| | Front Cover |
| | Title Page |
| | Acknowledgement |
| | Table of Contents |
| | List of Tables |
| | List of Figures |
| | Abstract |
| | Introduction |
| | Field and lab studies of the IRL... |
| | Literature review |
| | Model development |
| | Model calibration |
| | Model applications to Indian River... |
| | Conclusions and recommendation... |
| | Appendix A: Turbulence closure... |
| | Appendix B: Derivation of the advection-diffusion... |
| | Appendix C: Numerical solutions... |
| | Appendix D: 1-D wave-current boundary... |
| | Appendix E: Particle erosion simulator... |
| | References |
| | Biographical sketch |
|
| Full Citation |
| Material Information |
| |
Title: |
Modeling suspended sediment transport under combined wave current actions in Indian River Lagoon |
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Physical Description: |
xii, 234 leaves : ill. ; 29 cm. |
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Language: |
English |
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Creator: |
Sun, Detong, 1965- ( Dissertant ) Sheng, Y. P. ( Thesis advisor ) Dean, Robert G. ( Reviewer ) Mehta, Ashish J. ( Reviewer ) Thieke, Robert J. ( Reviewer ) Reddy, Dr. ( Reviewer ) Motz, Dr. ( Reviewer ) |
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Publisher: |
University of Florida |
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Place of Publication: |
Gainesville, Fla. |
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Publication Date: |
2001 |
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Copyright Date: |
2001 |
| Subjects |
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Subjects / Keywords: |
Coastal and Oceanographic Engineering thesis, Ph.D ( lcsh ) Dissertations, Academic -- Coastal and Oceanographic Engineering -- UF ( lcsh ) |
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Genre: |
bibliography ( marcgt ) theses ( marcgt ) non-fiction ( marcgt ) |
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Spatial Coverage: |
United States--Florida--Indian River Lagoon |
| Notes |
| |
Abstract: |
Aquatic systems that have received nutrient loads for long periods of time accumulate nutrients in bottom sediments. These sediments become a potential source of nutrients to the overlying water column. Sediment bound nutrients can then be released through mineralization of organic matter, followed by resuspension and diffusion of nutrients into the water column. Sediment transport processes are one of the controlling factors in these sediment-nutrient cycles. Accurate understanding of the sediment transport processes is, therefore, very important for water quality studies in the aquatic systems. The Indian River Lagoon (IRL) is a unique estuary of national significance providing home to more than 4300 kinds of plants and animals. However, in recent years, increased population along the shoreline of the IRL and its surroundings has stained its natural resources. The stress caused by the population growth and associated activities have increased total suspended solids (TSS) and nutrient loadings into the lagoon, which have led to poor water quality. In this study, sediment samples have been collected and analyzed in laboratory to obtain sediment parameters such as size distributions, settling velocities, critical shear stresses and erosion rate constants. Four episodic events were conducted during 1997 to 2000 to study sediment resuspension n the IRL, during which waves, currents, water levels, TSS and water quality data were collected. Twelve synoptic events were conducted between April 1997 and May 1998, during with TSS, salinity, and other water quality data were collected at 45 stations. Results of the episodic experiments showed that significant sediment resuspension occurred during these events. To quantitatively study suspended sediment transport in the IRL, a two-group suspended sediment transport model has been developed, in which suspended sediments were categorized into two size groups: a fine group with sediment size less that 62 microns and a coarse group with sediment size larger than 62 microns. Coupled with the CH3D hydrodynamic model, originally developed by Sheng (1986, 1989( and the SMB wave model, the sediment transport model is successfully calibrated with field data. Applications of the model of the IRL successfully simulated the episodic and synoptic events. Results showed that: (1) Resuspension and deposition processes were realistically formulated in the wave model with sufficient accuracy. (2) The internal loadings (sediments resuspended from the bottom) were dominant during the episodic events while for longer term (1 year or longer) the external loadings (sediments from river run-offs and other external sources) were more important. (3) Waves played a very important role in sediment resuspension in the IRL. |
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Thesis: |
Thesis (Ph.D.)--University of Florida, 2001. |
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Bibliography: |
Includes bibliographical references (leaves 221-233). |
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Statement of Responsibility: |
by Detong Sun. |
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General Note: |
Printout. |
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General Note: |
Vita. |
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Funding: |
Technical report (Universtiy of Florida. Coastal and Oceanographic Engineering Dept.) : |
| Record Information |
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Bibliographic ID: |
UF00075316 |
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Volume ID: |
VID00001 |
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Source Institution: |
University of Florida |
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Holding Location: |
University of Florida |
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Rights Management: |
All rights reserved, Board of Trustees of the University of Florida |
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Resource Identifier: |
aleph - 002789914 oclc - 49241355 notis - ANR8097 |
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| Table of Contents |
|
Front Cover
Front Cover
Title Page
Title Page
Acknowledgement
Acknowledgement
Table of Contents
Table of Contents 1
Table of Contents 2
Table of Contents 3
List of Tables
List of Tables
List of Figures
List of Figures 1
List of Figures 2
List of Figures 3
List of Figures 4
Abstract
Abstract 1
Abstract 2
Introduction
Page 1
Page 2
Page 3
Page 4
Page 5
Page 6
Page 7
Page 8
Page 9
Page 10
Page 11
Page 12
Field and lab studies of the IRL sediments
Page 13
Page 14
Page 15
Page 16
Page 17
Page 18
Page 19
Page 20
Page 21
Page 22
Page 23
Page 24
Page 25
Page 26
Page 27
Page 28
Page 29
Page 30
Page 31
Page 32
Page 33
Page 34
Page 35
Page 36
Page 37
Page 38
Page 39
Literature review
Page 40
Page 41
Page 42
Page 43
Page 44
Page 45
Page 46
Page 47
Page 48
Page 49
Page 50
Page 51
Page 52
Page 53
Page 54
Page 55
Page 56
Page 57
Page 58
Page 59
Page 60
Page 61
Page 62
Page 63
Page 64
Page 65
Page 66
Page 67
Page 68
Model development
Page 69
Page 70
Page 71
Page 72
Page 73
Page 74
Page 75
Page 76
Page 77
Page 78
Page 79
Page 80
Page 81
Page 82
Page 83
Page 84
Page 85
Page 86
Page 87
Page 88
Page 89
Page 90
Page 91
Model calibration
Page 92
Page 93
Page 94
Page 95
Page 96
Page 97
Page 98
Page 99
Page 100
Page 101
Page 102
Page 103
Page 104
Page 105
Page 106
Page 107
Page 108
Page 109
Page 110
Page 111
Page 112
Page 113
Page 114
Page 115
Page 116
Page 117
Page 118
Page 119
Page 120
Page 121
Page 122
Page 123
Page 124
Page 125
Page 126
Page 127
Page 128
Page 129
Page 130
Page 131
Page 132
Page 133
Page 134
Page 135
Page 136
Page 137
Page 138
Page 139
Page 140
Page 141
Page 142
Model applications to Indian River Lagoon
Page 143
Page 144
Page 145
Page 146
Page 147
Page 148
Page 149
Page 150
Page 151
Page 152
Page 153
Page 154
Page 155
Page 156
Page 157
Page 158
Page 159
Page 160
Page 161
Page 162
Page 163
Page 164
Page 165
Page 166
Page 167
Page 168
Page 169
Page 170
Page 171
Page 172
Page 173
Page 174
Page 175
Page 176
Page 177
Page 178
Page 179
Page 180
Page 181
Page 182
Page 183
Page 184
Page 185
Page 186
Page 187
Page 188
Conclusions and recommendations
Page 189
Page 190
Page 191
Page 192
Appendix A: Turbulence closure model
Page 193
Page 194
Page 195
Page 196
Appendix B: Derivation of the advection-diffusion equation
Page 197
Page 198
Page 199
Page 200
Appendix C: Numerical solutions to the sediment transport model
Page 201
Page 202
Page 203
Page 204
Appendix D: 1-D wave-current boundary layer model
Page 205
Page 206
Page 207
Page 208
Page 209
Page 210
Page 211
Page 212
Page 213
Page 214
Page 215
Appendix E: Particle erosion simulator test
Page 216
Page 217
Page 218
Page 219
Page 220
References
Page 221
Page 222
Page 223
Page 224
Page 225
Page 226
Page 227
Page 228
Page 229
Page 230
Page 231
Page 232
Page 233
Biographical sketch
Page 234
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