positive M03 (vertical flux of vertical normal stress), implying the occurrence of ejection events, take place above the flow separation region along the generated shear layer. However, near the lee-surface, positive M30 and negative M03 imply the presence of sweep events. For both the cases, maximum of normalized TKE (κ) is generated in the vicinity of crest location, which spread over the retarding flow region near-bed of the trough and wake-flow region downstream of the crest. The production of turbulence is mainly concentrated at the interface of intense ejection and sweep dominated zones over the trough region for the VFFS case, and for the other bed form, i.e., SFFS case, maximum turbulence production is concentrated at the near-bed crest location. Near the bed, the length-scale of eddies in the inertial sub-range decreases substantially compared to that in the upstream. It is seen that in the region of negative kinetic energy production, local maximum anisotropy is found, especially for b11,22,33S and b11,22,33V components. Interestingly, at the corresponding crest points for SFFS and VFFS, maximum affinity toward the one-component isotropy is measured almost throughout the vertical height. However, a clear increasing trend in the affinity to a better isotropy; i.e., the three-dimensional isotropy is identified as the vertical height increases up to z ≈ 3 cm above the bed when a fair downstream location for the VFFS case is considered. A special look toward the investigation of possible connection of the flow region with negative TKE production with the stream anisotropy shows that a substantial increase in the degree of anisotropy (Ad) in the anisotropy invariant maps of the negative TKE production takes place for both the cases, when compared to that for the positive TKE production region." @default.
- W2895035144 created "2018-10-12" @default.
- W2895035144 creator A5029696262 @default.
- W2895035144 creator A5075818279 @default.
- W2895035144 date "2018-10-01" @default.
- W2895035144 modified "2023-09-27" @default.
- W2895035144 title "Higher-order moments with turbulent length-scales and anisotropy associated with flow over dune shapes in tidal environment" @default.
- W2895035144 cites W1534253835 @default.
- W2895035144 cites W1560344122 @default.
- W2895035144 cites W1874839958 @default.
- W2895035144 cites W1907005196 @default.
- W2895035144 cites W1963842207 @default.
- W2895035144 cites W1966054558 @default.
- W2895035144 cites W1969672769 @default.
- W2895035144 cites W1970201018 @default.
- W2895035144 cites W1979321080 @default.
- W2895035144 cites W1981220015 @default.
- W2895035144 cites W1982318229 @default.
- W2895035144 cites W1988033442 @default.
- W2895035144 cites W1988666490 @default.
- W2895035144 cites W1989696804 @default.
- W2895035144 cites W1992366866 @default.
- W2895035144 cites W1999973399 @default.
- W2895035144 cites W2003510539 @default.
- W2895035144 cites W2006949077 @default.
- W2895035144 cites W2008179361 @default.
- W2895035144 cites W2010684968 @default.
- W2895035144 cites W2011044663 @default.
- W2895035144 cites W2014687122 @default.
- W2895035144 cites W2021225242 @default.
- W2895035144 cites W2021586222 @default.
- W2895035144 cites W2022075119 @default.
- W2895035144 cites W2029870271 @default.
- W2895035144 cites W2032220583 @default.
- W2895035144 cites W2034420071 @default.
- W2895035144 cites W2039552460 @default.
- W2895035144 cites W2046579301 @default.
- W2895035144 cites W2048269543 @default.
- W2895035144 cites W2052994945 @default.
- W2895035144 cites W2058851979 @default.
- W2895035144 cites W2064027308 @default.
- W2895035144 cites W2072845767 @default.
- W2895035144 cites W2073344806 @default.
- W2895035144 cites W2073713430 @default.
- W2895035144 cites W2083782750 @default.
- W2895035144 cites W2083859746 @default.
- W2895035144 cites W2089444415 @default.
- W2895035144 cites W2091790167 @default.
- W2895035144 cites W2092941459 @default.
- W2895035144 cites W2096194863 @default.
- W2895035144 cites W2099436805 @default.
- W2895035144 cites W2100278556 @default.
- W2895035144 cites W2101003809 @default.
- W2895035144 cites W2108726848 @default.
- W2895035144 cites W2116600346 @default.
- W2895035144 cites W2124280244 @default.
- W2895035144 cites W2133342843 @default.
- W2895035144 cites W2135259685 @default.
- W2895035144 cites W2139733637 @default.
- W2895035144 cites W2140683366 @default.
- W2895035144 cites W2145352299 @default.
- W2895035144 cites W2146995034 @default.
- W2895035144 cites W2149137816 @default.
- W2895035144 cites W2150067632 @default.
- W2895035144 cites W2151450119 @default.
- W2895035144 cites W2156060709 @default.
- W2895035144 cites W2196378260 @default.
- W2895035144 cites W2283133421 @default.
- W2895035144 cites W2313671713 @default.
- W2895035144 cites W2583151699 @default.
- W2895035144 cites W2601901956 @default.
- W2895035144 cites W2682374212 @default.
- W2895035144 cites W2102598138 @default.
- W2895035144 doi "https://doi.org/10.1063/1.5038433" @default.
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