FLOW VISUALIZATION AND FLUID-STRUCTURE INTERACTION ... …

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FLOW VISUALIZATION AND FLUID-STRUCTURE INTERACTION OF TORNADO-LIKE VORTICES by JOHN LYLE FOUTS, B.S.M.E. A THESIS IN MECHANICAL ENGINEERING Submitted to the Graduate Faculty of Texas Tech University in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE IN MECHANICAL ENGINEERING Approved December, 2003

Transcript of FLOW VISUALIZATION AND FLUID-STRUCTURE INTERACTION ... …

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FLOW VISUALIZATION AND FLUID-STRUCTURE

INTERACTION OF TORNADO-LIKE VORTICES

by

JOHN LYLE FOUTS, B.S.M.E.

A THESIS

IN

MECHANICAL ENGINEERING

Submitted to the Graduate Faculty of Texas Tech University in

Partial Fulfillment of the Requirements for

the Degree of

MASTER OF SCIENCE

IN

MECHANICAL ENGINEERING

Approved

December, 2003

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ACKNOWLEDGEMENTS

I would like to thank my advisors, Dr. Darryl L. James and Dr. Chris

Letchford, for their continued guidance and support throughout this project. I

would also like to thank the State of Texas and the Wind Science and

Engineering Research Center at Texas Tech University for their support of this

research. I also would like to thank Mr. Matthew Mason for his help with the

experiments and other support. Finally, I would like to thank my wife for her

support and help during the pursuit of this endeavor.

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TABLE OF CONTENTS

ACKNOWLEDGEMENTS II

ABSTRACT v

LIST OF TABLES vll

LIST OF FIGURES vill

CHAPTER 1

1 INTRODUCTION 1

L1 Background 1

^.2 Literature Review 3

1.2.1 Simulators 3

1.2.2 Measurements 8

1.2.3 Numerical Analysis 11

1.2.4 Conclusions and Objectives 14

2 EXPERIMENTAL SETUP 16

2.1 Design Criterion 16

2.2 Simulator 17

3 EXPERIMENTAL PROCEDURE 20

3.1 Principles of Operation 20

3.2 Procedures 25

3.3 Flow Visualization 25

3.4 Measurement Techniques 26

3.5 Uncertainty Analysis 27

4 RESULTS AND DISCUSSION 29

4.1 Flow Visualization 29

4.2 Pressure Measurements 46

4.2.1 Models 46

4.2.2 Orientation 47

1.1 Stationary Force Distributions 49

III

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4.2.3 Cube Model 53

4.2.4 Cylinder Model 65

4.3 Transient Analysis 75

4.3.1 Transient Cube 76

4.3.2 Transient Cylinder 90

4.4 Statistical Analysis 104

5 CONCLUSIONS AND RECOMMENDATIONS 107

5.1 Conclusions 107

5.2 Recommendations I l l

REFERENCES 112

APPENDIX A 115

IV

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ABSTRACT

A Ward-type tornado simulator has been built using a configuration of 16

slotted jets instead of a rotating screen to create the required far field circulation

needed to produce a tornado4ike vortex. Flow visualization data, velocity data

and pressure data were all obtained using the simulator. The produced vortices

observed ranged from a laminar, rope-like, single-celled vortex to a turbulent,

much larger diameter, two-celled vortex. Helium bubbles were used to visualize

the vortices in the convergent region of the tornado simulator. At a=0.5, the low

swirl ratios (the ratio of the tangential flow rate to the updraft flow rate) calculated

were s=2.23 and at a=1 s=1.51. The high swirl ratios calculated were s=8.03 at

a=0.5 and s=6.72 at a=1. The swirl ratios calculated are unique to the TTU TVS

II.

The initial vortex configuration in the TTU TVS II was that of a single-

celled vortex. During flow visualization, as the swirl ratio was Increased, a

breakdown bubble was observed moving down the vortex core region toward the

surface of the simulator. Once the breakdown bubble has traversed the vortex

core to the surface of the simulator, the vortex is defined as two-celled. The TTU

TVS II was capable of producing single-celled and two-celled vortices.

Pressure data was obtained on cubical and cylindrical models that were

positioned at various radial locations within the simulator. The models were also

subjected to moving tests through the TTU TVS II In order to compare the

stationary data to the moving data. Using the pressure data, non-dimensional

force coefficients were calculated and contour plots of the force coefficients on

the cube and cylinder were generated for the stationary tests while, for the

moving tests, specific points on the models were chosen, and the force

coefficients at these points were plotted as a function of position In the TTU TVS

II. The stationary tests show that both the cube and the cylinder models

experience flow regimes at different points In the TTU TVS II similar in pattern to

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those induced by boundary layer-type flows, but mainly towards the outer regions

ofthe simulator in low swirl cases (s=2.23 and s=1.51). Also for the cylinder, the

contour plots indicate a horseshoe vortex forms around the cylinder. At the

center of the simulator, both the cylinder and the cube disrupt the flow field

significantly, and at this point, the flow field is very complex and at the present

time the experimental equipment and data are not sufficient to quantify the flow In

this region. The leading and trailing edges of the roof as well as the leading and

trailing sides of each model were chosen and force coefficients were calculated

and plotted as a function of radial position In the TTU TVS II for the moving tests.

Each of these moving tests had approximately the same trends for the leading

edge and side and the trailing edge and side with a few exceptions. The

stationary test data followed the trends of the moving test data In most cases

tested. This would mean that less significance could be placed on the much

more complicated moving tests and more significance on the less complicated

stationary tests In future testing

Limited statistical analysis was also performed on the obtained data sets.

This showed that standard deviation for all cases Is very small, so the distribution

should be concentrated towards the center of the normal distribution. Most of the

skewness values are negative Indicating the normal distribution is skewed to the

right of the centerllne and slow, Infrequent variations In pressure below the mean.

Very high kurtosis values like the ones shown for the center of the roof of the

cylinder at the center of the simulator indicate an Increase In the high-frequency

content ofthe fluctuating pressure signals read.

VI

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LIST OF TABLES

0-1: Likely range of non-dimensional parameters 20

3-2: Velocity, Turbulence Intensity 24

3-3: Calculated Swirl Ratios 24

4-1: Scale Factors Between Simulated Vortex and Actual Vortex 47

4-2: Velocity Scale Factor Range In TTU TVS II 75

4-3: Cube Model Percent Error from Average Velocity 76

4-4: Cylinder Model Percent Error from Average Velocity 90

4-5: Statistical Values at Center of Roof on Cube and Cylinder at Center of

Simulator 105

|4-6: Statistical Values at Center of Roof on Cube and Cylinder at 2.0*ro in

Simulator 105

4-7: Statistical Values on North Face of Cube and Cylinder at Center of Simulator

105

4-8: Statistical Values on North Face of Cube and Cylinder at 2.0*ro in Simulator

106

4-9: Statistical Values on South Face of Cube and Cylinder at Center of

Simulator 106

|4-10: Statistical Values on South Face of Cube and Cylinder at 2.0*ro In

Simulator 106

VII

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LIST OF FIGURES

n- l : Ward-Type Tornado Simulator (Ward, 1972) 4

2-1: Texas Tech University Tornado Vortex Simulator II 19

2-2: Dimensions of TTU TVS II (Plan View) 19

0-1: Jet Velocity Profile (a=0.5, Low Swirl) 22

0-2: Jet Velocity Profile (a=0.5, High Swirl) 22

0-3: Jet Velocity Profile (a=1. Low Swirl) 23

0-4: Jet Velocity Profile (a=1. High Swirl) 23

f^-^•. start of Vortex Formation (a=0.5) 30

[4-2: Progression of Vortex Formation (a=G.5) 31

n-3: Single-Celled Vortex (a=1, LowSwIri, s=1.51) 31

M : Scale of Inner Cone of Single-celled Vortex (a=0.5. Low Swirl, s=2.23).... 32

|4-5: Scale of Single-Celled Vortex (a=1, Low Swirl, s=1.51) 33

^-6: Vortex with Helium Bubbles and Smoke (a=0.5, Low Swirl, s=2.23) 33

n-7: Two-Celled Vortex (a=1, High Swirl, s=6.72) 34

n-8: Scale of Two-Celled Vortex (a=0.5, High Swirl, s=8.03) 35

|4-9: Flow Visualization with Cube in Center (a=0.5, Low Swiri, s=2.23) 36

|4-10: Flow Visualization with Cube in Center (a=1, Low Swirl, s=1.51) 36

|4-11: Flow Visualization with Cube in Center (a=1, Low Swirl, s=1.51) 37

14-12: Flow Visualization with Cube Offset (a=0.5, Low Swirl, s=2.23) 38

n-^3: Flow Visualization with Cube Offset (a=0.5, Low Swirl, s=2.23) 38

14-14: Flow Visualization with Cube Offset (a=1, LowSwIri, s=1.51) 39

[4-15: Flow Visualization with Cube In Center (a=0.5. High Swiri, s=8.03) 40

[4-16: Flow Visualization with Cube in Center (a=1, High Swirl, s=6.72) 41

^-17: Flow Visualization with Cube Offset (a=0.5, High Swirl, s=8.03) 41

[4-18: Flow Visualization with Cube Offset (a=0.5. High Swiri, s=8.03) 42

^-^9•. Flow Visualization with Cube Offset (a=1, High Swiri, s=6.72) 42

p -20: Flow Visualization with Cylinder In Center (a=1, LowSwIri, s=1.51) 43

Vlll

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14-21: Flow Visualization with Cylinder in Center (a=1, High Swiri, s=6.72) 44

F -22: Flow Visualization with Cylinder Offset (a=1, Low Swiri, s=1.51) 45

P4-23: Flow Visualization with Cylinder Offset (a=1. High Swiri, s=6.72) 45

FI-24: Schematic of Model Cube and Cylinder 46

pi-25: Schematic of Surface of Tornado Simulator 48

[4-26: Positions where Models were Tested in Simulator 49

M 7 : Surface Pressure Profile for a=0.5, s=2.23 51

Ft-28: Surface Pressure Profile for a=0.5, s=8.03 51

[4-29: Suri ace Pressure Profile for a=1, s=1.51 52

[4-30: Surface Pressure Profile for a=1, s=6.72 52

^ -31 : Exploded View of Cubical Model 54

^-32: Force Coefficients on Cube at 2.0*ro (Point 1) in Simulator (a=0.5, s=2.23)

56

Fl-33: Force Coefficients on Cube at LOVo (Point 6) in Simulator (a=0.5, s=2.23)

57

[4-34: Force Coefficients on Cube at 2.0*ro (Point 1) In Simulator (a=0.5, s=8.03)

59

[4-35: Force Coefficients on Cube at 0.5*ro (Point 10) In Simulator (a=1, s=6.72)

59

Fl-36: Force Coefficients on Cube at 0.25*ro (Point 12) In Simulator (a=0.5,

s=8.03) 61

[4-37: Force Coefficients on Cube at 0.125*ro (Point 18) in Simulator (a=0.5,

s=2.23) 62

^-38: Force Coefficients on Cube at 0.0625*ro (Point 15) In Simulator (a=0.5,

s=2.23) 63

pt-39: Force Coefficients on Cube at Center (Point 16) of Simulator (a=1, s=6.72)

64

[4-40: Schematic of Exploded Cylinder 65

IX

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M l : Force Coefficients on Cylinder at 2.0% (Point 1) In Simulator (a=1, s=6.72)

67

14-42: Force Coefficients on Cylinder at I.OVo (Point 6) in Simulator (a=0.5,

s=8.03) 67

14-43: Force Coefficients on Cylinder at 0.5*ro (Point 10) In Simulator (a=0.5,

s=2.23) 68

M 4 : Force Coefficients on Cylinder at 0.25*ro (Point 12) in Simulator (a=1,

s=1.51) 68

Fi-45: Force Coefficients on Cylinder at 0.125*ro (Point 14) in Simulator (a=0.5,

s=2.23) 70

[4-46: Force Coefficients on Cylinder at 0.125*ro (Point 14) in Simulator (a=1,

s=6.72) 70

|4-47: Force Coefficients on Cylinder at Center (Point 16) in Simulator (a=0.5,

s=2.23) 72

[4-48: Force Coefficients on Cylinder at Center (Point 16) in Simulator (a=1,

s=6.72) 73

F*-49: Force Coefficients on Cylinder at 0.0625*ro (Point 17) In Simulator (a=0.5,

s=8.03) 73

14-50: Force Coefficients on Cylinder at 0.0625*ro (Point 17) In Simulator (a=1,

s=1.51) 74

^ - 5 1 : Force Coefficients at Leading Edge on Roof of Cube (a=0.5, s=2.23) 78

[4-52: Force Coefficients on Trailing Edge on Roof of Cube (a=0.5, s=2.23) 79

[4-53: Force Coefficients on Center of Leading Face of Cube (a=0.5, s=2.23).. 79

[4-54: Force Coefficients on Center of Trailing Face of Cube (a=0.5, s=2.23)... 80

|4-55: Force Coefficients on Leading Edge of Roof of Cube (a=0.5, s=8.03) 81

[4-56: Force Coefficients on Trailing Edge of Roof of Cube (a=0.5, s=8.03) 82

p^-57: Force Coefficients on Center of Leading Face of Cube (a=0.5, s=8.03).. 82

^-58: Force Coefficients on Center of Trailing Face of Cube (a=0.5, s=8.03)... 83

P4-59: Force Coefficients on Leading Edge of Roof of Cube (a=1, s=1.51) 84

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Ft-60: Force Coefficients on Trailing Edge of Roof of Cube (a=1, s=1.51) 85

[4-61: Force Coefficients on Center of Leading Face of Cube (a=1, s=1.51) 85

pt-62: Force Coefficients on Center of Trailing Face of Cube (a=1, s=1.51) 86

M 3 : Force Coefficients on Leading Edge of Roof of Cube (a=1, s=6.72) 87

^-64: Force Coefficients on Trailing Edge of Roof of Cube (a=1, s=6.72) 87

(4-65: Force Coefficients on Center of Leading Face of Cube (a=1, s=6.72) 88

pi-66: Force Coefficients on Center of Trailing Face of Cube (a=1, s=6.72) 88

14-67: Force Coefficients on Leading Edge of Roof of Cylinder (a=0.5, s=2.23) 92

[4-68: Force Coefficients on Trailing Edge of Roof of Cylinder (a=0.5, s=2.23). 92

fA-69: Force Coefficients on Leading Side of Cylinder (a=0.5, s=2.23) 93

Ft-70: Force Coefficients on Trailing Side of Cylinder (a=0.5, s=2.23) 93

[4-71: Force Coefficients on Leading Edge of Roof of Cylinder (a=0.5, s=8.03) 95

|4-72: Force Coefficients on Trailing Edge of Roof of Cylinder (a=0.5, s=8.03). 95

[4-73: Force Coefficients on Leading Side of Cylinder (a=0.5, s=8.03) '96

[4-74: Force Coefficients on Trailing Side of Cylinder (a=0.5, s=8.03) 96

[4-75: Force Coefficients on Leading Edge of Roof of Cylinder (a=1, s=1.51).... 98

[4-76: Force Coefficients on Trailing Edge of Roof of Cylinder (a=1, s=1.51) 98

[4-77: Force Coefficients on Leading Side of Cylinder (a=1, s=1.51) 99

[4-78: Force Coefficients on Trailing Side of Cylinder (a=1, s=1.51) 99

^-79: Force Coefficients on Leading Edge of Roof of Cylinder (a=1, s=6.72).. 101

[4-80: Force Coefficients on Trailing Edge of Roof of Cylinder (a=1, s=6.72)... 101

M 1 : Force Coefficients on Leading Side of Cylinder (a=1, s=6.72) 102

Ft-82: Force Coefficients on Trailing Side of Cylinder (a=1, s=6.72) 102

XI

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CHAPTER 1

INTRODUCTION

1.1 Background

In an average year, 800 tornadoes are reported nationwide, resulting In 80

deaths and over 1500 Injuries [1]. This makes the study of tornadoes very

important. Waterspouts, fire whiris, dust devils, and steam devils are other types

of small but intense vortical flows. A tornado Is defined as being a violently

rotating, tall, narrow column of air, averaging about 100m In diameter [2].

Tornadoes are produced within cumuliform clouds. Visually, a tornado consists

of a funnel-shaped cloud protruding out of the bottom of the cumuliform cloud

and is generally accompanied by a swiriing cloud of dust and debris which come

from the ground below the tornado. A funnel cloud is a tornado that does not

reach the ground. Tornadoes are classified in fluid flow dynamics as vortices,

which are flows with associated core of concentrated rotation. Tornadoes come

in many different shapes and sizes. The shapes range from a thin rope-like

shape to a large cone shape to multiple-vortices spinning around what appears

to be a central axis. Five discrete stages of the tornado life cycle are described

by Davies-Jones [2].

1. The dust-whiri stage, when the first signs of circulation are visible,

and a small vortical protrusion appears In the cloud above.

2. The organizing stage is the stage where the increase In Intensity of

the tornado is evident by an overall downward descent of the

funnel.

3. The mature stage is the stage where possible damage Is most

Intense. It is characterized by the funnel reaching its greatest width

and being almost vertical.

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4. The shrinking stage is the stage in which the tornado starts to loose

energy. It Is Indicated by an Increase In funnel tilt, a narrowing

damage swath, and decreasing funnel width.

5. The decay stage Is marked by the vortex being stretched into a thin

rope shape and becomes greatly contoured before dissipating.

The parent storm of a tornado Is two orders of magnitude In horizontal

dimension larger than the core of a tornado and its total energy and circulation

greatly exceed the energy and circulation associated with the tornado according

to Davies-Jones [2]. This Indicates that In order to find and predict

tomadogenesis, a thunderstorm with sufficient energy to produce a tornado must

be found. These thunderstorms are typically generated when warm, moist air

flows Into a building storm at low levels and rises through the storm. Evaporating

precipitation cools the drier air that surrounds the updraft of the storm, and this

cooler air sinks towards the ground. As it reaches the ground and starts to

spread out, it encounters the rising, warm, moist air and is drawn around the

warm air to form what Is now known as the leading edge of a thunderstorm

downdraft. As the downdraft gust propagates, It displaces and lifts the moist,

warm air In its path which feeds the generation of the thunderstorm. This cycle

continues to generate energy in the thunderstorm and eventually, If the

conditions are right, the updraft begins to rotate, and a tornado Is formed.

The problem with studying tornadoes in nature is the unpredictability and

the extreme danger of severe storms. The three other methods for studying

tornadoes are analytical work, numerical modeling, and experimental simulation.

Analytical work and numerical modeling are very difficult to perform due to the

nonlinearlty and uncertainty in the modeled equations and the lack of knowledge

of detailed real-worid boundary conditions. For such reason, a number of

different tornado simulators have been constructed over the last thirty to forty

years to try and mimic a tornadic wind field. These simulators try to create flows

that are dynamically and geometrically similar to natural atmospheric flow. YIng

and Chang presented one of the first known modern tornado vortex simulators in

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1969 [3]. They were followed by Ward In 1972 [4], Davies-Jones In 1973 [5],

Jlschke and Parang in 1974 [6], and Church, Snow and Agee In 1977 [7], Snow,

Church and Barnhart In 1979 [8], Church, Snow, Baker and Agee In 1979 [9], and

others since 1979. It was concluded by Davies-Jones after comparing different

configurations of tornado vortex simulators that the most appropriate apparatus

for tornado modeling is the Ward-type simulator developed by Ward In 1972 [4].

At Texas Tech, a Ward-type simulator has been constructed, but with slotted jets

to provide tangential acceleration instead of a mesh screen used In previous

simulators. These slotted jets allow for much easier access to the regions of

interest In the convergence region than the mesh screen does for obtaining

quantitative and qualitative data, namely pressure measurements, velocity

measurements, and flowfield visualization.

1.2 Literature Review

1.2.1 Simulators

Quite a bit of research went on in the 1960-1980's to produce an accurate

depiction of an actual tornado with the help of experimental tornado simulators.

Some of the first researchers to build a modern tornado vortex simulator were

YIng and Chang In 1969 [3]. They built an eariy model of what would later

become known as a Ward-type tornado simulator. YIng and Chang recognized

that there were two essential factors In producing a tornado vortex near the

ground, circulation and updraft. They produced circulation by rotating a

cylindrical wire screen, and they produced updraft by a separate exhaust fan

located at the top of their simulator. This configuration allowed YIng and Chang

to independently control the circulation and the updraft which, in later work,

proved essential to the control of the vortex size. YIng and Chang concluded

several things. First, that they could provide a controllable constant circulation

along the vortex axis with the rotating screen without Introducing an evident

secondary fiow, and that a complex buoyant effect could be avoided with the

suction fan located far above the hood opening. Second, that the pressure Is

neariy constant vertically in the turbulent ground boundary layer except In the 3

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region of the vortex core. Third, that it was not possible to carry out

measurements with probes at the present time in the complex flow at the foot of

the vortex without Introducing large errors. Fourth, that a successful mechanical

simulation of tornado-like vortices was evident by both the visual vortex core and

the reverse-flow funnel demonstrated with smoke visualization. Finally, that

above the boundary layer, the static pressure distribution and the tangential

velocity components depend mainly on the radius from the center of the

simulator and the circulation and only slightly on the vertical distance of the

confluent zone except for the vortex core region.

In 1972, Ward developed a tornado vortex simulator that would become

the standard for most experimental tornado research to date [4]. Ward's

apparatus (see Figure 1.1) was much the same as YIng and Chang, except that It

used a flow-straightening device at the top of the chamber that removed the

tangential component vorticity.

/ COLLECTION AREA

HONEYCOMB SECTION ^ ^ / I / 4 INCH MESH \ \ 3 / 4 INCH T H I C K ;

y EXHAUST

FAN

t CONVECTION CELL t

'A ^CONVERGENT \^ %^

ROTATING SCREEN

l / CONFLUENT

ZONE

/ DIRECTION

VANE I I- I FTH SCALE

Figure 1-1: Ward-Type Tornado Simulator (Ward, 1972)

Ward realized that there were three characteristic features of tornadoes

that he could simulate In a laboratory system. The three features were:

1. Characteristic surface pressure profile.

4

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2. Bulging deformation on the vortex core.

3. Multiple vortices in a single convergence system.

He found that (1) and (3) can be produced only when the diameter of the updraft

column Is greater that the depth of the Inflow layer in his model. Ward concluded

that the extreme radial pressure gradient accounts for centripetal acceleration,

and that air which was at a significantly higher potential temperature when the

vortex increases in scale could subside motion along the central axis. He also

said that these factors ((1) and (3) above) do not exist before vortex formation.

Ward also concluded that as a vortex forms, there is a large Influx of radial

momentum which can produce a force field such that a portion of the fluid mass

is required to converge against opposing centrifugal force plus any net outward

pressure.

Davies-Jones related the significance of core radius dependence to swiri

ratio In 1973 [5]. Davies-Jones used a Ward-type simulator to show that the non-

dimensional radius of the turbulent core in a tornado simulator Is primarily a

function of swiri ratio. This paper reinterprets Ward's data on turbulent core

radius, and concludes that volume flow rate is a much more important factor than

radial momentum flux In the production of Intense atmospheric vortices. Davies-

Jones also states that high-volume flow rate Is required for the production of

concentrated vortices for a given circulation and updraft radius. Also in 1974,

Jischke and Parang [6] showed that tornado-like vortices simulated In Ward-type

simulators show a systematic increase in core radius with Increased imposed

swiri and that an instability at a critical value of the imposed swiri causes the

usual single-celled vortex to undergo a transition to a two-celled vortex

configuration.

Church, Snow, and Agee created a four-meter wide and seven-meter tall

Ward-type tornado vortex generator In 1977 at Purdue University [7]. They

focused on laboratory simulation and study of tornado-like vortex features, with a

primary emphasis on quantitative investigation Into the nature and cause of the

multiple vortex phenomenon. The Purdue simulator demonstrated the ability to

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achieve vortex breakdown and multiple vortex formation, and offered the

possibility to obtain detailed Information about flow fields for various transitional

stages of vortex appearance and formation. This paper was followed up In 1979

with a second paper about the Purdue tornado simulator by Snow, Church, and

Barnhart [8]. They performed a series of laboratory experiments In the tornado

vortex simulator to obtain a better physical understanding of the mechanisms

producing the surface pressure fields recorded on barograph traces by Fujita [10]

and Ward [4]. Snow, Church, and Barnhart found that the surface pressure field

In the convergent region outside the central core is determined by two processes.

One Is radial Inertlal forces acting to decelerate the inflow by establishing a

region of higher pressure about the centerllne, and the other is the dynamic

pressure field Induced by the conservation of angular momentum acting to

produce a region of lower pressure about the centeriine. They also discovered

that the largest central-pressure deficits were found In single-celled vortices

characterized by Intermediate swiri ratio values, and that when two-celled

structures developed, the lowest pressures were found off-axis of the centeriine

in an annular region. They suggested that there Is a strong evidence of the

existence of a dynamically induced downdraft In the two-celled vortex.

Swiri ratio is one of the most important factors in tornado vortex

simulation. Church et al. helped to quantify this ratio In 1979 with the Purdue

tornado simulator [9]. They used a Ward-type simulator to observe five different

vortex configurations by varying the swiri ratio, the radial Reynolds number, and

the aspect ratio:

1. The single, laminar vortex or single-celled vortex.

2. The single-celled vortex with the upper turbulent region separated

from the lower laminar region by a breakdown bubble.

3. A fully developed turbulent core, where the breakdown bubble

penetrates to the bottom of the experimental chamber, joining the

two-celled vortex.

4. Vortex transition to two Intertwined helical vortices.

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5. Examples of higher order multiple-vortex configurations that form in

the core region.

They showed that as the angular momentum Increased, effectively Increasing

swiri ratio, the vortex evolved from a single-celled vortex to a two-celled vortex to

a multiple vortex configuration. This evolution Is characterized by the single-

celled vortex developing a "separation bubble" at the top of the vortex that

propagates towards the surface of the simulator as the swiri ratio Increased until

the bubble touches the surface and the vortex Is then characterized as two-

celled. They also Indicated that there was a downdraft in the center of the vortex

that penetrates to the level of the breakdown bubble and to the surface of the

simulator when the separation bubble touches the surface. It was also

concluded that the swiri ratio Is the parameter that primarily determines the core

configuration, not the aspect ratio or the radial Reynolds number.

The tornado simulator at Purdue University was updated in 1987 by Snow

and Lund [11]. The primary objective of the updated chamber was to construct

an apparatus suitable to take measurements of the radial and tangential

components of velocity in and near the core of tornado-like vortices using a Laser

Doppler Velocimeter (LDV). This simulator also used a vane assembly to create

swiri on the Incoming flow rather than using the traditional rotating wire screen.

In 1993, the American Geophysical Union published The Tornado: Its

Structure, Dynamics, Prediction, and Hazards' [12]. This book contains a vast

amount of information about tornadoes, and has a paper by Church and Snow on

laboratory models of tornadoes [13]. In this paper. Church and Snow compare

current and past tornado vortex simulators. All of the working tornado vortex

chambers discussed in this paper are variants of the Ward-type simulator and

use a system of vanes to produce circulation rather than a wire screen. The

working models of tornado simulators discussed are at Purdue University [11],

where the goal of the research was to Implement a LDV system to an updated

simulator, University of Oklahoma [14], where the goal of the research was to

quantify the effects of surface friction on rotating fluids, Kyoto University [15],

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where the research goal was to create multiple vortices and to study the

characteristics of tornado-like vortices on various surfaces, and at Miami

University in Ohio, where the goals were to study tornado-like vortices.

Davies-Jones compared different configurations of tornado simulators In

1976 [16]. His purpose was to comment critically on the relevancy of laboratory

experiments to tornadoes, and to assess their contributions to current knowledge

of tornado dynamics. Davies-Jones concluded that in 1976, high quality

measurements were still difficult to make due to the influences of probe

interference, vortex wander and extraneous perturbations. He also concluded

that Ward's model was probably the most realistic model as of 1976 due to Its

large exhaust radius and high Reynolds number which at a low aspect ratio and

a low swiri ratio appear to be the conditions necessary to simulate a tornado

vortex.

1.2.2 Measurements

There are two main types of data taken In a tornado vortex simulator,

velocity and pressure. Both of these measurements can be taken with or without

objects inside the flow field. Intrusive velocity measurements are taken using a

thermal anemometry system; within the past few decades, laser Doppler

velocimeters (LDV) and particle image veloclmetry (PIV) systems have been

employed due to their 'unobtrusive' nature. Lund and Snow used the second

generation Purdue University tornado vortex simulator to take LDV

measurements in tornado-like vortices [17]. They discussed radial and vertical

profiles of radial and vertical velocity component measurements and derived

vertical velocity components. Lund and Snow found that vertical and radial

profiles of radial and tangential velocity components reveal characteristic

boundary layer and vortex flow features. They found that the greatest tangential

speeds were in an annular volume of small radius and small radial width but

significant vertical extent, with large centrifugal accelerations and largest

pressure gradients occurring well aloft. They showed that LDV measurements

are an accurate means of collecting quantitative data about critical flow structure,

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but vortex wander hinders accurate measurement of the innermost core. Fiedler

and Rotunno theorized in 1985 that the most Intense laboratory vortex occurs

when the vortex Is in the form of an end-wall vortex or 'supercritical' vortex [18].

This is the vortex that forms upstream of the vortex breakdown 'bubble', and will

be described at length in section 4.1. They came up with a model for the

maximum Intensity of the vortices by modeling the end-wall vortex and finding the

criterion for vortex breakdown. Cleland performed axial vertical velocity

measurements of simulated super-critical tornado-like vortices in the Miami

University Tornado Vortex Chamber In 2001 [19]. The results suggest a strong

correlation between swiri ratio and super-critical Inner core region diameter, and

a breakdown of super-critical structure far below vortex breakdown.

Another important quantitative measurement in tornado simulator research

Is pressure distribution. Centeriine pressure distributions in a tornado simulator

are obviously an important starting point. Church and Snow obtained axial

pressure measurements In tornado-like vortices for two purposes [20]. First, they

wanted to determine how the magnitude of the central pressure deficit in a

columnar vortex varies with height, and second, to determine what functional

relationships exist between these deficits and the dynamic and geometric

parameters characterizing the flow. They presented vertical profiles of central

pressure deficits for a representative number of laminar and turbulent (single-

celled and two-celled) tornado-like vortices, showing that the variation of the

central pressure with the height is very complicated. They also found that the

largest pressure deficits in the low-swiri vortices are slightly above the surface of

the simulator, not on the surface, and that the low-swiri vortices have generally a

greater central pressure deficit than that of moderate to high-swiri events.

Pauley followed Church and Snow with measurements of axial pressures

in two-celled tornado-like vortices [21]. His goal was to better define the vertical

momentum balance in the cores of two-celled laboratory vortices, where two-

celled vortices Is defined as one with a stream surface dividing an outer cell of

swiriing inflow and up flow from an inner cell which may have down flow near the

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axis. Pauley found that the axial pressure increased with height downstream

(above the bubble) of the vortex breakdown. He also found Indications through

visualization that downstream flow of breakdown is two-celled everywhere, and

that the strongest axial down flow occurred at the middle levels of the vortex.

Jlschke and Light used a modified Ward-type tornado simulator to study

interaction of model structures and tornadic flow fields [22]. They took

measurements of pressure, with and without swiri, on the surfaces of a

rectangular model. Jischke and Light's experiments showed that when

compared with ordinary boundary layer flow, the addition of swiri to flow could

significantly change the forces and moments experienced by the model. They

concluded that location of the model with respect to the tornado vortex and Its

orientation are very important factors in a tornado's capacity for damage In

addition to the tornado's maximum wind speed. Jlschke and Light next studied

tornadic wind loads on a cylindrical structure [23]. The cylindrical structure was

meant to model a nuclear reactor containment building. It was a circular cylinder

with a hemispherical roof. They compared surface pressure coefficients for swiri

angles of 0° and 45° with the model In the convergent zone of the simulator, and

with the model at the boundary of the convergent and convective zones. They

found that when the model is oriented In the convergent flow region of the

simulator, a region where the vertical velocity component is small, the results are

similar to the results of an infinite circular cylinder with circulation. When the

model is near the boundary of the convergent and convective zones of the

simulator, the vertical velocity components of the tornado4ike vortices induce a

circulation about the model which leads to an asymmetric pressure distribution.

That results in forces on the building having both drag and side force

components.

Chang used an indirect approach of using model simulation in laboratory

experiments In 1971 to study tornado wind effects on buildings and structures

[24]. Chang wanted to establish the dynamic similarity of the vortex that was

experimentally created to a typical tornado near and In the ground boundary

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layer. He used a cubical model of a building fitted with distributed pressure taps

that was placed In a fixed position inside the tornado-like vortex. Chang

performed pressure tests for two cases and at two locations. He concluded that

experimental tornado vortex modeling to test wind loading on buildings was

feasible, and accurate representation of dynamic and kinematic effects of full-

scale tornado wind loadings on real buildings, and that pressure distributions

show the combined effects of dynamic pressure and suction.

Bienkiewicz and Pragnesh studied the effects of swiri ratio and surface

roughness on the flow generated by a Ward-type simulator and on building

loading [25]. They concluded that surface roughness has a major effect on the

flow characteristics of a vortex; moderate roughness delayed the transition to and

development of multiple vortices at moderate swiri ratios. Bienkiewicz and

Pragnesh also found that the swiri ratio highly Influences the mean pressure

coefficient on the roof of a building.

Wang also built a working Ward-type tornado vortex simulator, the TTU

TVS I [26]. He tested scale models of generic cubical and cylindrical structures

In this simulator utilizing stationary and transient tests. He found that the roof of

the cylinder encountered more suction than the roof of the cube and that the

pressure fluctuated by as much as 150% between stationary and transient

testing of the models. Wang also found that the pressure distributions for the

dynamic tests he performed were of similar magnitude as the stationary tests he

performed.

1.2.3 Numerical Analvsis

Although the work being done currently at TTU with the tornado vortex

simulator is strictly experimental, it should be noted that numerical calculations

also play an Important role in the worid of tornado study. The fields of

experimental fluid dynamics and computational fluid dynamics are very useful

when combined together. Each field has Its own strengths and weaknesses, so

by exploiting both, one can draw from the strengths of each. Rotunno studied

tornado-like vortex dynamics with fine resolution calculations by using an

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axisymmetric numerical model of the flow within a Ward-type tornado simulator

[27]. His results Indicated that the swiri ratio was the single most Important

parameter In governing the structure of the vortex. Rotunno's model was

consistent with laboratory experiments performed previously by others. He found

that the boundary layer separation at low swiri, a high shear core wall

surrounding a relatively stagnant inner region, and vortex breakdown and

transition to turbulence were all observed and simulated. Hariow and Stein

obtained numerical solutions for tornado4lke vortices using a high speed

computer In 1974 [28]. They did not introduce any special procedures to force

the occurrence of a single-celled or two-celled vortex, however, numerous

examples of single-celled and two-celled vortices were obtained In the range of

parametric variations Investigated. Hariow and Stein concluded that for the first

time numerical calculations performed had shown possible variations In vortex

structure without the requirements for special boundary conditions In the

numerical model to force previously expected results.

Nolan and Farrell studied the structure and dynamics of axl-symmetric

tornado-like vortices with a numerical model of axl-symmetric incompressible

flow [29]. They agreed with previous tornado research and found that the

angular momentum of the background rotating wind field and the turbulent eddy

viscosity, a value that was not determined, entirely determines the structure of a

tornado. Nolan and Farrell also stated that the structure and dynamics of actual

tornadoes will depend crucially on the details of their turbulent swiriing boundary

layers.

Wicker and Wilhelmson studied tornado genesis within a supercell with a

three-dimensional numerical simulation using a two-way interactive nested grid

[30]. During the 40-mlnute simulation, two tornadoes grow and decay within the

storm's mesocyclone, each with a life of about 10 minutes. Winds exceeding

60m/s and 0.018kPa/m of horizontal pressure gradients were recorded for the

tornadoes. When compared to Doppler and field observations of supercells and

tornadoes, the simulated storm evolution showed many similar features.

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Lewellen and Lewellen used large eddy models to simulate a tornado's

interaction with surface structure [31]. The review by Davies-Jones In 1986 was

consistent with the Lewellens' findings In that the swirl ratio variation shows that

the average flow transforms from one with a vortex breakdown above the surface

for low swiri to a two-celled flow on the surface at moderate to high swiri. They

also showed with time averaged velocity distributions that the Interaction of the

tornado with the surface intensifies the low level vortex for all values of swiri.

Selvam has also modeled tornado forces on buildings [32]. He

encountered difficulties in the imposition of boundary conditions, selecting a

turbulence model, and in numerical convergence. He derived a solution

procedure to solve the pressure correction equations. Selvam found that the

forces created on a building's roof were more than five times larger than the

straight boundary layer flow In the forced vortex region and of the same order in

the free vortex flow. Selvam and Millett modeled tornado-structure interaction

with a cubical building using finite-differences to solve the RANS equation and

large eddy simulation equation turbulence model [33]. They found that a

translating tornado produces 45 percent greater overall forces on the walls and

100 percent greater overall forces on the roof than a quasi-steady wind does.

They also found that these forces change magnitude and direction quickly when

the core of the tornado is near the building, and that the localized suction

pressures on the building envelope are generated in multiple locations and are

greater than those in a straight line wind.

Flow in the surface boundary layer beneath a Rankine vortex using a

numerical technique was studied In three-dimensions by Chi and JIh [34]. They

derived generalized equations of motion based on dimensionless vorticity,

stream function and circulation. They found that their method of using Gauss-

Seidel's Iteration procedure to solve the equations assuming a uniform effective

viscosity and a Rankine-type intense vortex at the upper boundary was stable in

the range of Reynolds numbers for natural tornadoes.

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Howells and Smith described an axl-symmetric numerical vortex model

suitable for modeling Intense tornadic activities In 1983 [35]. They used a

stretched grid in the radial direction to provide economical resolution of the vortex

core and the rotating cloud updraft. Howells and Smith found that it was

dynamically possible to generate a relatively narrow vortex in a suitable

background field of ambient rotation that was driven by a much broader field of

buoyant forcing aloft.

Smith also attempted to numerically model tornado-like vortices and

quantify the effects of boundary conditions [36]. He examined the boundary

conditions for Rotunno's numerical model to simulate tornado-like vortices

focusing on the lateral boundary condition for tangential velocity and the upper

boundary condition for radial and tangential velocity, to determine if either had

any significant Impact on vortex development. The presence and absence of the

flow-stralghtening baffle are attempted to be simulated by the upper boundary

conditions. He found that at what he considered low swiri ratios (s=0.87), the

upper boundary condition had a very distinct Impact on the single-celled vortex

by producing changes In the pressure field that Intensified the vortex. At higher

swiri ratios, the upper boundary condition did not appear to have significant

Impact on the development of the vortex. As for the lateral boundary condition,

Smith found that it did not have a significant impact on the development of the

vortex.

1.2.4 Conclusions and Objectives

Ward-type tornado simulators have long been used to study tornado-like

vortices due to their realistic modeling capabilities. The parameters that affect

the type of vortex formed are swiri ratio and aspect ratio. Reynolds number does

not have much influence on the tornado vortex as long as the flow Is turbulent.

As the swiri ratio Is Increased, the vortex starts to break down from a single-

celled vortex to a two-celled vortex and eventually to multiple vortices. Velocity

and pressure measurements have been performed inside the flow field of

tornado simulators as well as on different models which are placed Inside the

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flow field. These models show that the flow field In and around a tornado-like

vortex Is very different from traditional boundary-layer flow.

The objective of this research is to further develop a Ward-type tornado

simulator based on a previous model at Texas Tech University which utilized

slotted jets to provide tangential flow rather than a rotating screen or vanes. The

new simulator will be used to quantify vortices formed. Selected configurations

of boundary conditions will then be used to obtain flow visualization data, velocity

data, and pressure data inside the tornado vortex chamber as well as on scaled

models of generic structures both stationary and transient in nature.

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CHAPTER 2

EXPERIMENTAL SETUP

2.1 Design Criterion

In order to reproduce a tornado In the laboratory, two basic sources of

energy are needed to provide the updraft and circulation. The updraft usually

comes by means of a blower on the top of what will become the tornado chamber

that pulls air out of the chamber. Circulation Is essentially the fluid dynamics

equivalent of angular acceleration. Traditionally, with Ward-type simulators, the

circulation Is caused by a rotating screen or more recently, turning vanes. These

both create sufficient circulation required to generate and maintain single or

multiple vortices and provide a great flow field to perform the task of flow

visualization. The problem with both lies in the actual testing of the flow field.

When the screen or vanes are rotating. It becomes very difficult to place

measurement devices to measure pressure or velocity in the regions of interest

in the flow field.

The Texas Tech University Tornado Vortex Simulator II (TTU TVSII)

eliminates the Impediment of the rotating screen or vanes. For the pressure

testing, the pressure distribution on various models of structures would be

performed while the structures were stationary In specific locations and while the

structures were being translated through the flow field that was created by the

simulator. Instead of using the rotating screen or vanes, slotted jets are used.

The jets protruded from a plenum that was pressurized by a blower with

independent control from the updraft blower. A one-quarter inch slit was cut Into

the jets, and the silt extended from the surface of the simulator to the roof of the

simulator. Using these jets provided access to the regions where the flow field

would be tested. The downside to the slotted jet approach was the quantification

of the actual circulation. With a rotating screen or vanes, the circulation that Is

produced Is very uniform around the perimeter of the simulator. With the slotted

jets, the circulation Is not as uniform because the jet velocity decays and diffuses

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In different directions as a function of distance from the jet exit. The simulator's

dimensions were based on the likely atmospheric range as mentioned by

Church, et al. [9]. The two most important geometric ratios are the aspect ratio

and the swiri ratio. Church, et al. [9] reported that the aspect ratio of a natural

tornado is between 0.2 and 1, and that the swiri ratio (based on a uniform flow) of

a natural tornado varies between 0.05 and 2. Swiri ratio for this simulator will be

discussed In section 3.1.

Three major regions of fluid flow exist In the tornado simulator, the

confluence region, the convergence region, and the convection region. The

confluence region is the region where the fluid flow first enters the tornado

simulator between the roof and the surface. The convergence region is the

region of the simulator where the circulating and updraft flow converge to create

a vortex. This is located at the very center of the simulator between the surface

and the roof. The convection region of the simulator Is the region In which the

vortex propagates up and out of the simulator. These sections are discussed at

length by Wang [26].

2.2 Simulator

Wang at Texas Tech University built the first TTU Tornado Vortex

Simulator and quantified the flow characteristics of the simulator [26]. This

simulator is the first known simulator to use the slotted jet approach rather than a

rotating screen or vanes to provide circulation. Although this simulator served as

a great proof of concept, Its shortcoming was its small size. The original TTU

Tornado Vortex Simulator had a radius to jets of only 0.5m. This radius did not

provide a sufficient confluence zone for the Incoming flow to develop

independently of the slotted jets. In order to remedy this problem, the Texas

Tech University Tornado Vortex Simulator II (TTU TVSII) was constructed. As

mentioned before, a series of sixteen equally spaced slotted jets (50.8mm

diameter pipe with 6.35mm wide silt cut axially) were placed radially around and

protruding from a large (2mx2mx0.6m) plenum. The slots that were cut Into the

pipe spanned the length between the surface of the simulator and the roof where

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the updraft hole was located. This plenum was supplied with a variably

controllable supply of air by means of a blower. To quantify the flow rate of the

air entering the plenum, an orifice plate was constructed and calibrated according

to ASME specifications to be placed between the blower and the plenum. The

surface of the test section of the simulator was located above the plenum and

could be adjusted up and down as the radial updraft hole was kept constant to

control the aspect ratio. The test section Itself was two meters in diameter.

Above the surface of the test section was a roof and in the center of the roof a

radial updraft hole that led Into a convection chamber. The updraft hole Is fixed

with a 0.381m diameter. The convection chamber was made of a cylindrical

piece of plexiglass and measured one meter in diameter. At the top of the

convection chamber Is the flow-stralghtening device that Ward [4] recommended

that eliminates the fan blower's vorticity from the tornado-like vortex. The flow

straightening device is simply a honeycomb grid approximately 76.2mm in length.

Atop the honeycomb grid is the blower that creates suction in the convection

chamber and creates the needed updraft flow. Figure 2-1 Is a schematic of the

Texas Tech University Tornado Vortex Simulator II, and Figure 2-2 is a

schematic of the dimensions of the simulator. The height of the convection

chamber Is 0.813m and the distance from the roof to the surface Is variable

between 0.064 and 0.1905m for an aspect ratio of one-half and one, respectively.

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16 Slotted Jets

Roof

Surface

Vortex Blower

Oriface Plate

Hnnpyrnmh

Convection Chamber

Plenum

Figure 2-1: Texas Tech University Tornado Vortex Simulator II

North

West East

South

Figure 2-2: Dimensions of TTU TVS II (Plan View)

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CHAPTER 3

EXPERIMENTAL PROCEDURE

3.1 Principles of Operation

There are many forms of tornado simulators In the present day. Most are

designed to produce a visible flow field of a vortex that looks like a tornado, but

not all capture the atmospheric complexities associated with an actual tornado

that will lead to meaningful quantification of the flow characteristics. The

traditional Ward-type simulators with Independent control over the tangential and

the updraft flow rates can replicate a scaled down version of the atmospheric

conditions present when a tornado is formed. As previous studies have shown,

the parameters that govern tornadic flow in the atmosphere are the three non-

dimensional ratios, aspect ratio, a, swiri ratio, s, and radial Reynolds number,

Ror. In order to achieve dynamic and geometric similarity, the experimental

aspect and swiri ratio must be comparable to the natural aspect and swiri ratios.

Studies by Church et al. [9] list the typical characteristics of actual rotating

thunderstorm-tornado cyclone system as shown In Table 3-1.

Table 3-1: Likely range of non-dimensional parameters

Dimensionless Group Likely Atmospheric Range

Aspect Ratio (a)

Swirl Ratio (s)

Radial Reynolds Number

(Re,)

0.2-1

0.05-2

10^-10^^

The aspect ratio, a. Is given by the equation:

a = • (3.1)

where h Is the height measured in the convergent region of the simulator

between the surface and the roof, and ro is the radius of the updraft hole. On the

TTU TVS II, the aspect ratio Is adjustable by moving the ground surface up or

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down to achieve the desired ratio. The two ratios that were utilized for this study

were a=0.5 and a=1 which fall In the range that Church, et al. [9] described.

The swiri ratio is another of the important non-dimensional parameters

that dictates the type of flow field that will occur in the simulator. The swiri ratio Is

defined as the ratio of tangential flow rate to updraft flow rate. It is given by:

F r s = "- (3.2)

2Q ^ '

where F Is the circulation, ro Is the radius of the updraft hole, and Qup is the

volume flow rate through the updraft hole. The circulation, F, evaluated at the

slotted jets is not as simple to calculate as It Is for a rotating screen, because the

jet velocity profile Is a function of the nozzle height and distance from the jet exit.

In the case of the rotating screen, the circulation can be directly related to the

speed of the rotating screen if It Is assumed a perfect coupling exists between

the incoming air and the rotating screen. The circulation is defined as the cyclic

integral of the tangential velocity dotted with a differential arc length of the curve

for this work. In order to calculate the circulation in the TTU simulator, a single-

channel hot film probe was used to measure the jet velocity profile as a function

of height and position. The following relation was used to determine the

circulation:

T = <^Vds^n^^V(x)-dx (3.3) 0

where V(x) is the mean jet velocity obtained using a curve fit of measured

velocities as a function of distance from the jet, / Is the distance between jets,

and n is the number of jets. The jet velocity profiles were obtained by sampling

eight axial positions three times a piece and averaging. This was done at three

different heights, low, mid, and high, for each case, then the low, mid and high

were averaged and a trendllne was fitted to the overall averaged profiles for each

case (Figure 3.1, Figure 3.2, Figure 3.3, and Figure 3.4).

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0.15 0.2 Rasition (m)

o

0

A

+

Low Height

Mid Height

Hgh Height

Average

-Fbwer (Average)

0.35

Figure 3-1: Jet Velocity Profile (a=0.5, Low Swirl)

0.15 0.2

Position (tn)

o

a

A

+

Low Height

Md Height

High Height

Average

-RDwer

0.35

Figure 3-2: Jet Velocity Profile (a=0.5, High Swirl)

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o

n

A

+

Low Height

Md Height

High Height

Average

-Fbwer

0.2

Position (m)

0.3 0.4

Figure 3-3: Jet Velocity Profile (a=1. Low Swiri)

18

16

14

~ •'2

1 . 10

o <u >

o \ + \ A ^

A

..ft

o

v=0.6136x-°^93

T 8 - *

o

D

A

+

Low Height

Mid Height

High Height

Average

-Rower

0.05 0.1 0.15 0.2

BDsition (nfi)

0.25 0.3 0.35

Figure 3-4: Jet Velocity Profile (a=1. High Swiri)

The equation for the trendline Is integrated using equation 3.3 above to find the

circulation.

Once the circulation Is known, the only other parameter that needs to be

calculated to obtain the swiri ratio is the updraft volume flow rate, Qup. The

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updraft volume flow rate was determined using the single-nomer hot-film to

traverse the updraft hole to obtain velocities across the updraft hole. For

comparison. Table 3.2 shows the updraft velocity across the updraft hole of the

simulator and the turbulence intensity at each of these points.

Table 3-2: Velocity, Turbulence Intensity Radius, (mm) 0.000 12.700 25.400 38.100 50.800 76.200 101.600 127.000

a=1/2, low swirl Velocity, (m/s)

Turbulence Intensity

15.117

18.553

14.499

18.810

14.199

17.664

12.873

26.487

14.183

22.710

12.322

28.765

12.698

22.600

12.787

29.674

190.500

10.162

41.816

3=1/2, liigh swirl Velocity, (m/s)

Turbulence Intensity

10.430

31.330

10.839

30.969

10.320

34.407

10.424

30.487

9.840

30.798

9.542

33.580

8.845

31.031

8.769

33.922

8.171

32.845

a=1, low swirl

Velocity, (m/s) Turbulence

Intensity

12.163

14.637

11.913

16.049

13.993

22.349

13.492

17.379

12.946

16.142

14.729

16.615

14.363

17.120

14,789

21.029

13.018

27.164

a=1, tiigh swirl

Velocity, (m/s) Turbulence

Intensity

7.978

31.581

8.386

36.889

9.814

34.250

9.394

34.310

8.796

35.790

8.379

36.413

8.942

33.739

8.344

33.692

7.551

34.165

These velocities were then multiplied by annuli of the updraft hole and

summed to obtain a volume flow rate. To ensure repeatability of swiri ratio each

time the simulator was used, an orifice plate between the blower and the plenum

was attached to a manometer and monitored. Using the manometer, the change

In pressure across the orifice plate could be adjusted to a precise, predetermined

value each time testing was to be done. Using the data acquired, swirl ratios

were found and are presented In Table 3.3, and are unique to the TTU TVSII.

Table 3-3: Calculated Swirl Ratios

Swir l Ratio Aspect Ratio

a=0.5 a=1

Low Swir l 2.23 1.51

High Swir l 8.03 6.72

The radial Reynolds number, Rer, Is defined by Church et al. [10] as the

volume flow rate per axial length, q, divided by two times pi times the kinematic

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viscosity of the fluid in question. The axial length Is described as h, the depth of

the convergence region. The equation for radial Reynolds number is:

27IV

Even though It Is typically discussed as an Important ratio in tornado vortex

generation, Ward [4] states that it was not an important parameter in determining

the type of vortex that is developed as long as the flow field Is turbulent.

3.2 Procedures Two main types of vortices were studied In the TTU tornado simulator.

The first is called a single-celled vortex and the second a two-celled vortex. The

swiri ratios calculated above correspond to a single-celled and a two-celled

vortex for the low swiri and the high swiri, respectively. The single-celled vortex

is characterized by a thin, rope-like, vortex, which some refer to as laminar [9].

The two-celled vortex is characterized by a much larger vortex that has a stream

surface dividing an outer cell of swiriing in-flow and up-flow from an Inner cell In

which down flow near the axis exists. The first step In quantifying the swiri ratios

that would be used In the study was to visualize each type of vortex and record

the pressure change across the orifice plate at which the vortex occurred. This

ensured that the same type of vortex could be obtained for each test, even when

no flow visualization material was used. It is also notable that the vortex rotates

in a counter-clockwise direction throughout all tests. The flow field created

consists of two main components. The tangential component of the flow field Is

the flow that Is rotating In a horizontal plane around the model. The radial

component of the flow field is the flow coming in from the sides of the simulator in

a vertical plane.

3.3 Flow Visualization

Flow visualization is essential to determine what type of vortex is being

formed in a tornado simulator. Four visualization methods were used to study

the vortex: helium bubbles, "smoke," a fog generator, and liquid nitrogen. The

helium bubbles method uses a helium bubble generator to create uniformly sized

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bubbles that are neutrally buoyant. This method turned out to be the best of the

three ways to visualize the vortex due to control of location and quantity of

bubbles introduced. When performing the flow visualization on the TTU tornado

vortex simulator, neutrally buoyant helium bubbles from a helium bubble

generator were Introduced at the surface of the simulator with effectively no

vertical or radial velocity component. The bubbles are Illuminated with the aid of

an arc lamp. The bubbles were swept through the convergence region of the

simulator up into the convective chamber and out of the chamber through the

updraft fan. The "smoke" methods created visualization material that could not

be reasonably controlled. Visualizing the vortices using liquid nitrogen and fog

from the fog generator has shown promise, as some control of the quantity

introduced is available, but at this time problems exist for controlling the amount

of liquid nitrogen or fog to use for optimum visualization.

3.4 Measurement Techniques

To measure velocity, a TSI IFA 300 constant temperature anemometer

system was utilized. In order to control the IFA 300, TSI's ThermalPro software

was used. The IFA 300 constant temperature anemometer measures velocities

by means of a single-channel hot-film probe. The probe was controlled by a

dual-axis linear traverse and was connected to the IFA 300 system via a thirty

meter cable. All velocities reported were obtained using a frequency of 1000 Hz

and four kilopolnts per channel (4000 points). Velocity measurements are an

Integral part of the data which was collected and great care was taken to obtain

the velocities without disturbing the flow regime. However, the hot-film

anemometry system is very intrusive, especially In a rotating flow such as this, so

velocity measurements are subjected to interference. Due to these limitations,

only a jet exit velocity profile and the updraft hole velocity profile were obtained

using the hot-film anemometry system.

Pressure measurements were performed In the tornado vortex simulator

using of a Scanlvalve DSM 3000 system and ZOC 33/64Px and ZOCEIM

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scanning modules. For the stationary tests performed, only the ZOC 33/64Px

scanning module was needed, but for the dynamic moving tests, the ZOCEIM

module was employed to serve as a precision timer so that the velocity of the

model could be obtained as it traversed the simulator. The ZOC 33/64Px

scanning modules consists of 64 piezoreslstive sensors that are activated via

pneumatic switching by the DSM 3000 CPM which is the pressure distribution

control module. The ZOCEIM module was calibrated to read a voltage signal

when a switch Is tripped. During the dynamic moving tests, the switch was

tripped twice in order to obtain a starting and a stopping point. All pressure

measurements were performed at 300 Hz for six seconds, but the dynamic

moving tests will have a slightly reduced time frame.

3.5 Uncertainty Analvsis Uncertainty analysis was calculated for the swiri ratio and the stationary

force coefficient. Uncertainty is limited to man-made and instrumental

uncertainty due to the fact that there Is no method at this time to determine the

flow-induced uncertainty. The method used to calculate uncertainty was the

general error propagation equation:

"/ = z y, (3.5)

The uncertainty in the swiri ratio is given by:

w, =. ds

— I

ar

ds

52, Qup

up J

(3.6)

where Ur=UQup=0.5% as reported by the manufacturers calibration. The

uncertainty in swiri ratio Is approximately 5%.

The uncertainty in force coefficient is:

(dC, Ur = .

dp -1-

dC.

dw ) -H

dc. ydA, J

dCj \ 2

(3.7)

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where Up=0.2%, Uw=0.5%, and UAI,2=1%- Up and Uw were obtained by

manufacturer's specifications, Uai,2 was obtained by direct calculation. This

makes the uncertainty in force coefficient 1.16%.

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CHAPTER 4

RESULTS AND DISCUSSION

For this tornado simulation study, flow visualization and pressure

measurements on model structures were performed to determine fluid structure

Interactions. This is the first step in ultimately designing safer structures. For

flow visualization, helium bubbles and various other flow visualization materials

were introduced in the flow field of the TTU TVSII and pictures were taken to

qualitatively show what type of flow existed Inside the TTU TVSII. These pictures

showed various types of tornado vortex structures.

To quantitatively examine the TTU TVSII, pressure measurements were

taken on two different scale models of structures, one being a cube the other a

cylinder. These pressure measurements were then converted into force

coefficients and plotted In contour plots of each structure at various radial

locations Inside the simulator. Also, in an attempt to model a natural tornado as

precisely as possible and to compare with stationary tests, moving tests were

performed with each model where the model was traversed across the simulator

while simultaneously collecting pressure measurements. These pressure

measurements were converted to force coefficients, and plotted as a function of

radial position in the simulator.

4.1 Flow Visualization Flow visualization is a very Important process to qualitatively determine

what type and direction of flow is present in any fluid flow field. As previously

stated in section 3.3, different types of flow visualization techniques were utilized

in the TTU tornado vortex simulator, but helium bubbles proved to be the best

means of visualizing the flow field.

The flow field of the TTU tornado simulator behaves much like other

simulators before [3, 6, 7, 8]. When the swiri ratio is very small, on the order of

zero, the fluid Inside the tornado simulator does not experience much tangential

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velocity, only updraft velocity. For this reason, the flow in the convergence

region acts in much the same way as the flow In a conventional wind tunnel with

a horizontal velocity component until It reaches the updraft hole. As the fluid

moves horizontally under the region of the updraft hole the flow changes from

mostly radial to mostly vertical. The fluid is then expelled out of the top of the

convection chamber. As swiri is slowly Imparted on the fluid, the fluid starts to

circulate tangentially as it moves toward the updraft hole. When the circulating

fluid Interacts with the updraft, it is lifted through the updraft hole stretching Its

vorticity vertically. This is the start of the formation of the tornado vortex. Figure

4-1 shows a slight protrusion of bubbles from the top surface of the simulator

which is where the updraft hole Is located. The updraft flow still dominates the

circulating flow.

'^mm

Figure 4-1: Start of Vortex Formation (a=0.5)

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ism l^ssJS:^^n;^''.:2..i,^a»^^;^>^;^>y-';t^ mmm MM ^TJ'jC^Sg^S^^^^I^^SS ***^^^*'^*^'^^i»i7iM?5S*ii^li'SiRfii

HP M%*PW*< S8P

i

Figure 4-2: Progression of Vortex Formation (a=0.5)

Figure 4-3: Single-Celled Vortex (a=1, Low Swirl, s=1.51)

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As the swiri ratio is increased, the vortex propagates downward toward the

surface of the tornado simulator, eventually reaching the surface. Figure 4-2

shows the progression as the swiri ratio increases and the vortex moves from the

updraft hole to the surface of the simulator. Figure 4-1 and Figure 4-2 are shown

at an aspect ratio of a=0.5; this type of vortex is called a single-celled vortex.

Figure 4-3 shows a single-celled vortex at an aspect ratio a=1. The Inner core

diameter of these single-celled vortices ranged from ten to fifteen millimeters in

width as shown In Figure 4-4 and Figure 4-5 for the aspect ratio of one-half and

one, respectively. (Please note that the ruler scale is inches.) Figure 4-6 shows

two different vortices, each at an aspect ratio of one-half and low swiri ratio,

visualized with helium bubbles and fog from a fog generator. Notice that the

vortex of bubbles has a much smaller diameter that the vortex of smoke. This is

due to the fact that the bubbles converge to the inner vortex core and the smoke

defines the outer region of the vortex core which has an estimated diameter of

approximately 50mm.

Figure 4-4: Scale of Inner Cone of Single-celled Vortex (a=0.5. Low Swirl, s=2.23)

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'• , O L . -'U^'l

, - _ _ ,

Figure 4-5: Scale of Single-Celled Vortex (a=1, Low Swirl, s=1.51

Figure 4-6: Vortex with Helium Bubbles and Smoke (a=0.5, Low Swirl, s=2.23)

As the swiri ratio is increased, i.e., the ratio of the tangential flow rate to

the updraft flow rate increases, the tangential flow rate starts to have a

dominating effect on the updraft flow rate meaning that the tangential flow rate

has more of an influence on the flow field than the updraft flow rate. When this

happens, an adverse pressure gradient starts to occur spawning the 'breakdown

bubble' at the top of the vortex. This 'bubble' forms the boundary between the

supercritical flow upstream and the subcritical flow downstream. The

supercritical flow upstream of the breakdown bubble is very similar. In

appearance, to the single-celled vortex described eariier. However, the 33

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subcritical flow downstream is tripped by the bubble and appears to be turbulent.

As the tangential flow rate is increased, the bubble moves down the vortex

toward the surface of the simulator. This causes a deceleration In the axial

direction of the vortex inner core and eventually, an actual down draft in the very

center of the vortex. This central down flow region is surrounded by the vertical

vorticity of upflow. When the breakdown bubble reaches the surface of the

simulator, the core of the vortex expands radially and the down flow in the central

core penetrates to the surface. When the combination of the updraft and

downdraft are each present at the same time, and the breakdown bubble has

penetrated the vortex core to the surface of the simulator, the vortex Is defined as

two-celled. Figure 4-7 shows a two-celled vortex.

Figure4-7: Two-Celled Vortex (a=1. High Swirl, s=6.72)

A two-celled vortex is much larger in diameter that a single-celled vortex.

In the TTU tornado simulator, the two-celled vortices generally ranged from 80 to

100 millimeters as shown In Figure 4-8. (Note that the scale on the ruler Is

measured In Inches.)

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Figure 4-8: Scale of Two-Celled Vortex (a=0.5, High Swirl, s=8.03)

Another interesting study with flow visualization Is the Interaction of the

fluid flow field with structures. Two generic structures, one a 30 millimeter cube

and the other a 30 millimeter cylinder were place In different positions Inside the

tornado simulator. These structures combined with the flow visualization material

provided Images of the fluid-structure interaction in the fluid flow field inside the

TTU tornado vortex simulator. In all Images, the helium bubbles were introduced

on either side of the cube. Figure 4-9 shows the cubical model in the center of

the TTU tornado vortex simulator at low swiri and an aspect ratio of one-half.

Figure 4-10 and Figure 4-11 show the same cubical model In the center of the

tornado simulator at low swiri and an aspect ratio of one. These Image shows

that the single-celled vortex is severely disrupted by the placement of the cube.

The single-celled vortex is evident in all three figures, but it is disrupted by the

sharp edges on the cube.

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Figure 4-9: Flow Visualization with Cube in Center (a=0.5, Low Swirl, s=2.23)

Figure 4-10: Flow Visualization with Cube in Center (a=1, Low Swirl, s=1.51)

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Figure 4-11: Flow Visualization with Cube in Center (a=1, Low Swirl, s=1.51)

Figure 4-12 and Figure 4-13 show the cubical model in the tornado simulator

slightly off center (0.5*ro to center of cube) at low swiri, s=2.23, and an aspect

ratio of one-half. These images show that there is a definite single-celled vortex

present even with the disruption in flow caused by the cubical model.

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Figure 4-12: Flow Visualization with Cube Offset (a=0.5, Low Swirl, s=2.23)

Figure 4-13: Flow Visualization with Cube Offset (a=0.5. Low Swirl, s=2.23)

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Figure4-14: Flow Visualization with Cube Offset (a=1, Low Swirl, s=1.51)

Figure 4-14 shows four different positions of the cubical model In the

tornado simulator at an aspect ratio of one and low swiri. As the cubical model

moves away from the center of the tornado simulator, more of the helium bubbles

are swept up through the updraft hole without being caught in the vortex that Is

formed (note that the bubble nozzles are also moving). As the cubical model

gets closer to the center of the tornado simulator, more of the bubbles are pulled

into the visualized vortex. This is due to the fact that the farther away from the

center of the tornado simulator In the convergence region the cube gets, the

more the flow behaves like boundary layer flow. This is because the radial flow

component of velocity greatly supercedes that of the tangential flow component

of velocity at low swiri ratios. At high swiri ratios, when the vortex is considered 39

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two-celled. The vortex does not seem to be neariy as disrupted by the cubical

model as when the vortex is single-celled (Figure 4-15 and 4-16). This Is

because the tangential flow component dominates over the radial flow

component for the high swiri case. This means that the larger vortex Is being

more influenced by the tangential velocity component than the radial velocity

component of the fluid flow.

Figure 4-15: Flow Visualization with Cube in Center (a=0.5. High Swirl, s=8.03)

When the cube Is offset as in Figure 4-17, Figure 4-18, and Figure 4-19

the helium bubbles are caught in the tangential flow rather than the radial flow.

These figures show that In the high swiri case, the vortex Is not very disrupted by

the presence of the model.

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Figure 4-16: Flow Visualization with Cube in Center (a=1. High Swirl, s=6.72)

Figure 4-17: Flow Visualization with Cube Offset (a=0.5, High Swirl, s=8.03)

41

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Figure 4-18: Flow Visualization with Cube Offset (a=0.5. High Swirl, s=8.03)

Figure 4-19: Flow Visualization with Cube Offset (a=1, High Swirl, s=6.72)

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Another Interesting model to observe along with the flow visualization

material In the TTU tornado simulator is a generic model of a cylinder. Due to Its

circular geometry, the fluid flow field around the cylinder is more uniform than the

flow field around the cubical model. When the cylinder is in the center of the

tornado simulator, a vortex continues to form above the cylinder for both high and

low swiri ratio cases. The vortices that form above the cylinder are much more

consistent with the vortices formed when no model Is present than the vortices

that form above the cubical model. Figure 4-20 and Figure 4-21 show the

cylinder In the center of the tornado simulator at low swiri and high swiri,

respectively. It Is cleariy evident that the vortices above the cylinder are not

neariy as disrupted as the vortices above the cubical model.

Figure 4-20: Flow Visualization with Cylinder in Center (a=1. Low Swirl, s=1.51)

43

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Figure 4-21: Flow Visualization with Cylinder in Center (a=1, High Swirl, s=6.72)

The flow around the cylinder also encounters little disruption when the

cylinder is offset from the center (Figure 4-22 and Figure 4-23). The vortical flow

sweeps the bubbles that are on the outside of the cylinder around the cylinder

following the cylinder's circular profile and into the vortex Itself. This happens for

low and high swiri ratio, but is much more pronounced in the high swiri ratio case.

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Figure 4-22: Flow Visualization with Cylinder Offset (a=1, Low Swirl, s=1.51)

Figure 4-23: Flow Visualization with Cylinder Offset (a=1, High Swirl, s=6.72)

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4.2 Pressure Measurements

4.2.1 Models

As used with the flow visualization, two generic models were constructed

to study the fluid-structure interaction in the Texas Tech University Tornado

Vortex Simulator. One Is a thirty millimeter cube with a flat roof and the other is a

thirty millimeter in diameter cylinder (Figure 4-24). The cube had a total of sixty-

four pressure taps distributed across its faces, 16 evenly distributed on the top

face and 12 on each side. The cylinder had a total of 39 pressure taps, seven on

the top and 32 arranged In vertical rows of four every 45 degrees around the

perimeter of the cylinder. The pressure taps on each model consisted of 1.02mm

Internal diameter tubing that was 200mm long. This tubing was glued from the

inside In the holes drilled Into the models and any excess tubing protruding from

the models was carefully trimmed off with a razor blade.

30mm Cube

Figure 4-24: Schematic of Model Cube and Cylinder

In order to compare the models tested with actual full-size buildings, a

scale ratio has to be obtained. One parameter that Is known from the flow

visualization is the inner core diameter of the vortices. According to Church [7],

the core diameter for a typical F2 tornado is estimated to range between 10 and

150 meters. Using this range coupled with the fact that the TTU tornado vortex

simulator produces vortices ranging on average from 12.5 mm for the single-

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celled vortex to 90 mm for the two celled vortex, a scale factor range can be

calculated (Table 4-1). At the low-scale range, the model of the cube and

cylinder correspond to a structure similar in size to a storm shelter at 3.33m by

3.33m. At the high-scale range, the models correspond to a tremendous 360m

by 360m structure.

Table 4-1: Scale Factors Between Simulated Vortex and Actual Vortex

TTU Tomado Vortex Simulator Vortex Diameter (m)

0.0125-0.090

Typical F2 Tomado in Nature (m)

10-150

Scale

-1:100-1:10000

4.2.2 Orientation

The orientation of the models with respect to the vortex must be

established for both the stationary and moving tests when testing the two models

to obtain the pressure distribution. The sides on each model were labeled north,

south, east, west, and top, and the models were positioned In the simulator

consistently each time tests were taken. The model was always positioned

starting on the north side of the simulator with the north face of each model

facing north. The pressure tests were performed with the models advancing from

north to south. Pressure data was obtained for model locations between +2.0*ro

of the updraft hole, with a total of thirty-one positions. A schematic of the surface

of the tornado simulator is shown in Figure 4-25, and the different positions that

the models were tested at are shown in Figure 4-26. Note that more locations

near the center of the simulator were used.

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North

West East

South

Figure 4-25: Schematic of Surface of Tornado Simulator

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West

Position North

South

East

Figure 4-26: Positions where Models were Tested in Simulator

4.3 Stationary Force Distributions

The cubical and cylindrical models were positioned at each of the 31

positions described above for each aspect ratio and swiri ratio. Through these

tests, differential pressures were obtained for each of the pressure taps on the

two models. Pressure coefficients are reported for most tornado vortex simulator

studies. Pressure coefficients are dimensionless due to the fact that a differential

pressure Is divided by some dynamic reference pressure. Originally, for this

study, pressure coefficients were to be used. The reference pressure that would

non-dimensionalize the differential pressure was obtained by use of a pitot static

tube placed at the center of the updraft hole facing downward toward the surface

of the tornado simulator. This configuration gave valid results when the swiri was

very low, but as the swiri increased, downdrafts started to occur at the center of

the updraft hole that resulted In negative pressures as measured by the pitot

static tube (e.g., not the dynamic pressure).

Due to the fact that the dimensionless pressure coefficient was Invalid,

force coefficient calculations were obtained for each pressure tap on the models. 49

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The force coefficients were generated by non-dlmensionallzing the recorded

differential force with a momentum Integral relation. The force coefficients were

calculated with the equation

c,-'-y (4^1) p^w A

where p is the density of air, w is the axial velocity component at the center of the

updraft hole and A is the frontal area of the model. The F-F^ef term In the

numerator is calculated by the equation

where prPret is the differential pressure obtained with the Scanlvalve pressure

measurement system at each pressure tap minus the differential pressure

obtained with the Scanlvalve pressure measurement system on the surface of

the simulator at each point studied, and /4,is the small area associated with each

pressure tap. The surface pressure profiles (gage pressures) relative to the local

atmospheric conditions used in calculations are shown In the following figures

(Figure 4-27, Figure 4-28, Figure 4-29, and Figure 4-30).

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Figure 4-27: Surface Pressure Profile for a=0.5, s=2.23

-50 -

-100 -

i^-150

"-200

-250

-300

-350 -2

1

.

-

1

1 1 1

~~^^--..^^

\ \

1 1 1

^-^^ y

• 1

^

1

-1.5 -0.5 0 r/ro

0.5 1.5

Figure 4-28: Surface Pressure Profile for a=0.5, s=8.03

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Figure 4-29: Surface Pressure Profile for a=1, s=1.51

Figure 4-30: Surface Pressure Profile for a=1, s=6.72

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For the cubical model, the top face area was divided Into sixteen equal

areas of 56.25mm^ each and each side area was divided Into twelve equal areas

of 75mm^ each. Likewise, for the cylinder, the body was divided into thirty-two

equal areas of 88.36mm^ each, and the top face area was divided Into seven

different regions of 80mm^ each. Using the calculated areas, the product of each

gage pressure calculated at each pressure tap and the corresponding calculated

area was obtained. This produced a force (in Newtons) at each finite area on the

two different models. To non-dimensionalize this force, a momentum Integral

relation was needed. The most accurate velocity measurement which could be

obtained and was repeatable was the updraft hole velocity at its center point.

Using the updraft velocity at each swiri ratio and aspect ratio, the area of the

frontal face of each model, and the density of air, a reference force was

calculated that would non-dimensionalize the directly calculated forces on the

models. These force coefficients were plotted using MatLab on contour plots. It

should be noted that the contour plots represent the area on the models bounded

by the pressure taps, not the actual area of the model. It Is also notable that the

vortex rotates In a counter-clockwise direction throughout all tests. The flow field

created consists of three main components, tangential, radial, and axial. The

tangential component of the flow field Is the flow that is rotating In a horizontal

plane around the model. The radial component of the flow field Is the flow

coming in from the sides of the simulator In a vertical plane. The axial

component of flow is the flow moving up through the convection region of the

simulator. It should also be noted that a representative selection of figures has

been chosen for these results and discussion. Appendix A contains figures for

each position described at each swiri and aspect ratio.

4.3.1 Cube Model

Contour plots of force coefficients as a function of position on the cubical

model were generated for this study. Each figure will contain a set of five

different contour plots that correspond to each face of the cube in an exploded

view. Figure 4-31 shows a map of where each face is plotted In the exploded

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view of the cube. This is held constant throughout all figures and also, the word

vortex has been added to each figure representing the orientation of the model

with respect to the vortex center. It should be noted that each face Is rotated

outward on Its adjacent axis with the top face for the exploded view of the cube

and that the contour plots generated are bounded by the matrix of pressure taps

on the cube.

North Face

Vortex Rotation Direction

infest Face Top Face East Face

South Face

Figure 4-31: Exploded View of Cubical Model

Figure 4-32 and Figure 4-33 show the exploded view of the cube with

contour plots of force coefficients for each face at position 1 (2.0*ro) and 6

(1.0*ro), respectively, in the simulator at a=0.5, s=2.23. At these locations In the

simulator, the greatest force coefficients on the cube are on the side faces, with

the north face having the greatest force coefficients In magnitude. In the case of

low aspect ratio, a=0.5, it can be seen that the values on the north face of the

cube are greater In magnitude than the values on the other faces of the cube.

This could indicate a possible separation of flow from the cube at the top, east

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and west faces. The force coefficients on these specific model plots are of the

same pattern as force coefficients on model plots that are in a boundary layer

type flow with positive pressures on the north face, much lower pressure along

the top face, and slightly lower pressures along the south face. This Implies that

the flow around the cubical model is dominated by the radial flow coming in from

the outside of the simulator rather than the tangential flow rotating inside the

simulator In a horizontal plane Indicating that the radial flow velocity component

has the greater contribution to the pressure distribution on the cubical model than

the tangential flow. Although the magnitudes of the values on each of the side

faces for the high aspect ratio, a=1, cases are closer to being equal to each other

than the values for the a=0.5 case, the same type of patterns exist on the high

aspect ratio case, a=1, as did on the low aspect ratio case, a=0.5, indicating

again, a possible pattern of force coefficients that look like the pattern for

boundary layer type flow force coefficients on a similar model. This Is a very

typical pattern of force coefficient on the cube when the cube Is positioned

greater than 0.5*ro from the center of the simulator In the low swiri case (s=2.23

and s=1.51), and occurs when the cube Is positioned on either side of the

simulator, the north or the south side. It should be noted at this point that some

of the figures showing contour plots of force coefficients on the cubical model

with all positive force coefficients. This Is due to the fact that the local surface

pressure (measured without a model present) Is lower than the pressure

obtained at any position on the cube. A possible reason for this is that the flow is

disrupted In such a way that the local velocity Is smaller when the model is

present in the simulator than when the model Is not present. This lower local

velocity would cause a greater local static pressure and therefore the calculated

pressure coefficients would be positive rather than negative.

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Figure 4-32: Force Coefficients on Cube at 2.0*ro (Point 1) in Simulator (a=0.5, s=2.23)

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XlO'

3

2.5

2

1.5

\ o

/ i/

Figure 4-33: Force Coefficients on Cube at 1.0*ro (Point 6) in Simulator (a=0.5, s=2.23)

Figure 4-34 and Figure 4-35 show the exploded view of the cube with

contour plots of force coefficients for each face at position 1 (2.0*ro) at a=0.5 and

s=8.03 and at point 10 (0.125*ro) in the simulator at a=1 and s=6.72, respectively.

Both plots show the greatest force coefficients acting on the north and east faces

of the cube. This would indicate a combination of radial and tangential flow

components contribute significantly to the forces acting on the cube. The lower

force coefficients on the south and west faces indicate a possible separation from

the north-west and south-east corners of the cube. This pattern of force

coefficient on the cube is the same for the high swiri (s=8.03 and s=6.72) cases

from when the cube Is between 2.0*ro and 0.5*ro from the center of the simulator.

This pattern of force coefficients is also present when the cube is at a=0.5,

s=2.23 and a=1, s=1.51 at 0.25*ro in the tornado simulator. The force

coefficients on the cube at these two lower swiri ratios when the cube Is much

closer to the vortex in the tornado simulator behave much like the force

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coefficients on the cube at higher swiri ratios when the cube Is much farther away

from vortex. This Is due to the fact that the circulation Is much greater In the high

swiri (s=8.03 and s=6.72) cases than in the low swiri (s=2.23 and s=1.51) cases

causing the flow field to rotate less at the outer regions of the simulator In the low

swiri (s=2.23 and s=1.51) cases than It does in the high swiri (s=8.03 and s=6.72)

cases. As a consequence, the cube must be much closer to the vortex,

approximately 0.25*ro away from the center of the simulator. In the low swiri

(s=2.23 and s=1.51) cases to experience the same force coefficients exerted on

it during the high swiri (s=8.03 and s=6.72) cases when it Is much farther away

from the vortex, approximately 0.5-2.0*ro away from the center of the simulator.

It should be noted that the plots shown are for the cube positioned on the north

side of the vortex. When the cube Is positioned the same distance away on the

south side, the faces with the greatest force coefficients acting on them will be

the mirror Image. Therefore, since these plots show the greatest force

coefficients acting on the north and east faces of the cube with possible

separations at the northwest and southeast corners of the cube, the plots of the

cube when it Is oriented on the south side of the vortex show the greatest force

coefficients acting on the south and west faces of the cube with possible

separations at the northwest and southeast corners of the cube.

58

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3

2.5

2

1.5

°^y/ — 0 . 5 6 - ^

\ /y

o

y^

3

2.5

2

1.5

1

V 1 \yc y ^0.74-

/

y /p.T^s;^

Figure 4-34: Force Coefficients on Cube at 2.0% (Point 1) in Simulator (a=0.5, s=8.03)

2.5

2

1.5

1

--0 05 / /

- - 0 . 1 - ^ ^

V

/

•':5-^

^ . 1 5 "

xlO-

rf 1 ] /^^

z '

r

— 1 -

A''

\ \ \ \ \'<' VKA \ ioXX ^-^S \ —oS /

::—-^-^

/ n , V c.'

s\ \ \ \ \

/ <o

\ 9'l

\\]

N ^ /

" / \ / ^

yyy^ ^ - -0.1 • — ^ -0.15

2 Vortex

Figure 4-35: Force Coefficients on Cube at 0.5*ro (Point 10) in Simulator (a=1, s=6.72)

59

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Figure 4-36 and Figure 4-37 show the contour plots of force coefficients

along each face of the cube at 0.25*ro (Point 12) in the simulator at a=0.5 and

s=8.03 and at 0.125*ro (point 18) at a=0.5 and s=2.23, respectively. These plots

are of the cube at different swiri ratios and on different sides of the vortex, but

they show the same pattern of force coefficients emerging on opposite sides of

the cube. In each case, the greatest force coefficients now occur on the east and

west faces of the cube for the s=8.03 and s=2.23 cases, respectively. For the

case when the cube is at 0.25*ro (point 12) In the simulator (cube on the north

side of the vortex), the greatest force coefficients are located on the east face of

the cube and all other faces experience significantly lower force coefficients,

possibly due to flow separation on these faces of the cube. For the case when

the cube Is at 0.125*ro (point 18) in the simulator (cube on the south side of the

vortex), the greatest force coefficients are located on the west face of the cube

and all other faces experience significantly lower force coefficients, possibly due

to flow separation on these faces of the cube. This is a force coefficient pattern

which looks very similar, as before, to the pattern of force coefficients created on

a similar model In a boundary layer-type flow, only now the tangential component

of the flow seems to be causing the boundary layer-type flow pattern of force

coefficients rather than the radial component of the flow. This Is due to the fact

that the flow regime rotating around the center of the simulator moves faster the

closer to the center of the simulator it gets due to angular acceleration, so the

tangential flow component contacting the model as the model gets closer to the

center of the simulator is greater than the radial flow component contacting the

model. This causes the model to experience greater force coefficients on the

east and west sides depending on which side of the vortex it is on rather than the

north and south sides.

This phenomenon of force coefficient patterns which look like patterns on

similar models in boundary layer-type flow experienced by the east and west

faces of the cube Is seen in a very small region of the simulator. For the low swiri

cases (s=2.23 and s=1.51), it is seen only when the cubical model is

60

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approximately 0.125*ro from the center of the simulator, and for the high swiri

cases (s=8.03 and s=6.72), it Is seen only when the model is approximately

0.25*ro to 0.125*ro from the center of the simulator. At these points, the model is

just outside of the inner core vortex formation for each respective case, a point at

which the tangential velocity component Is maximum.

xlO^

y"'S^ / ^ ^ ^

3r

2.5

2

1.5

1

<

Figure 4-36: Force Coefficients on Cube at 0.25*ro (Point 12) in Simulator (a=0.5, s=8.03)

61

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\, ''

Vortex

- O . A ' ^ ' " '

•• T A

\ \ °- ^ r / / W

^^ '-'^yi \ ^ ^

x10'

Figure 4-37: Force Coefficients on Cube at 0.125*ro (Point 18) in Simulator (a=0.5, s=2.23)

Figure 4-38 and Figure 4-39 show the contour plots of the force

coefficients on the cube at 0.0625*ro (point 15) In the simulator at a=0.5 and

s=2.23 and at the center of the simulator at a=1, s=6.72, respectively. At this

points, the cube Is very close to if not partially consumed by the actual tornado

vortex in the low swiri (s=2.23 and s=1.51) or single-celled vortex case and

partially consumed by the tornado vortex in the high swiri (s=8.03 and s=6.72) or

two-celled vortex case. Due to its proximity to the actual vortex, the cube

undergoes forces exerted by a very complex flow field. The side faces of the

cube all have positive force coefficients that are of comparable magnitude in

each respective case. The top face of the cube in each of the low swiri (s=2.23

and s=1.51) cases have negative force coefficients acting on them when the

cube is 0.0625*ro away from the center of the simulator. In the high swiri cases

(s=8.03 and s=6.72) when the cube is 0.0625*ro away from the center of the

simulator and In all cases when the cube Is in the center of the simulator, the top

62

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faces have positive coefficients acting on them. This Is Indicative of the fact that

the local surface pressure is lower than the local pressures exerted on the

cubical model at this point In the simulator, so the cube is creating a blockage

effect in the flow field. The flow field at these points In the simulator is very

complex and is very disrupted by the model's presence. At the present time, the

flow field at these points can not be quantified due to lack of experimental

equipment and data.

3

2.5

2

1.5

1

yy^y ^,^0.75

-0.55

x10^

~~ 0.75X

\ ^ >

o o of.

/ <ra p

^^y^ - ' ^ ^ ' ' ' ^

/ / •

<o o'

-y

Figure 4-38: Force Coefficients on Cube at 0.0625*ro (Point 15) in Simulator (a=0.5, s=2.23)

63

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3

2.5

2

1.5

1

^ .<^

/

.y ^tc^

' 3 . 5 ~ ^ ^

3 — ^

\

\ ) ^ / •cn /

M

" \ \ \ j ?

x10'

Figure 4-39: Force Coefficients on Cube at Center (Point 16) of Simulator (a=1, s=6.72)

64

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4.3.2 Cvlinder Model

Contour plots of force coefficients as a function of position on the

cylindrical model have also been generated for this study. Each figure will

contain a set of three different contour plots that correspond to the top face of the

cylinder and the body of the cylinder. Figure 4-40 shows a map of the exploded

faces of the cylinder. This is held constant throughout all figures. For the top of

the cylinder, plots are of the force coefficient as a function of position on the

cylinder connected with a smooth line. The top left plot will be of the three taps

on the cylinder top face along the west-to-east center-line and the top right plot

will be of the five taps along the north-to-south center line.

South

East West

North

East North West South

Figure 4-40: Schematic of Exploded Cylinder

Points 1 (2.0*ro), 6 (I.OVo), 10 (0.5*ro) and 12 (0.25%) are shown in

Figures 4-41, 4-42, 4-43, and 4-44, respectively. The aspect swiri ratios are a=1

and s=6.72, a=0.5 and s=8.03, a=0.5 and s=2.23, and a=1 and s=1.51,

respectively. Due to the cylinder's geometry, each case of swiri and aspect ratio

65

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behaves much the same when the cylinder Is positioned between 2.0*ro and

0.25*ro from the center of the simulator. The major difference In each case Is the

magnitude of the force coefficients. All cases show that there are positive force

coefficients on the cylinder. The greatest force coefficients occur on the north­

east portion of the cylinder for all cases. The roof of the cylinder experiences

very small force coefficients on the entire face for each case shown. The force

coefficients decrease In a uniform manner as they progress around the cylinder

starting at the northeastern portion of the cylinder. Also, the flow around the

cylinder is approximately uniform in the northwest and southeast portions of the

cylinder Indicating a flow pattern similar to the pattern on a similar model in a

boundary layer flow. The coefficients are all positive due to the fact that the local

surface pressure measured without any model present is lower than the local

pressure recorded on the cylinder, and possibly that the local velocities are

disrupted In such a way that they are lower when the model is in the simulator,

thus increasing the local pressure.

As found by Holroyd using oil storage tanks [37], the force coefficient

pattern Induced on each of these figures Is strongly Indicative of the helical air

flow induced by a horseshoe vortex. This horseshoe vortex consists of a very

strong circumferential component and a weaker downward flow [37], The

stagnation point for each figure lies on the northeastern portion of the cylinder.

The region of minimum pressure lies between the southwest and the northeast

portions of the cylinder. This minimum pressure point could Indicate a separation

of flow from the cylinder.

66

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XlO''

5 0

Vortex

Figure 4-41: Force Coefficients on Cylinder at 2.0% (Point 1) in Simulator (a=1, s=6.72)

5 0

Vortex

Figure 4-42: Force Coefficients on Cylinder at 1.0*ro (Point 6) in Simulator (a=0.5, s=8.03)

67

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XlO' 3

2

1

C 0

-1

-2

-3 1

W

1.5 2.5

3.5 •

3 •

2.5 •

2 •

1.5 •

- \

_

1

% 1 \ /

v

IN O

~ i 1

c

M \ I

I \ CO I \ tJl I

-0.3

-

I / / / /

/ /

0.4-

/ P

' -y ,

* =)

1 1 1

CO I d 1 0.35

1

o > O. /

1 / ^

y ^ ^

,

\ y

/ , /

W Vortex

Figure 4-43: Force Coefficients on Cylinder at 0.5*ro (Point 10) in Simulator (a=0.5, s=2.23)

3

2

1

5 0

-1

-2

-3 1 W

1.5 2.5

Vortex

Figure 4-44: Force Coefficients on Cylinder at 0.25% (Point 12) in Simulator (a=1, s=1.51)

68

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Figure 4-45 and Figure 4-46 show the force coefficients on the cylinder at

a=0.5 and s=2.23 and at a=1 and s=6.72, respectively, at 0.125*ro (point 14) In

the tornado simulator, but they are representative of all cases of aspect ratio and

swiri ratio when the cylinder is at this location in the tornado simulator. The

greatest force coefficients recorded on the cylinder continue to be in the north­

eastern portion of the cylinder. Although the horseshoe vortex continues to be

indicated by these plots, the force coefficients on the southeast portion of the

cylinder are now greater than the force coefficients on the northwest portion of

the cylinder. This indicates that the vortex formed In the tornado simulator is

having significant impact on the flow field around the cylinder. The flow that Is

converging toward the vortex Is causing greater forces on the southeast portion

of the cylinder because the tangential flow is moving from east to west, and the

cylinder Is north of the vortex. This causes a possible flow separation from the

cylinder on the northwest side while not separating from the south-east side of

the cylinder but separating more towards the east side of the cylinder. Also, the

top face has an increased force coefficient on the west side Indicating a possible

flow separation from the top of the cylinder on the northeast side and

reattachment or slight reattachment to the cylinder on the west portion of the top

face. These contour plots also show the force coefficients starting to distribute

themselves more around the cylinder rather than vertically on the cylinder. At

these points in the simulator, the cylinder Is very close to the visualized vortex If

not touching the visualized inner vortex.

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4

35

3

25

2

1.5

o 'p-

\ \ A \ \

^

\

1 T

/

— 0.4

'[] /

i \

-

/ 6 W

Vortex

Figure 4-45: Force Coefficients on Cylinder at 0.125*ro (Point 14) in Simulator (a=0.5, s=2.23)

x10'

O 0

Vortex

Figure 4-46: Force Coefficients on Cylinder at 0.125% (Point 14) in Simulator (a=1, s=6.72)

70

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Force distributions on the cylinder at the center of the tornado vortex

simulator (point 16) at a=0.5, s=2.23 and a=1, s=6.72 and at 0.0625% (point 17)

at a=0.5, s=8.03 and a=1, s=1.51 are shown in Figures 4-47, 4-48, 4-49, and 4-

50, respectively. The greatest force coefficients acting on the cylinder at the

center of the simulator are In the north-east region of the cylinder for all cases,

but they are toward the west portion of the cylinder for 0.0625*ro (point 17). The

greatest forces are toward the west portion of the simulator at point 17 due to the

fact that at this point, the cylinder Is located on the south side of the vortex.

At the center of the simulator, in the low swiri cases (s=2.23 and s=1.51),

the force coefficient distribution propagates around the cylinder from greatest to

least force. The lowest force coefficients are found at the base of the cylinder

while the greatest force coefficients are found near the top of the cylinder. The

top In the low swiri cases have great suction forces which are fairiy evenly

distributed acting on them. For the case of high swiri (s=8.03 and s=6.72), the

force coefficients on the cylinder propagate around the cylinder from greatest to

least starting at the north-east region of the cylinder. Where the force

coefficients In the low swiri case were increasing from base to top of cylinder, the

forces In the high swiri case were much more evenly distributed from top to

bottom, and went from greatest to least force as these vertical asymptotes

propagated around the cylinder.

Force coefficients on the cylinder at 0.0625*ro (point 17) show the greatest

force coefficient on the western portion of the cylinder for the s=2.23 and s=1.51

cases, and the greatest force coefficients on the south-western portion of the

cylinder for the s=8.03 and s=6.72 cases. At this point, the cylinder Is positioned

very close to the center of the simulator, and the force coefficients on the body of

the cylinder are close to equal at different heights all the way around the cylinder.

The force coefficients also are lowest at the bottom portion of the cylinder and

Increase as the cylinder Increases vertically. The force coefficients on the roof of

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each cylinder are negative except for the s=6.72 case, where the force

coefficients are positive on the roof of the model.

Figure 4-47: Force Coefficients on Cylinder at Center (Point 16) in Simulator (a=0.5, s=2.23)

72

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Figure 4-48: Force Coefficients on Cylinder at Center (Point 16) in Simulator (a=1, s=6.72)

x10'

5 0

Figure 4-49: Force Coefficients on Cylinder at 0.0625*ro (Point 17) in Simulator (a=0.5, s=8.03)

73

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xlC

Figure 4-50: Force Coefficients on Cylinder at 0.0625% (Point 17) in Simulator (a=1, s=1.51)

The remainder of the positions tested in the simulator with the cylindrical

model behaved similariy to the positions shown above. They are different only in

the fact that all of the figures shown, with the exception of the 0.0625*ro (point

17) figures, were shown with the cylinder on the north side of the vortex. If the

cylinder is located on the south side of the vortex, the greatest and least force

coefficient values will be on the opposite side of the cylinder at each respective

position tested. These figures are included in Appendix A.

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4.4 Transient Analvsis Since tornadoes do not remain stationary In nature, a transient analysis

was also performed on the cubical and cylindrical models In the tornado

simulator to compare the force distribution from the stationary tests to determine

if the added complexity of a dynamic test is needed. According to Wang [32], the

rotational speed of a typical Fujita scale F2 tornado Is estimated to range

anywhere from 50-70m/s. Using single-channel hot film anemometry, the

rotating speed of the vortices at eaves height in the TTU TVS II ranges between

3-17m/s. Using these results and applying kinematic similarity, a scale factor

was calculated and is presented in Table 4-2.

Table 4-2: Velocity Scale Factor Range in TTU TVS 11

Rotating Speed in TTU TVS II (m/s)

3-17

Rotating Speed F2 tomado (m/s)

50-70

Scale Factor

2.9-23

Also, according to Wang [32], the translational speed of a typical F2

tornado is estimated to be between 0 and 13m/s. Using a mid value for velocity

scale factor of 13m/s, the moving tests scale to a 9.75m/s translation speed of a

natural tornado when a translation speed of 0.75m/s Is used in the TTU TVS II.

In order to take these measurements, the ZOCEIM scanning module was

employed. The ZOCEIM was connected to a switch that could be tripped to

record a predetermined voltage. Using this data combined with the fact that the

Scanlvalve system was set up to record data at 300Hz and the knowledge that

the model would move a predetermined distance, the model was pulled through

the tornado simulator, tripping switch so that the ZOCEIM would record a voltage

at the predetermined starting and stopping points. This gave the number of

frames of data sampled at 300Hz that the model traversed In the given distance.

Using this information, the speed of the model could be obtained. Equation 4.1

was used to obtain the moving force coefficient, and a series of the runs are

plotted traversing the simulator. One representative run of the series has a 6

point moving average trend line added in order to better understand and smooth

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the data. A 6 point moving average trend line was chosen because it was the

greatest number of points that provided representative data.

4.4.1 Transient Cube

The same cubical model used in the stationary tests In the TTU TVS II

was used for the moving tests performed. Twenty total runs were performed at

each aspect ratio and each swiri ratio with the cube. The average speed of the

twenty runs was calculated and the twelve runs that had the least amount of

deviation from this average were selected for detailed analysis. The greatest

percent error of deviation from the average velocity for each case is shown In

Table 4-3.

Table4-3:

Greatest Percent Error fi-om

Average Velocity

Cube Model Percent Error from Average Velocity

a=0.5, s=low

11.7

a=0.5, s=high

6.3

a=1, s=low

7.2

a=1, s=high

9.1

Several distinctive locations on the cube were selected to be analyzed for

the transient analysis. On the top face of the cube, the leading edge and trailing

edges were picked due to their significance. The leading edge is defined as the

edge that gives the positive dot product of the velocity and the outward normal of

the cube. The trailing edge is the edge that gives the negative dot product of the

velocity and the outward normal of the cube. Since the cubical model does not

have a centeriine of pressure taps, the two center pressure taps on the leading

edge of the top face and the two center taps on the trailing edge of the top face

were averaged to obtain data that would correspond to the center of the leading

and trailing edges. The leading edge of the cube will be defined as the edge

adjacent to the south face of the cube. This edge Is adjacent to the leading face

of the cube as It traverses through the TTU TVS II. The trailing edge Is just the

opposite edge of the leading edge, and Is adjacent to the north face of the cube.

The trailing edge is adjacent to the trailing face of the cube as it traverses

through the TTU TVS II. The two other points to be studied on the cubical model 76

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are the center of the south face of the cube and the center of the north face of

the cube. These faces represent the leading and trailing faces of the cube as It

traverses the TTU TVS II.

At an aspect ratio of 0.5 and s=2.23, figures are shown for the leading

edge, the trailing edge, the center of the leading face, and the center of the

trailing face on the cube (Figure 4-51, Figure 4-52, Figure 4-53, and Figure 4-54).

Each figure shows raw data from several of the moving tests, 6-polnt moving

average for a representative moving test series, and the values of the force

coefficients on the cube for the stationary cases as the cube traverses the

simulator. The leading and trailing edges of the roof show that at around

+0.25*ro(a negative ro value Indicates that the model has not passed through the

vortex core, positions 1-15 in Figure 4-27), the force coefficients are lowest,

although the leading edge has a larger force coefficient in magnitude. These

figures show that the values for the moving data are very representative of the

values for the stationary data. The leading, or south, face of the cube shows a

negative force coefficient at approximately -0.25*ro. From this point, the force

coefficient gets larger until the maximum force coefficient Is reached at the center

of the simulator. The force coefficient then decreases until it levels off when the

cube reaches approximately 0.25*ro In the simulator. After leveling off, the force

coefficient is slightly larger than It was at the points before -0.25*ro. The trailing,

or north, face of the cube, as expected, has force coefficients just opposite of the

south face. The force coefficient is fairiy constant until the cube reaches a point

approximately -0.25*ro, when the force coefficient Increases, until it Is at its

maximum at the center of the simulator. At this point, the force coefficient

decreases until the cube Is at approximately 0.25*ro, where the force coefficient

is lowest. The force coefficient then Increases again until the cube Is at

approximately 0.5*ro where the force coefficients level off to an approximate

constant level, just lower in magnitude than the force coefficients on the trailing

face before the cube Is at -0.25*ro. These figures show that although the data for

the moving tests have slightly different magnitudes than the data for the

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stationary tests, the stationary tests show the same trends as the moving tests

for all cases. However, the transient data can be larger than either the moving

average or the stationary data by as much as 50 percent (Figures 4-53 and 4-

54).

Stationary

-Moving Average

Figure 4-51: Force Coefficients at Leading Edge on Roof of Cube (a=0.5, s=2.23)

78

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•Moving Average

Stationary

Figure 4-52: Force Coefficients on Trailing Edge on Roof of Cube (a=0.5, s=2.23)

•Moving Average

Stationary

Figure 4-53' Force Coefficients on Center of Leading Face of Cube (a=0.5, s=2.23) 79

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•Moving Average

Stationary

Figure 4-54: Force Coefficients on Center of Trailing Face of Cube (a=0.5, s=2.23)

Figure 4-55, Figure 4-56, Figure 4-57, and Figure 4-58 show the leading

edge, trailing edge, leading face, and trailing face force coefficients, respectively,

of the cube at a=0.5 and s=8.03. The leading and trailing edges of the roof show

very similar patterns for this case as they did in the s=2.23 case, but the

magnitudes are much greater. They both show that there Is a large force

coefficient at the center of the simulator. Also, both figures show that the lowest

force coefficients occur at approximately +0.25*ro, but rather than abruptly

Increasing to positive values, the force coefficients Increase rather slowly,

indicating that the vortex in the s=8.03 case Is larger in diameter than In the

s=2.23 case. The force coefficients on the leading, south, and trailing, north,

faces also are very similar in the s=8.03 case to the s=2.23 case, but they are

much greater In magnitude In the s=8.03 case. These faces also show the

slower decrease and Increase around the +0.25ro regions of the simulator

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Indicating once again a larger vortex diameter. These figures also show, as the

figures before did, that the data from the moving tests closely corresponds with

the data from the stationary tests.

Stationary

•Moving Average

Figure 4-55: Force Coefficients on Leading Edge of Roof of Cube (a=0.5, s=8.03)

81

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Figure 4-56: Force Coefficients on Trailing Edge of Roof of Cube (a=0.5, s=8.03)

• Stationary

^ ^ M o v i n g Average

r/ro

Figure 4-57: Force Coefficients on Center of Leading Face of Cube (a=0.5, s=8.03)

82

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-25

• Stationary

•"••Moving Average

Figure 4-58: Force Coefficients on Center of Trailing Face of Cube (a=0.5, s=8.03)

Force coefficients on the leading edge, trailing edge, leading face, and

trailing face of the cube are shown in Figures 4-59 through 4-62, respectively, for

a=1, s=1.51. The leading and trailing edges on the roof of the cube show a

different trend for a=1 case than they did for the a=0.5 case. They each still have

the largest force coefficient at the center of the simulator, but the leading edge

has an abrupt decrease in force coefficient when the cube reaches approximately

-0.25*ro and the trailing edge has an abrupt decrease in force coefficient when

the cube reaches approximately 0.25*ro where the largest In magnitude force

coefficient Is reported. These trends are similar to the trends seen on the cube

faces rather than edges in the a=0.5 cases. The leading and trailing faces

continue to behave as they did In the previous cases. The windward face, as It

approaches the vortex, has force coefficients that decrease, then Increase, and

then level off just as In previous cases, and the leeward face, as it approaches

the vortex, has force coefficients that Increase, then decrease, then level off just

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as In previous cases. The moving test data Is representative of the stationary

test data in all cases except for the trailing edge of the cube where the stationary

data Is very different from the moving data. This could be due to a flaw in the

stationary data since the moving data was repeated several times and these

repetitions showed a general trend.

- + * •

" stationary

^ ^ M o v i n g Average

Figure 4-59: Force Coefficients on Leading Edge of Roof of Cube (a=1, s=1.51)

84

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- 4 T 5 -

Stationary

•Movmg Average

Figure 4-60: Force Coefficients on Trailing Edge of Roof of Cube (a=1, s=1.51)

Figure 4-61: Force Coefficients on Center of Leading Face of Cube (a=1, s=1.51) 85

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stationary

•Moving Average

Figure 4-62: Force Coefficients on Center of Trailing Face of Cube (a=1, s=1.51)

Figure 4-63, Figure 4-64, Figure 4-65, and Figure 4-66 show force

coefficients acting on the cube at leading edge, trailing edge, leading face, and

trailing face, respectively, at a=1 and s=6.72. These figures are much like those

from the a=0.5 and s=2.23 case, only slightly different in magnitude. The

patterns that the force coefficients produced for the a=0.5 and s=2.23 case are

the same as the patterns that the force coefficients produced for the a=1, s=6.72

case. Also, the moving test data is very representative of the stationary test data

at a=1 and s=6.72 for all of the cases shown.

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- 4 - 1 -

-2.5

Stationary

•Moving Average

Figure 4-63: Force Coefficients on Leading Edge of Roof of Cube (a=1, s=6.72)

stationary

"Moving Average

Figure 4-64: Force Coefficients on Trailing Edge of Roof of Cube (a=1, s=6.72)

87

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^^Mov ing Average

• Stationary

Figure 4-65: Force Coefficients on Center of Leading Face of Cube (a=1, s=6.72)

• stationary

^ ^ M o v i n g Average

Figure 4-66* Force Coefficients on Center of Trailing Face of Cube (a=1, s=6.72) 88

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The flow regime around the cube behaves in much the same way at each

aspect ratio and each swiri ratio considered with the exception of the roof of the

cube In the a=1 and s=1.51 case. The major difference in the resulting data

when the aspect ratio and swiri ratios are changed Is the magnitude of the data.

These tests also showed that overall, the moving tests data was very

representative of the stationary tests data with the exception being in the a=1 and

s=1.51 case. This indicates that future testing on cubical models can be done In

the stationary case rather than the moving case and yield approximately the

same results, although in some specific cases the results could be off by up to 50

percent, and the same trends. Performing only stationary tests on the cubical

model would greatly simplify the experimental process.

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4.4.2 Transient Cvlinder

As with the cubical model, the same cylinder model that was used In the

stationary tests In the TTU TVS II was used for the moving tests performed.

Twenty total runs were performed at each aspect ratio and each swiri ratio with

the cylinder. The average speed of the 20 runs was calculated and the 12 runs

that had the least amount of deviation from this average were selected to be

used to analyze force coefficients on the cylinder as it traversed the simulator.

The greatest percent error of deviation from the average velocity for each case Is

shown in Table 4-4.

Table 4-4: Cylinder Model Percent Error from Average Velocity

a=0.5, s=2.23

Greatest Percent Error from

Average Velocity 6.03

a=0.5, s=8.03

3.7

a=1, s=1.51

3.9

a=1, s=6.72

15

Several distinctive locations on the cylinder model were selected to be

analyzed for the transient analysis. On the top face of the cylinder, the leading

edge and trailing edges were picked due to their significance. The leading edge

of the cylinder will be defined as the edge adjacent to the south side of the

cylinder and results In the positive dot product of the velocity and outward normal

direction of the cylinder. This edge is adjacent to the leading side of the cylinder

as It traverses through the TTU TVS II. The trailing edge is just the opposite

edge of the leading edge, and Is adjacent to the north side of the cylinder. The

trailing edge is adjacent to the trailing side of the cylinder as It traverses through

the TTU TVS II. The two other points to be studied on the cylindrical model are

the center of the south side of the cylinder and the center of the north side of the

cylinder. These sides represent the leading and trailing sides of the cylinder as It

traverses the TTU TVS 11.

Figures 4-67 through 4-70 show the force coefficients on the cylinder at

the leading edge, the trailing edge, the leading side, and the trailing side, 90

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respectively, for a=0.5 and s=2.23. This case for the cylinder looks much like the

same case for the cube. The leading and trailing edges are fairiy constant, and

at about +0.25*ro the force coefficient decreases to a negative value. At the

center of the simulator, the force coefficient is at its maximum value. The force

coefficient on the leading side of the cylinder decreases slightly at approximately

-0.25*ro and increases to Its maximum value at the center of the simulator. It

then decreases again until the cylinder Is at approximately 0.25*ro where It

seems to level off at a magnitude slightly larger than It was before the cylinder

reached -0.25*ro. The trailing side of the cylinder behaves slightly differently. At

approximately -0.25*ro the force coefficient Increase until It is at a maximum at

the center of the simulator. It then decreases to a minimum value at

approximately 0.25*ro. The force coefficient on the trailing side of the cylinder

then increases slightly until it levels off at a magnitude slightly lower than the

magnitude of the force coefficient on the cylinder before it reached -0.25*ro in the

simulator. The moving test data corresponds to the stationary test data on the

leading edge and leading side of the cylinder, but the stationary test data has a

much lower force coefficient value at 0.25*ro for the trailing edge and trailing side

of the cylinder. Although the magnitudes of the force coefficients are different,

the moving test results continue to follow the general trends of the stationary test

results.

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stationary

•Moving Average

Figure 4-67: Force Coefficients on Leading Edge of Roof of Cylinder (a=0.5, s=2.23)

Figure 4-68: Force Coefficients on Trailing Edge of Roof of Cylinder (a=0.5, s=2.23) 92

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Stationary

•Moving Average

Figure 4-69: Force Coefficients on Leading Side of Cylinder {a=0.5, s=2.23)

stationary

•Moving Average

Figure 4-70" Force Coefficients on Trailing Side of Cylinder (a=0.5, s=2.23)

93

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Figure 4-71, Figure 4-72, Figure 4-73, and Figure 4-74 show force

coefficients on the cylinder at the leading edge, the trailing edge, the leading

side, and the trailing side, respectively, for a=0.5 and s=8.03. The leading edge

behaves in the same manner as It did for the s=8.03 case, but the trailing edge

behaves differently. The trailing edge of the cylinder behaves In a manner similar

to the leading side of the cylinder in the a=0.5 and s=2.23 case. The force

coefficient decreases to a minimum level when the cylinder reaches

approximately -0.25*ro and then increases to a maximum at the center of the

simulator. The force coefficient on the trailing edge then decreases as the

cylinder progresses through the simulator until It reaches a point approximately

0.25*ro in the simulator where it levels off. Both the leading and trailing sides

have force coefficients that are fairiy stable until the cylinder reaches

approximately -0.5*ro In the simulator. At this point, both sides experience a

decrease in force coefficient until it reaches a minimum value when the cylinder

Is at approximately -0.25*ro in the simulator. The force coefficient then Increases

to a maximum value when the cylinder is at 0.25*ro, where the force coefficient

then decreases and levels out at a magnitude approximately equal to the

magnitude of the force coefficient before the cylinder reached -0.5*ro. The

leading and trailing sides both experience the same force coefficients due to the

fact that the swiri ratio Is very high, meaning that the tangential component of

flow provides a greater contribution to the flow field than the radial component of

flow. The moving test data Is very close to the stationary test data In the leading

edge and leading side cases, but not in the trailing edge or trailing side of the

cylinder. In the trailing edge and trailing side cases, the stationary tests show a

force coefficient that is much lower than the force coefficient for the moving tests

at approximately 0.25*ro.

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-2.5 -2

Stationary

•Moving Average

Figure 4-71: Force Coefficients on Leading Edge of Roof of Cylinder (a=0.5, s=8.03)

stationary

•Moving Average

Figure 4-72' Force Coefficients on Trailing Edge of Roof of Cylinder (a=0.5, s=8.03) 95

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stationary

•Moving Average

Figure 4-73: Force Coefficients on Leading Side of Cylinder (a=0.5, s=8.03)

Stabonary

•Moving Average

Figure 4-74: Force Coefficients on Trailing Side of Cylinder (a=0.5, s=8.03) 96

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Figures 4-75 through 4-78 show force coefficients on the cylinder at the

leading edge, the trailing edge, the leading side, and the trailing side,

respectively, for a=1 and s=1.51. The force coefficients In the leading edge case

follow the trend of the force coefficient decreasing when the cylinder approaches

the point -0.25*ro and then Increasing until the cylinder reaches the center of the

simulator. The force coefficient then decreases until the cylinder reaches

approximately 0.25*ro where the force coefficients start to increase and continue

to Increase until the cylinder reaches a point approximately 0.5*ro where the force

coefficient levels off to a level at approximately the same magnitudes recorded

before the cylinder reaches the -0.25*ro point In the simulator. The leading side

of the cylinder behaves much like the leading side of the cylinder In the a=0.5

and s=8.03 case. The trailing edge and trailing side of the cylinder have force

coefficients that start to decrease slightly at -0.25*ro and then Increases until the

cylinder Is at the center of the simulator. At this point, the force coefficient

decreases until the cylinder reaches approximately 0.25*ro where the force

coefficients Increase and then level out when the cylinder reaches approximately

0.5*ro In the simulator. The moving test data is very different In magnitude from

the stationary test data for each of these cases except for the trailing side case

where the moving test data corresponds to the stationary test data. The overall

trend of the stationary test data loosely matches the trends for the moving test

data.

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-2:fr-

-4 :5 -

r/ro

Stationary

•Moving Average

Figure 4-75: Force Coefficients on Leading Edge of Roof of Cylinder (a=1, s=1.51)

stationary

•Moving Average

Figure 4-76: Force Coefficients on Trailing Edge of Roof of Cylinder (a=1, s=1.51)

98

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2.5 L-

stationary

•Moving Average

Figure 4-77: Force Coefficients on Leading Side of Cylinder (a=1, s=1.51)

-a*-

-4T5-

Z -2.5 -2 -1.5 -1 -0.5

• stationary

^ ^ M o v i n g Average

Figure 4-78: Force Coefficients on Trailing Side of Cylinder (a=1, s=1.51) 99

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Figure 4-79, Figure 4-80, Figure 4-81, and Figure 4-82 show the force

coefficients on the cylinder at the leading edge, the trailing edge, the leading

side, and the trailing side, respectively, for a=1 and s=6.72. The leading edge

and leading side of the cylinder show approximately the same trend as the

cylinder traverses the simulator. The force coefficient starts to decrease when

the cylinder reaches approximately -O.SVQ in the simulator until It reaches a

minimum value when the cylinder is approximately -0.25*ro from the center of the

simulator. The force coefficient then Increases until the cylinder reaches the

center of the simulator where the force coefficient starts to decrease. When the

cylinder reaches approximately 0.25*ro In the simulator the magnitude of the

force coefficient levels off to be approximately constant as the cylinder continues

to traverse the simulator. The trailing edge and trailing side of the cylinder

experience force coefficients just opposite of what the leading edge and leading

side of cylinder experienced. The stationary test results show force coefficients

similar to those experienced by the cylinder In the leading and trailing side cases

for a=0.5 and s=8.03. The force coefficients decrease to a minimum when the

cylinder is at approximately -0.25*ro In the simulator, then increase until the

cylinder reaches the center of the simulator, then decrease to another minimum

when the cylinder reaches approximately 0.25*ro In the simulator, and then level

off as the cylinder continues to traverse the simulator. The moving test data

does not follow the stationary test data very well except for the trailing side case.

100

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Figure 4-79: Force Coefficients on Leading Edge of Roof of Cylinder (a=1, s=6.72)

r/ro

Figure 4-80- Force Coefficients on Trailing Edge of Roof of Cylinder (a=1, s=6.72) 101

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" stationary

^ ^ M o v i n g Average

Figure 4-81: Force Coefficients on Leading Side of Cylinder (a=1, s=6.72)

stationary

"Moving Average

Figure 4-82: Force Coefficients on Trailing Side of Cylinder (a=1, s=6 72)

102

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The flow regime around the cylinder does not behave In the same way at

each aspect ratio and each swiri ratio considered as the flow around the cube.

Some differences In the resulting data occurred when the aspect ratio and swiri

ratios were changed. These tests also showed that overall the stationary tests

data was not very representative of the moving tests data In magnitude, but in

most cases, the trends were somewhat close to one another. This Indicates that

future testing should consider whether stationary or transient tests should be

performed on the cylinder depending on the experimental requirements.

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4.5 Statistical Analvsis Originally, the pressure measurement data was collected by means of a

Scanlvalve DSM 3000 system connected to a ZOC 33/64Px electronic pressure

scanning module at 300Hz for six seconds. This provided 1800 data points for

each data set taken. For the models that were tested, five different data sets

were obtained for each of the 31 positions In the tornado simulator. This means

that each pressure tap on the model would have five separate data sets of 1800

points each for each of the 31 positions In the simulator. Statistical data is

presented for the north and south faces and the center of the roof on the cube

and cylinder when each Is positioned at the center of the tornado simulator and

at 2.0*ro In the simulator.

The first step was to obtain the mean value of each data set for each

pressure tap for each of the five runs. The data that was reported was obtained

by taking the mean of the five runs at each position. This is. In fact, the mean of

the means of the data which gives a representative value of what the pressure

difference would be for each pressure tap at any given time. The mean values of

the five different runs when the cubical and cylindrical models were placed at the

center (point 16) and at 2.0*ro in the tornado simulator are shown in Tables 4-5,

4-6, 4-7, 4-8, 4-9, and 4-10. These mean values are the values which were used

to calculate the force coefficients on the cube and cylinder In the previous two

sections.

The standard deviation values were also calculated using the five mean

values found and are shown below for the cube and cylinder at the center of the

tornado simulator and at 2.0*ro In the simulator on the north and south faces and

at the center of the roof. The standard deviation for all cases Is very small, so

the distribution should be concentrated towards the center of the normal

distribution. The skewness was calculated using the raw data obtained from the

five different data sets described above. Most of the skewness values are

negative indicating the normal distribution is skewed to the right of the centeriine.

These negative skewness values also indicate slow. Infrequent variations In

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pressure below the mean [37]. The positive values for skewness indicate that

the normal distribution is skewed to the left of the centeriine. The kurtosis was

found using the same raw data used to find the skewness. To have the same

peak height as the normal distribution, the kurtosis should equal 3. Each of the

cases where the kurtosis Is negative has a distribution curve that is more flat than

the normal distribution curve, and each of the cases where the kurtosis Is positive

has a distribution curve that Is more peaked than the normal distribution curve.

Very high kurtosis values like the ones shown for the center of the roof of the

cylinder at the center of the simulator indicate an increase in the high-frequency

content of the fluctuating pressure signals read by the Scanlvalve system [37].

Table 4-5

Mean St. Dev.

Skewness Kurtosis

: Statistical Values at Center of Roof on Cube and Cylinder at Center of Simulator

Cube Roof Center a=0.5, 8=2.23 -0.403 0.030 -0.608 4.444

a=0.5, s=8.03 -0.682 0.038 -0.011 -0.237

a=1, 8=1.51 -0.303 0.030 -1.072 4.048

a=1, 8=6.72 -0.628 0.008 0.035 0.085

Cylinder Roof Center a=0.5, 8=2.23 -0.586 0.033 -3.212 25.957

a=0.5, s=8.03 1.387 0.031 -0.367 0.369

a=1, 8=1.51 -0.150 0.006 -2.908 29.739

a=1, 8=6.72 -0.611 0.030 -0.405 0.432

Table 4-6: Statistical Values at Center of Roof on Cube and Cylinder at 2.0*ro in Simulator

Mean St. Dev.

Skewness Kurtosis

Cube Roof Center a=0.5, 8=2.23 -0.024 0.001 -0.007 0.035

a=0.5, 8=8.03 -0.030 0.001 -0.054 0.033

a=1, 8=1.51 -0.004 0.001 0.021 -0.028

a=1, 8=6.72 -0.035 0.002 -0.089 0.027

Cylinder Roof Center a=0.5, s=2.23 -0.021 0.001 -0.020 0.062

a=0.5, 8=8.03 -0.030 0.001 0.036 -0.062

a=1, s=1.51 -0.010 0.001 0.005 0.077

a=1, 8=6.72 -0.024 0.001 -0.056 0.120

Table 4-7: Statistical Values on North Face of Cube and Cylinder at Center of Simulator

Mean St. Dev.

Skewness Kurtosis

Cube North Face a=0.5, 8=2.23 -0.185 0.018 -0.713 0.662

a=0.5, s=8.03 -0.606 0.021 -1.134 1.500

3=1, s=1.51 -0.135 0.024 -0.991 1.869

3=1, 8=6.72 -0.582 0.014 -0.426 0.237

Cylinder North Side 3=0.5, 8=2.23 -0.205 0.011 -0.596 0.575

3=0.5, 8=8.03 -0.761 0.053 -0.294 0.022

3=1, 8=1.51 -0.444 0.028 -0.860 1.086

a=1, s=6.72 -0.614 0.029 -0.309 0.164

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Table 4-8: Statistical Values on North Face of Cube and Cylinder at 2.0*ro in Simulator

Mean St. Dev.

Skewness Kurtosis

Cube North Face 3=0.5, 8=2.23 -0.0140 0.0007 -0.0067 -0.0178

a=0.5, 8=8.03 0.0050 0.0007 0.0349 -0.0397

3=1, 8=1.51 0.0152 0.0008 0.0004 -0.0669

3=1, 8=6.72 -0.0033 0.0017 -0.0778 0.2493

Cylinder North Side 3=0.5, 8=2.23 0.0001 0.0005 -0.0286 0.0355

3=0.5, 8=8.03 -0.0144 0.0013 0.0231 -0.0199

3=1, 8=1.51 -0.0131 0.0012 -0.0041 0.0186

3=1. 8=6.72 -0.0142 0.0027 -0.0290 -0.0343

T3ble 4-9: Statistical Values on South Face of Cube and Cylinder at Center of Simulator

Mean St. Dev.

Skewness Kurtosis

Cube South Face 3=0.5, s=2.23 -0.127 0.007 -0.296

3,490.000

3=0.5, 8=8.03 -0.683 0.044 -0.364 0.109

3=1, 8=1.51 0.007 0.005 -0.743 1.496

3=1, s=6.72 -0.618 0.014 -0.254 0.052

Cylinder South Side 3=0.5, s=2.23 -0.339 0.013 -0.509 0.326

3=0.5, 8=8.03 -0.967 0.058 -0.244 0.039

3=1, s=1.51 -0.183 0.010 -0.280 -0.055

3=1, 8=6.72 -0.652 0.038 -0.708 1.011

Table 4-10: Statistical Values on South Face of Cube and Cylinder at 2.0% in Simulator

Mean St. Dev.

Skewness Kurtosis

Cube South Face a=0.5, 8=2.23 -0.015 0.001 0.001 -0.031

3=0.5, s=8.03 -0.023 0.001 -0.045 -0.033

3=1, s=1.51 -0.733 0.001 0.004 0.000

a=1, 8=6.72 -0.015 0.002 -0.050 0.069

Cylinder South Side 3=0.5, s=2.23 -0.022 0.001 -0.052 -0.033

3=0.5, 8=8.03 -0.028 0.000 -0.031 -0.056

a=1, 8=1.51 0.002 0.001 0.007 0.011

3=1, s=6.72 -0.021 0.002 0.021 -0.095

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CHAPTER 5

CONCLUSIONS AND RECOMMENDATIONS

5.1 Conclusions

A Ward-type tornado simulator has been built using a configuration of 16

slotted jets instead of a rotating screen to create the required far field circulation

needed to produce a tornado-like vortex. This configuration provided an aspect

ratio In the same range as the aspect ratio reported for natural tornadoes [8], but

produced a swiri ratio that was unique to the Texas Tech University Tornado

Vortex Simulator II. Flow visualization data, velocity data and pressure data

were all obtained using the simulator. The observed vortices that were produced

ranged from a rope-like, single-celled vortex to a much larger diameter, two-

celled vortex.

Helium bubbles were used to visualize the vortices In the convergent

region of the tornado simulator. As the swiri ratio, the ratio of the tangential flow

rate to the flow rate at the updraft hole, was increased from zero, a small

protrusion of a vortex was observed in the center of the updraft hole. Continuing

to increase the swiri ratio, the vortex of bubbles descended to until it reached the

surface of the TTU TVS II. At this point, the vortex was a rope-like, single-celled

vortex. Velocity and flow rate measurements were obtained with the TTU TVS II

in the same configuration as It was when the single-celled vortex was observed

in order to calculate the swiri ratio acting in the TTU TVS II at this configuration.

This would be the swiri ratio used for the low swiri cases in the pressure tests. At

an aspect ratio of a=0.5, this swiri ratio was s=2.23 and at a=1, this swiri ratio

was 1.51. As the swiri ratio continued to Increase, an adverse pressure gradient

starts to occur spawning the 'breakdown bubble' at the top of the vortex. This

•bubble' forms the boundary between the supercritical flow upstream and the

subcritical flow downstream. The supercritical flow upstream of the breakdown

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bubble Is very similar, In appearance, to the single-celled vortex described

eariier. However, the subcritical flow downstream is tripped by the bubble and is

turbulent in nature. As the tangential flow rate Is Increased, the bubble moves

down the vortex toward the surface of the simulator. This causes a deceleration

In the axial direction of the vortex inner core and eventually, an actual downdraft

in the very center of the vortex. This central down flow region Is surrounded by

the vertical vorticity of upflow. When the breakdown bubble reaches the surface

of the simulator, the core of the vortex expands radially and the down flow in the

central core penetrates to the surface. When the combination of the updraft and

downdraft are each present when the breakdown bubble has penetrated the

vortex core to the surface of the simulator, the vortex Is defined as two-celled.

Again, velocity and flow rate measurements were obtained with the TTU TVS II In

the two-celled vortex configuration. This would be the swiri ratio used for the

high swiri cases in the pressure tests. At a=0.5, this swiri ratio was s=8.03 and at

a=1, this swiri ratio was 6.72. The swiri ratios calculated are unique to the TTU

TVS II.

In order to study low-rise structure Interaction In tornadic winds, pressure

data was obtained on a cubical and cylindrical model that were positioned at

various radial locations within the simulator. The models were also subjected to

moving tests through the TTU TVS II in order to compare the stationary data to

the moving data. Using the pressure data, non-dimensional force coefficients

were calculated and contour plots of the force coefficients on the cube and

cylinder were generated for the stationary tests while, for the moving tests,

specific points on the models were chosen, and the force coefficients at these

points were plotted as a function of position in the TTU TVS II. These plots

indicate that the cubical model severely disrupts the flow at the center of the

simulator.

The stationary tests show that both the cube and the cylinder models

experience flow patterns, at different points In the TTU TVS II, similar to that of

models In a boundary layer-type flow. At s=2.23 and s=1.51 (low swiri ratios)

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when the cube Is positioned between O.SVo and 2.0*ro In the tornado simulator,

the pattern of force coefficients seen on the cube indicates a pattern of flow like

that of the pattern associated with a boundary layer-type flow. When the cylinder

is between 0.25*ro and 2.0*ro in the TTU TVS II at s=2.23, s=1.51, s=8.03 and

s=6.72, the force coefficient contour plots also indicates a pattern of flow which Is

associated with that of a boundary layer type flow. Also for these cases for the

cylinder, the contour plots indicate a horseshoe vortex forms around the cylinder.

In a very small region of the simulator, 0.125*ro for s=2.23 and s=1.51 and

0.125*ro to 0.25*ro in the simulator for s=8.03 and s=6.72, the cubical model

experiences the pattern of flow similar to that of a boundary layer-type flow, but

with the flow Impinging on the east or west (side) faces of the cube rather than

the north or south faces. This Indicates that the model is very close to the

converging vortex, and the tangential flow component of the flow field Is the

major contributor to the flow on the model. At the center of the simulator, both

the cylinder and the cube disrupt the flow field significantly. Also, at this point,

the flow field Is very complex and at the present time the experimental equipment

and data are not sufficient to quantify the flow In this region. At all other points in

the simulator, the flow field comprised of the radial and tangential components of

flow are acting on the cubical and cylindrical models In such a way that the force

coefficients indicate a combination of each of the components of flow.

For the moving tests performed on the cube and cylinder in the TTU TVS

II, several interesting points on each model were chosen to study. The leading

and trailing edges of the roof as well as the leading and trailing sides of each

model were chosen and force coefficients were calculated and plotted as a

function of radial position in the TTU TVS II. Each of these moving tests had

approximately the same trends for the leading edge and side and the trailing

edge and side with a few exceptions. The force coefficient on the leading edge

and side of each model was fairiy constant until the model reached a point

approximately -0.25*ro away from the center of the simulator. At this point In the

simulator, the force coefficients on the leading edge and side of each model

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decreased to a minimum value when the model reached a point between

-0.25*ro and the center of the simulator before starting to Increase again. The

force coefficients Increase until the model reaches the center of the simulator

where the force coefficient starts to decrease again. The force coefficient

decreases until the model reaches approximately 0.25*ro In the simulator where

the force coefficient levels off to approximately the same as the level when the

model was between -2.0*ro and -0.25*ro In the simulator. The trailing edge and

side of each model behaves In a manner similar to the leading edge and side,

only on the opposite side of the simulator. This Is the way that the force

coefficients behave in most of the moving tests.

An important note is that the stationary test data followed the trends of the

moving test data In most cases tested. This would mean that less significance

could be placed on the much more complicated moving tests and more

significance on the less complicated stationary tests In future testing. The

stationary tests are much easier to perform and control than the moving tests, so

a greater quantity of experimental data could be collected easier with the

stationary tests.

Limited statistical analysis was also performed on the data. This showed

that standard deviation for all cases is very small, so the distribution should be

concentrated towards the center of the normal distribution. Most of the skewness

values are negative Indicating the normal distribution is skewed to the right of the

centeriine. These negative skewness values also Indicate slow, Infrequent

variations In pressure below the mean [37]. Very high kurtosis values like the

ones shown for the center of the roof of the cylinder at the center of the simulator

indicate an increase In the high-frequency content of the fluctuating pressure

signals read by the Scanlvalve system [37].

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5.2 Recommendations

Several recommendations can be made for future work using the TTU

TVS II or other Ward-type tornado simulators utilizing the slotted jet design.

• Increasing the scale of the simulator and Increasing the swiri ratio should

produce greater vortex breakdown and ultimately, multiple vortices.

• A less intrusive velocity measurement system would be very beneficial In

collecting data due to the fact that It would not Interrupt the flow regime.

Ideally, PIV or LDV systems should be used to collect data in such a

complex flow field.

• Longer sampling times and more repeatable data would also be beneficial

In quantifying the flow regime.

• A greater range of swiri ratios should be studied.

• Different building model configurations should also be explored in the

tornado simulator.

I l l

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REFERENCES

1. Tornadoes...Nature's Most Violent Storms (1992). NOAA. Retrieved July 10, 2003, from ftp://ftp.nws.noaa.gov/om/brochures/tornado.pdf

2. Davies-Jones, R. P., Tornado Dynamics, In Thunderstorm Morphology and Dynamics, 2"" ed., edited by E. Kessler, pp. 197-236, University of Oklahoma Press, Norman, 1986.

3. YIng, S. J. & Chang, C. C. (1970). Exploratory model study of tornado4ike vortex dynamics. J. Atmos. Sci., 27, 3-14.

4. Ward, Neil B. (1972). The exploration of certain features of tornado dynamics using a laboratory model. J. Atmos. Sci., 29, 1194-1204.

5. Davies-Jones, Robert P. (1973). The dependence of core radius on swiri ratio in a tornado simulator. J. Atmos. Sci., 30, 1427-1430.

6. Jischke, M. C. & Parang, M. (1974). Properties of simulated tornado-like vortices, d. Atmos. Sci., 31, 506-512.

7. Church, C. R. & Snow, J. T. & Agee, E. M. (1977). Tornado vortex simulation at Purdue University. Bull. Amer. Meteor. Soc, 58, 900-908.

8. Church, C. R. & Snow, J. T. & Barnhart, B. J. (1980). An Investigation of the Surface Pressure Fields beneath Simulated Tornado Cyclones. Amer. Meteor. Soc, 37, 1013-1026.

9. Church, C. R. & Snow, J. T. & Baker, G. L. & Agee, E. M. (1979). Characteristics of tornado-like vortices as a function of swiri ratio: A laboratory investigation. J. Atmos. Sci., 36, 1755-1776.

10. Fujita, T. T. (1959). A detailed analysis of the Fargo tornadoes of June 20, 1957. Tech. Rep. No. 5, Severe Local Storms Project, University of Chicago, 129pp.

11. Snow, J. T. & Lund, D. E. (1988). A second generation tornado vortex chamber at Purdue University, In Preprints, 15'^ Conference on Severe Local Storms, pp. 323-326.

12. Church, C. R. & Burgess, D. & Doswell, C. & Davies-Jones, R. P. The Tornado, Its Structure. Dynamics, Prediction and Hazards. American Geophysical Union, Washington, DC, (1993).

13. Church, C. R. & Snow, J. T. (1993). Laboratory models of tornadoes. The Tornado: Its Structure, Dynamics, Prediction, and Hazards, C. Church et al., Eds., Amer. Geophys. Union, 277-296.

14. Wilkins, E. M, & Sasaki & Johnson, H. L. (1975). Surface friction effects on thermal convection in a rotating fluid: A laboratory simulation, Mon. Weather Rev., 103, 305-317.

15. Monji, N. & Wang, Y. (1989). A laboratory investigation of the characteristics of tornado-like vortices over various rough surfaces. Acta Meteorol. Sin., 3,506-515.

112

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16. Davies-Jones, R. P., (1976). Laboratory simulations of tornadoes, in Proceedings ofthe Symposium on Tornadoes: Assessment of Knowledge and Implications of Man, American Meteorological Soc, Boston, Mass., pp. 151-173.

17. Lund, D. E. & Snow, J. T. (1993). Laser Doppler velocimeter measurements in tornadolike vortices. The Tornado: Its Structure, Dynamics, Prediction, and Hazards, C. Church et al., Eds., Amer. Geophys. Union, 297-306.

18. Fiedler, B. H. & Rotunno, R., (1986). A theory for the maximum windspeeds In tornado4ike vortices, d. Atmos. Sci., 43, 2328-2340.

19. Cleland, J. D. (2001). Laboratory measurements of velocity profiles In simulated tornado-like vortices. J. Undergrad. Res. Physics, 18, 51-57.

20. Church, C. R. & Snow, J. T. (1985). Measurements of axial pressures In tornado4lke vortices, J. Atmo. Sci., 42, 576-582.

21. Pauley, R. L. (1989). Laboratory measurements of axial pressures in two-celled tornado-like vortices. J. Atmo. Sci., 46, 3392-3399.

22. Jlschke, M. C. & Light, B. D. (1983). Laboratory simulation of tornadic wind loads on a rectangular structures. Proceedings ofthe Sixth International Conference on Wind Engineering.

23. Jischke, M. C. & Light, B. D. (1979). Laboratory simulation of tornadic wind loads on a cylindrical structures. Proceedings ofthe Sixth International Conference on Wind Engineering, pp 1049-1059.

24. Chang, C. C. (1971). Tornado wind effects on buildings and structures with laboratory simulation. Proceedings ofthe Third International Conference on Wind Effects on Buildings and Structures, pp. 231-240.

25. Bienkiewicz, B. & Dudhia, P. (1993). Physical modeling of tornado-like flow and tornado effects on building loading. The 7'^ US National Conference on Wind Engineering, pp. 95-104.

26. Wang, H. (2001). Fluid-Structure Interaction of a Tornado-Like Vortex With Low-Rise Structures. Master's Thesis.

27. Rotunno, R. (1979). A study In tornado-like vortex dynamics, d. Atmos. Sci., 36, 140-155.

28. Harlow, F. H. & Stein, L. R. (1974). Structural analysis of tornado-like vortices. J. Atmos. Sci., 31, 2081-2098.

29. Nolan, D. S. & Farrell, B. F. (1999). The structure and dynamics of tornado-like vortices. J. Atmos. Sci., 56, 2908-2936.

30. Wicker, L. J., & Wilhelmson, R. B. (1995). Simulation and analysis of tornado development and decay within a three-dimensional supercell thunderstorm, d. Atmos. Sci., 52, 2675-2703.

31. Lewellen, D. C. & Lewellen, W. S. (1996). Large eddy simulations of a tornado's interaction with the surface. 78"' Conference on Severe Local Storms, pp. 392-395.

32. Selvam, R. P., Computer modeling of tornado forces on buildings. 33. Selvam, R. P. & Millett, P. C. (2003). Computer modeling of the tornado-

structure Interaction: investigation of structural loading on cubic building.

113

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Proceedings of 1V^ International Conference on Wind Engineering, pp 837-844.

34. Chi, S. W. & JIh, J. (1974). Numerical modeling of the three-dimensional flows in the ground boundary layer of a maintained axisymmetrical vortex. Tellus, 26, pp. 444-455.

35. Howells, P. & Smith, R. K. (1983). Numerical simulations of tornado4lke vortices. Geophys. Astrophys. Fluid Dynamics, 27, 253-284.

36. Smith, D. R. (1986). Effect of boundary conditions on numerically simulated tornado-like vortices. J. Atmo. Sci., 44, 648-656.

37. Holroyd, R. J. (1983). On the behaviour of open-topped oil storage tanks in high winds. Part I. Aerodynamic aspects. J. Wind Eng. Ind. Aero., 12, 329-352.

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APPENDIX A

LIST OF CONTOUR PLOTS OF FORCE COEFFICIENTS ON CUBE AND

CYLINDER INCLUDED ON CD

115

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The following figures are on the CD Included.

Page In Word Doc. On CD

A l : Cube at 2.0*ro (a=0.5, s=2.23. North of Vortex) 3

A2: Cubeat1.0*ro(a=0.5, s=2.23. North of Vortex) 4

A3: Cube at 0.5*ro (a=0.5, s=2.23, North of Vortex) 5

A4: Cube at 0.25% (a=0.5, s=2.23, North of Vortex) 6

A5: Cube at 0.125*ro (a=0.5, s=2.23. North of Vortex) 7

A6: Cube at 0.0625% (a=0.5, s=2.23. North of Vortex) 8

A7: Cube at Center (a=0.5, s=2.23) 9

A8: Cube at 0.0625*ro (a=0.5, s=2.23. South of Vortex) 10

A9: Cube at 0.125% (a=0.5, s=2.23. South of Vortex) 11

A10: Cube at 0.25% (a=0.5, s=2.23. South of Vortex) 12

A l l : Cubeat0.5%(a=0.5,s=2.23, South of Vortex) 13

A12: Cube at 1.0% (a=0.5, s=2.23, South of Vortex) 14

A13: Cubeat2.0%(a=0.5,s=2.23, South of Vortex) 15

A14: Cubeat2.0%(a=0.5, s=8.03, North of Vortex) 16

A15: Cube at 1.0% (a=0.5, s=8.03. North of Vortex) 17

A16: Cube at 0.5% (a=0.5, s=8.03, North of Vortex) 18

A17: Cube at 0.25% (a=0.5, s=8.03. North of Vortex) 19

A18: Cube at 0.125% (a=0.5, s=8.03, North of Vortex) 20

A19: Cubeat0.0625%(a=0.5,s=8.03, North of Vortex) 21

A20: Cube at Center (a=0.5, s=8.03) 22

A21: Cubeat0.0625%(a=0.5,s=8.03, South of Vortex) 23

A22: Cube at 0.125% (a=0.5, s=8.03, South of Vortex) 24

A23: Cube at 0.25% (a=0.5, s=8.03. South of Vortex) 25

A24: Cube at 0.5% (a=0.5, s=8.03, South of Vortex) 26

A25: Cube at I.OVo (a=0.5, s=8.03. South of Vortex) 27

A26: Cubeat2.0*ro(a=0.5,s=8.03, South of Vortex) 28

A27: Cube at 2.0% (a=1, s=1.51. North of Vortex) 29

116

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A28: Cube at 1.0% (a=1, s=1.51. North of Vortex) 30

A29: Cube at 0.5% (a=1,s=1.51. North of Vortex) 31

A30: Cube at 0.25*ro (a=1, s=1.51. North of Vortex) 32

A31: Cube at 0.125% (a=1,s=1.51. North of Vortex) 33

A32: Cube at 0.0625% (a=1,s=1.51. North of Vortex) 34

A33: Cube at Center (a=1, s=1.51) 35

A34: Cube at 0.0625*ro(a=1,s=1.51, South of Vortex) 36

A35: Cube at 0.125% (a=1, s=1.51, South of Vortex) 37

A36: Cube at 0.25% (a=1,s=1.51, South of Vortex) 38

A37: Cube at 0.5% (a=1, s=1.51, South of Vortex) 39

A38: Cube at 1.0% (a=1, s=1.51, South of Vortex) 40

A39: Cube at 2.0% (a=1, s=1.51. South of Vortex) 41

A40: Cubeat2.0%(a=1,s=6.72, North of Vortex) 42

A41: Cube at 1.0% (a=1, s=6.72. North of Vortex) 43

A42: Cubeat0.5%(a=1,s=6.72, North of Vortex) 44

A43: Cube at 0.25% (a=1,s=6.72. North of Vortex) 45

A44: Cube at 0.125% (a=1,s=6.72, North of Vortex) 46

A45: Cube at 0.0625% (a=1, s=6.72. North of Vortex) 47

A46: Cube at Center (a=1,s=6.72, ) 48

A47: Cube at 0.0625% (a=1, s=6.72. South of Vortex) 49

A48: Cube at 0.125% (a=1, s=6.72. South of Vortex) 50

A49: Cube at 0.25% (a=1, s=6.72, South of Vortex) 51

A50: Cube at 0.5% (a=1, s=6.72, South of Vortex) 52

A5^: Cube at 1.0% (a=1,s=6.72. South of Vortex) 53

A52: Cubeat2.0%(a=1,s=6.72, South of Vortex) 54

A53: Cylinder at 2.0% (a=0.5, s=2.23, North of Vortex) 55

A54: Cylinder at 1.0% (a=0.5, s=2.23. North of Vortex) 56

A55: Cylinder at 0.5% (a=0.5, s=2.23, North of Vortex) 57

A56: Cylinder at 0.25% (a=0.5, s=2.23. North of Vortex) 58

117

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A57

A58

A59

A60

A61

A62

A63

A64

A65

A66

A67

A68

A69

A70

A71

A72

A73

A74

A75

A76

A77

A78

A79

A80

A81

A82

A83

A84

A85

: Cylinde

Cyllnde

Cylinde

Cyllndei

Cylindei

Cyllndei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylindei

Cylinder

Cylindei

Cylinder

Cylinder

Cylinder

'a t

•at

'at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

•at

at

at

0.125*ro (a=0.5, s=2.23. North of Vortex) 59

0.0625*ro (a=0.5, s=2.23. North of Vortex) 60

Center (a=0.5, s=2.23) 61

0.0625% (a=0.5, s=2.23, South of Vortex) 62

0.125% (a=0.5, s=2.23. South of Vortex) 63

0.25% (a=0.5, s=2.23. South of Vortex) 64

0.5% (a=0.5, s=2.23. South of Vortex) 65

1.0%(a=0.5, s=2.23. South of Vortex) 66

2.0% (a=0.5, s=2.23. South of Vortex) 67

2.0%(a=0.5,s=8.03, North of Vortex) 68

1.0%(a=0.5,s=8.03, North of Vortex) 69

0.5*ro (a=0.5, s=8.03. North of Vortex) 70

0.25% (a=0.5, s=8.03. North of Vortex) 71

0.125% (a=0.5, s=8.03. North of Vortex) 72

0.0625*ro (a=0.5, s=8.03. North of Vortex) 73

Center (a=0.5, s=8.03) 74

0.0625% (a=0.5, s=8.03. South of Vortex) 75

0.125*ro (a=0.5, s=8.03. South of Vortex) 76

0.25% (a=0.5, s=8.03, South of Vortex) 77

0.5*ro (a=0.5, s=8.03. South of Vortex) 78

1.0%(a=0.5, s=8.03. South of Vortex) 79

2.0*ro (a=0.5, s=8.03. South of Vortex) 80

2.0%(a=1,s=1.51, North of Vortex) 81

1.0%(a=1,s=1.51, North of Vortex) 82

0.5*ro (a=1, s=1.51. North of Vortex) 83

0.25% (a=1, s=1.51. North of Vortex) 84

0.125*ro(a=1, s=1.51, North of Vortex) 85

0.0625% (a=1, s=1.51. North of Vortex) 86

Center (a=1, s=1.51) 87

118

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Inder at 0.0625% (a=1,s=1.51, South of Vortex) 88

inder at 0.125% (a=1, s=1.51. South of Vortex) 89

inderat0.25%(a=1,s=1.51, South of Vortex) 90

Inder at 0.5*ro(a=1, s=1.51, South of Vortex) 91

Inderal 1.0*ro(a=1, s=1.51, South of Vortex) 92

Inder at 2.0% (a=1, s= 1.51, South of Vortex) 93

Inder at 2.0% (a=1, s=6.72. North of Vortex) 94

inder at 1.0% (a=1, s=6.72, North of Vortex) 95

Inder at 0.5*ro(a=1, s=6.72. North of Vortex) 96

Inderat0.25%(a=1,s=6.72, North of Vortex) 97

Inder at 0.125% (a=1,s=6.72. North of Vortex) 98

Inder at 0.0625% (a=1,s=6.72. North of Vortex) 99

inder at Center (a=1, s=6.72) 100

inder at 0.0625*ro (a=1, s=6.72, South of Vortex) 101

A100: Cylinder at 0.125*ro(a=1,s=6.72, South of Vortex) 102

A101: Cylinder at 0.25% (a=1, s=6.72, South of Vortex) 103

A102: Cylinder at 0.5% (a=1, s=6.72. South of Vortex) 104

A103: Cylinder at 1.0% (a=1, s=6.72. South of Vortex) 105

A104: Cylinder at 2.0% (a=1, s=6.72. South of Vortex) 106

A86

A87

A88

A89

A90

A91

A92

A93

A94

A95

A96

A97

A98

A99

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

Cyl

119

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