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Incisional cyclic steps of permanent form in mixed bedrock-alluvial rivers

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Izumi_et_al-2017-Journal_of_Geophysical_Research__Earth_Surface.pdf1.62 MBPDF見る/開く
この文献へのリンクには次のURLを使用してください:http://hdl.handle.net/2115/66340

タイトル: Incisional cyclic steps of permanent form in mixed bedrock-alluvial rivers
著者: Izumi, Norihiro 著作を一覧する
Yokokawa, Miwa 著作を一覧する
Parker, Gary 著作を一覧する
キーワード: bedrock
cyclic step
incision
macroroughness
abrasion
alluviation
発行日: 2017年 1月
出版者: American Geophysical Union
誌名: Journal of geophysical research earth surface
巻: 122
号: 1
開始ページ: 130
終了ページ: 152
出版社 DOI: 10.1002/2016JF003847
抄録: Most bedrock river channels have a relatively thin, discontinuous cover of alluvium and are thus termed mixed bedrock-alluvial channels. Such channels often show a series of steps formed at relatively regular intervals. This bed form is the bedrock equivalent of cyclic steps formed on beds composed of cohesive soil in gullies. In this paper, we perform a full nonlinear analysis for the case of cyclic steps in mixed bedrock-alluvial channels to explain the formation of these steps. We employ the shallow water equations in conjunction with equations describing the process of bedrock incision. As a model of bedrock incision, we employ the recently introduced Macro-Roughness Saltation Abrasion Alluviation model, which allows direct interaction between alluvial and bedrock morphodynamics. The analysis is greatly simplified by making the quasi-steady assumption that alluvial processes occur much faster than bedrock erosional processes. From our analysis, we obtain the conditions for the formation of cyclic steps in bedrock, as well as the longitudinal profiles of bed elevation, water surface elevation, and areal fraction of alluvial cover. It is found from the analysis that when the sediment supply is small relative to the transport capacity, cyclic steps form only on slopes with very high gradients. The analysis indicates that the shape of a step formed on bedrock is characterized by a relatively short upstream portion with an adverse slope and a long, almost planar downstream portion with a constant slope.
Rights: Copyright 2017 American Geophysical Union. All Rights Reserved.
資料タイプ: article
URI: http://hdl.handle.net/2115/66340
出現コレクション:雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

提供者: 泉 典洋

 

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