https://ogma.newcastle.edu.au/vital/access/ /manager/Index ${session.getAttribute("locale")} 5 https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:27921 Sat 24 Mar 2018 07:36:07 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:30078 Sat 24 Mar 2018 07:31:16 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:30203 q² diffusion term is negligible compared to advection term along the axis and the advection and energy dissipation terms dominate the budget. However, in the CC wake, aside from the advection and energy dissipation terms, the q² diffusion term also contributes significantly to the budget. At the region close to the centreline, the gain of the energy due to the contributions from the advection and diffusion terms is equal to the loss due to the isotropic dissipation, indicating that the isotropic dissipation rate ε iso is a good surrogate of the mean TKE dissipation rate ε.]]> Sat 24 Mar 2018 07:31:04 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:28196 0.95−y_0.10) is in the range of 6560 ≤ Re_δ(=U_sδ/ν)≤ 12540, where U_s is the velocity difference between the high and low speeds. The measurements show that the mixing layer thickness δ grows linearly with x. The mean velocity profiles (U) collapse relatively well at all stations when the distance y is normalised by the variable η(=(y−y_0.50)/δ). Further, the Reynolds stress profiles at x/M₁=60 and 65 collapse well suggesting that the decaying turbulent in the SML has reached self-preservation.]]> Fri 14 Jul 2017 14:28:59 AEST ]]>