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For steady rotation the flow around the solid particle is restrained in a relatively narrow region, whereas with translation the velocity field extends to large distances.
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In directions perpendicular to the accretor's rotation axis, the flow tends to flatten onto a disk because the rotation resists the inflow of the material.
Many techniques have been applied as the use of flow inserts, rough inner surfaces, internal fins and giving rotation in the flow [15].
A near vertical extraction of singlet oxygen is effected at the generator exit, followed by a 90° rotation of the flow forming a novel verti-horizontal COIL scheme.
However, once the fluid reaches this region and by development of rotation in the flow, as discussed above, a sudden disturbance is created at the boundary layer and its growth is stopped.
While the strong differential rotation of the flow for some Ro supplies significant ω effect, so far no states have been found with strong enough α effect to give self-sustaining dynamo action.
Groundwater flow patterns within the freshwater saltwater interface in coastal aquifers include rotation in the flow direction of saltwater that originates from the sea and circulates in the aquifer.
Computation results show that when the backward crooked elbow blades are used, the mixed stream that passes through the two blades produces a vortex in the positive direction which counteracts the attached vortex in the opposite direction due to the high-speed turbo rotation, making the flow steadier, thus improving both the grade efficiency and precision of the turbo classifier.
We present the method for computation of fluid flows that are characterized by the large degree of expansion/contraction and in which the fluid velocity is dominated by the bulk component associated with the expansion/contraction and/or rotation of the flow.
The above methods have been applied to boundary control by rotation of the flow around a circular cylinder and show 30 to 60% drag reduction, compared to the fixed cylinder configuration, for Reynolds numbers in the range from 200 to 1000.
The Coriolis force imparts rotation on the flow and arises as winds begin to flow in toward the lower pressure created by the pre-existing disturbance.
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