| | Front Cover |
| | Title Page |
| | Acknowledgement |
| | Table of Contents |
| | List of Figures |
| | List of Tables |
| | List of symbols |
| | Abstract |
| | Introduction |
| | Vertical structure of suspension... |
| | Approach to vertical transport... |
| | Experiments |
| | Application to Lake Okeechobee |
| | Summary, conclusions and recom... |
| | Appendix A. Description of cores... |
| | Appendix B. Concentration profiles... |
| | Appendix C. Time-concentration... |
| | Bibliography |
|
| Full Citation |
| Material Information |
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Title: |
Erodibility of fine sediment in wave-dominated environments |
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Series Title: |
UFLCOEL |
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Physical Description: |
xvii, 141 leaves : ill. ; 28 cm. |
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Language: |
English |
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Creator: |
Hwang, Kyu-Nam, 1961- ( Dissertant ) Mehta, A. J. ( Reviewer ) Sheng, Y. P. ( Reviewer ) Reddy, K. R. ( Reviewer ) University of Florida -- Coastal and Oceanographic Engineering Laboratory |
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Publisher: |
University of Florida -- Coastal and Oceanographic Engineering Laboratory |
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Place of Publication: |
Gainesville, Fla. |
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Publication Date: |
1989 |
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Copyright Date: |
1989 |
| Subjects |
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Subjects / Keywords: |
Turbidity ( lcsh ) Sediment transport ( lcsh ) Coastal and Oceanographic Engineering thesis M.S Suspended sediments -- Measurement ( lcsh ) Erosion -- Okeechobee, Lake -- Florida ( lcsh ) Coastal and Oceanographic Engineering -- Dissertations, Academic -- UF |
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Genre: |
bibliography ( marcgt ) theses ( marcgt ) non-fiction ( marcgt ) |
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Spatial Coverage: |
United States--Florida--Lake Okeechobee |
| Notes |
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Abstract: |
Prediction of turbidity due to fine grained bed material load under wave action is critical to any assessment of anthropogenic impact on the coastal or lacustrine environment. Waves tend to loosen the mud deposit and generate steep suspension concentration gradients, such that the sediment load near the bottom is typically orders higher than that near the surface. In a physically realistic but simplified manner, a vertical sediment transport model was used to simulate prototype trends in the evolution of fine sediment concentration profiles and corresponding erodible bed depth under progressive, non-breaking wave action. field data collection and laboratory experiments were carried out with Lake Okeechobee bottom sediment to determine the characteristic parameters related tot he fine sediment erodibility under waves. these measured parameters served as input data for the transport model. Prior field observations support the simulated trends, which reveal the genesis of near-bed high concentration fluidized mud layer coupled with relatively low surficial concentrations. It is recognized that estimation of the depth of bottom erosion requires an understanding of mud dynamics and competent in situ sediment concentration profiling. Measurement of sediment concentration in the upper water column alone, without regard to the near bed zone, can lead to an order of magnitude underestimation of the erodible bed depth. |
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Thesis: |
Thesis (M.S.)--University of Florida, 1989. |
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Bibliography: |
Includes bibliographical references (leaves 137-140). |
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Statement of Responsibility: |
by Kyu-Nam Hwang. |
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General Note: |
Typescript. |
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General Note: |
Vita. |
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Funding: |
This publication is being made available as part of the report series written by the faculty, staff, and students of the Coastal and Oceanographic Program of the Department of Civil and Coastal Engineering. |
| Record Information |
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Bibliographic ID: |
UF00076136 |
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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: |
oclc - 22340512 |
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| Downloads |
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| Table of Contents |
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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 Figures
List of Figures 1
List of Figures 2
List of Figures 3
List of Figures 4
List of Tables
List of Tables 1
List of Tables 2
List of symbols
Unnumbered ( 13 )
Unnumbered ( 14 )
Unnumbered ( 15 )
Unnumbered ( 16 )
Unnumbered ( 17 )
Abstract
Abstract
Introduction
Page 1
Page 2
Page 3
Page 4
Vertical structure of suspension under water
Page 5
Page 6
Page 7
Page 8
Page 9
Approach to vertical transport problem
Page 10
Page 11
Page 12
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
Experiments
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
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
Page 69
Page 70
Page 71
Page 72
Page 73
Page 74
Application to Lake Okeechobee
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
Page 92
Page 93
Page 94
Page 95
Page 96
Summary, conclusions and recommendations
Page 97
Page 98
Page 99
Page 100
Page 101
Appendix A. Description of cores from Lake Okeechobee
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
Appendix B. Concentration profiles from settling tests
Page 128
Page 129
Page 130
Page 131
Page 132
Page 133
Appendix C. Time-concentration relationship from erosion tests
Page 134
Page 135
Page 136
Bibliography
Page 137
Page 138
Page 139
Page 140
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