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The k-ω model has the ability to accommodate the roughness effects as bed boundary conditions and is considered to be more accurate in assessing the boundary-layer properties (Suntoyo, 2006).
During the measurement of bubble size by a probe inserted into a fluidized bed, parts of some of the bubbles located near the bed boundary are not accessible to the probe.
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We invoke the effects of bed boundaries to explain additional pressure drop in the FTMs.
In contrast, fractures in the mudrock beds rarely penetrate beyond the bed boundaries into the adjacent carbonate beds.
Using these images, several features such as the natural fractures, bed boundaries, and faults can be discriminated.
Vertical fracture penetrations measured from the middle of chalk and limestone beds generally extend to and often beyond bed boundaries into the vertically adjacent mudrock beds.
(c) Basal boundary processes In contrast to a structure fully ruled by the fluid-phase dynamics, it has been suggested that the formation of DBs was controlled by the basal flow-bed boundary (Branney and Kokelaar 2002, Chap. 4).
Relatively high correlations were found among the van Genuchten model parameters and the bottom boundary condition (bed rock).
The vertical grid is only required near the flow bottom boundary to assess the boundary layer for the bed stress calculation.
The fluctuation of data may occur due to measurement error, change of roughness of the bottom boundary and due to change of bed elevation at the central section.
Further, seed distributions were altered in fragmented beds when compared to continuous beds, both within and directly outside the bed's boundaries.
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