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contributor authorChjeng-Lun Shieh
contributor authorChih-Ming Tseng
contributor authorShaohua Marko Hsu
date accessioned2017-05-08T20:43:54Z
date available2017-05-08T20:43:54Z
date copyrightJanuary 2001
date issued2001
identifier other%28asce%290733-9429%282001%29127%3A1%2817%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/25093
description abstractMovable bed experiments from a flume into a basin were conducted to study the development of alluvial deltas. The experimental setup was aimed at the bed-load mode. Results showed that the development of the delta can be divided into three stages. In the first stage, the delta progressed mainly in its length, and a successfully derived equation described the shape of the delta in this stage. In the second stage, the delta developed mainly in its width. The length, width, front thickness, and central thickness of the delta were used to scale the geometric similarity. The plane geometry of deltas can be described using Gaussian functions. Transverse and longitudinal profiles fit the hyperbolic and linear function, respectively. The length, width, and thickness of the delta deposition at the end of the second stage have their own maximum values,
publisherAmerican Society of Civil Engineers
titleDevelopment and Geometric Similarity of Alluvial Deltas
typeJournal Paper
journal volume127
journal issue1
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(2001)127:1(17)
treeJournal of Hydraulic Engineering:;2001:;Volume ( 127 ):;issue: 001
contenttypeFulltext


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