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azu_td_hy_e9791_1988_161_sip1_w.pdf
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azu_td_hy_e9791_1988_161_sip1_w.pdf
Author
Chanyotha, Seree,1956-Issue Date
1988Committee Chair
Laursen, Emmett M.Peterson, Margaret S.
Metadata
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The University of Arizona.Rights
Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.Abstract
The characteristics and behavior of rivers depend on numerous factors which are highly variable and complex. Sediment characteritics and sediment-transport capacity of rivers are important factors that influence river characteristics. Significant amounts of ground-water inflowing to or outflowing from a river reach affect flow characteristics of that reach, which in turn alter the capability of the reach for transporting sediment and result in changed river characteristics. In addition, inflow from a tributary carrying a sediment load with the same concentration as the main stream increases the capability to transport the sediment load of the downstream reach of the confluence. A simplified mathematical model of a generalized river reach was developed to investigate how ground-water recharge and inflow to the stream and tributary inflow affect and alter river characteristics.Type
Thesis-Reproduction (electronic)text
Degree Name
M.S.Degree Level
mastersDegree Program
Civil Engineering and Engineering MechanicsGraduate College