Pregled bibliografske jedinice broj: 242784
Enhancement of mixing processes in semi-deep coastal channels by a bathymetry change
Enhancement of mixing processes in semi-deep coastal channels by a bathymetry change // Environmental Hydraulics / Lee, J.H.W. ; Lam, K.M. (ur.).
London : Delhi: A.A. Balkema Publishers, 2005. str. 297-302 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
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Naslov
Enhancement of mixing processes in semi-deep coastal channels by a bathymetry change
Autori
Ravlić, Nenad
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Environmental Hydraulics
/ Lee, J.H.W. ; Lam, K.M. - London : Delhi : A.A. Balkema Publishers, 2005, 297-302
Skup
4th International Sysmposium on Environmental Hydraulics & the 14th Congress of Asia & Pacific Division IAHR
Mjesto i datum
Hong Kong, Kina, 15.12.2004. - 18.12.2004
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
stratified flow; coastal channels; shallow sill; mixing; homogenization; 3-D modeling
Sažetak
Recent investments in construction of a number of submarine outfalls in Croatia pushed the local scientific community to focus attention to hydrodynamics of numerous stratified semi-deep (60-80 m) coastal channels in the Eastern Adriatic, which are planned to receive important quantities of partially treated wastewater in the near future. In some cases, however, simple channel geometry is complicated by bottom irregularities which are suspected to be the main cause of enhancement of mixing rates between different layers of stratified fluid. As a consequence, partial or complete destruction of typical density stratification can result in sur-facing of intermediate layers, where trapping of wastewater mixture is expected in normal oceanographic conditions. In order to examine hydrodynamics in the zone affected by a bathymetry change, the 3-D numerical model has been set up and tested in the channel where sea bottom irregularity, extending perpendicularly to the shore, encompasses one half of the channel width. Beside phenomenological description of this type of stratified flow, obtained re-sults are compared with known functional relationships governing turbulent interfacial mixing in layered flows.
Izvorni jezik
Engleski
Znanstvena područja
Fizika, Građevinarstvo
POVEZANOST RADA
Ustanove:
INSTITUT IGH, d.d.