This dissertation presents the turbulence of multiphase plumes and tidal vortices by
studying and quantifying coherent structures that affect the dynamics of the flow. The
measurements presented in this dissertation were taken using particle image velocimetry
(PIV). After preprocessing the images and conducting the PIV analysis to get the final
velocity fields, the local swirl strength was used to identify coherent structures (vortices)
in the flow. This dissertation used the identified vortices to quantify the turbulent
properties of the flows.
The mean and turbulent properties of bubble plumes are found to be self-similar
within the measured air flow rates when appropriately nondimensionalized. The timeaveraged
velocity profile was shown to have a Gaussian distribution when
nondimensionalized by the centerline velocity and plume radius. The bubble plumes
were found to have the most energetic vortices along the plume edge and a modulated
turbulent energy spectrum with a slope in the inertial subrange from -7/6 instead of the
classical -5/3.
The mean and turbulent properties of an inertial particle plume are presented,
revealing the time-averaged velocity and vorticity profiles to be self-similar for all cases
when nondimesionalized by the centerline velocity and plume radius. The average
vortex properties were not self-similar for all flow cases with the largest two particles
sizes being self-similar and the smallest particle vortex properties being similar to
bubble plume data. Despite the difference in vortex properties, the turbulent energy
spectra in inertial particle plumes followed the same modulation as the bubble plumes.
PIV experiments from the tidal starting-jet vortices detail the influence of a finite
channel length using identified vortice. The results show the trajectory and development
of the tidal starting-jet vortices to be changed by a region of vorticity that develops
inside the channel and is expelled as a vortex during the ebb tide. This expelled lateral
boundary layer vortex is shown to move the starting-jet vortex away from the tidal jet
shear layer thus reducing the input vorticity. When the expelled boundary layer vortex
strength is 1/5 the starting-jet vortex the system dynamics change resulting in a deviation
in the starting-jet vortices' trajectory.
This dissertation successfully uses the local swirl strength to quantify the
turbulence of multiphase plumes and tidal starting-jet vortices. Using these results,
engineers will be able to better predict the efficiency of CO2 ocean sequestration and
tidal flushing. Furthermore, the techniques of quantifying coherent structures developed
in this dissertation can be applied to a multitude of turbulent flows.
| Identifer | oai:union.ndltd.org:tamu.edu/oai:repository.tamu.edu:1969.1/ETD-TAMU-2010-05-7893 |
| Date | 2010 May 1900 |
| Creators | Bryant, Duncan Burnette |
| Contributors | Socolofsky, Scott A. |
| Source Sets | Texas A and M University |
| Language | en_US |
| Detected Language | English |
| Type | thesis, text |
| Format | application/pdf |
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