| 11. | Provided that Um is not too large, this velocity profile is stable to hydrodynamic perturbations.
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| 12. | Depth migration begins with time data converted to depth data by a spatial geological velocity profile.
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| 13. | Velocity profile of the Herschel Bulkley fluid for various flow indices " n ".
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| 14. | We can see in this image the developing velocity profile of a fluid entering a pipe.
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| 15. | A developed velocity profile in a duct that shows why polished surfaces have little effect on flow.
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| 16. | In this region the velocity profile develops and thus the flow is called the hydrodynamically developing flow.
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| 17. | The velocity profile is an equation to calculate the velocity based on a specific location in the flow.
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| 18. | The velocity profile will be non-uniform due to friction between the annulus wall and the fluid.
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| 19. | The fuller velocity profile of the turbulent boundary layer allows it to sustain the adverse pressure gradient without separating.
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| 20. | For all but the simplest of velocity profiles U, numerical or asymptotic methods are required to calculate solutions.
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