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Mixing intensity of the liquid phase was characterized by both exchange flows and homogenization times.
The aim of this paper is to assess the effect of the CDW on exchange flows and sediment fluxes.
Exchange flows between the dock and the Scheldt are mainly a combination of horizontal eddies and salinity-driven flows, with velocities around 0.4 m/s.
This method allows exchange flows with two groups of layers to be solved for the same set of geometries that the pure two-layer theory can handle, including sill contraction combinations and non-rectangular cross-sections.
Determining this effect requires (1) understanding and reproduction of the sediment dynamics close to the Deurganckdok, and (2) accurate reproduction of the exchange flows between the dock and the Scheldt, and the effect of the CDW thereon.
Gas hold-up, mixing intensity of dispersion characterised by exchange flows between adjacent impellers and a volumetric mass transfer coefficient are presented for 18 impeller configurations in triple-impeller vessel of inner diameter 0.29 m.
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With Okwui Okpokwasili, who had tubes hooked up to cups on her breasts, the exchange flowed in the other direction.
Impeller energy dissipation ratio, impeller exchange flow rate and baffle exchange flow rate increased while baffle volume ratio decreased with agitation rate and impeller diameter.
However, it is shown here that the experiments can also be used to give the exchange flow rate between zones.
The exchange flow rate between two neighbouring modules V̇exchange related to the connecting area remains constant during the scale-up.
Using the numerical model, we examined the dynamics in stage, water depth, discharge from hydraulic structures along the canal, and exchange flow among canal and marsh compartments.
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