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The existence of a main flow channel induces short-circuiting, which reduces hydraulic and treatment efficiency.
Results show that increasing sinuosity of the main flow channel can promote mixing and improve hydraulic efficiency.
There is no motor magnet inside the main flow channel, therefore, more blood can pass through it.
Recent studies have shown that the hydraulic performance of a wetland can be significantly affected by the presence of a main flow channel (MFC) where vegetation density is much lower than the average vegetation density in the wetland.
A conceptual wetland characterized by a main flow channel (MFC) and lateral vegetated zones (LVZs) is modeled here using a two-dimensional depth-averaged hydrodynamic and advection dispersion model.
The inner hole makes the main flow channel possible, while the gap between the inner end of the stator and the outer end of the cylinder magnet gives the shape of the tributary flow channel.
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Nanometer pore throats and microscopic capillary pore throats are the main flow channels for gas in tight sand.
Estimating the efficiency of contaminant removal of a wetland requires separate knowledge of the residence time statistics in the main flow channels, where the flow velocity is relatively higher, and in the more densely vegetated zones, where the velocity is smaller and most of the biochemical transformations occur.
However, in the proppant-shale experiment, a more uniform velocity field was the result of narrowing of the main flow channels.
Airflow predictions are very close by using the draft and the detailed CFD modeling because of the simple structure of two main flow channels.
Additionally, most of these fractures are water-bearing prior to stimulation and form the main flow channels after stimulation and during circulation (Dezayes et al. [2010] and references therein).
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