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Exact(28)
In each case, the flow seems unlikely to slacken.
In the first case the flow is confined near the sphere whereas in the second case the flow extends up to the box plates.
In the other case the flow is reactive in the stagnation boundary layer.
In this case, the flow resulted in the northward advection of warm moist air that was captured in the Ny Alesund radiosonde data (Fig. 1 and Supplementary Figure 1).
In comparison with planar case, the flow deviations are largely contained with endwall profiling but closer to the endwall it enhances the overturning and secondary flow kinetic energy.
In this case, the flow is induced through a limestone-gravel-filled permeable reactive barrier to increase pH to near the optimum for aluminum hydroxide and chromium precipitation.
Similar(32)
In both cases, the flow of intelligence simply ends, and future collection can be seriously limited.
In all cases, the flow regime was laminar or in the transition region.
In those cases, the flow of mud normally continues for some time, similar to the way lava flows from a conventional volcano.
In both cases, the flow velocity in the fracture diminishes with time, due to a decrease in porosity.
As test cases, the flow in plane channels and over a periodic arrangement of hills is considered.
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