INSTABILITY OF THE OPEN CHANNEL FLOW OVER WAVY BED AND THE FREE SURFACE WAVES OBSERVED IN THE RAPIDS OF THE RIVER
-
- Kyotoh Harumichi
- Asian Institute of Technology, Water Resources Engineering Program
-
- Fukushima Masaki
- 社団法人 土木学会 筑波大学大学院 工学研究科
Bibliographic Information
- Other Title
-
- 波状底面を持つ開水路流れの安定性と河川早瀬の波
- 液状底面を持つ開水路流れの安定性と河川早瀬の波
- エキジョウ テイメン オ モツ カイスイロ ナガレ ノ アンテイセイ ト カセ
Search this article
Abstract
Surface waves in the rapids of the river show the complicated patterns which are influenced by the bottom topography. Two-dimensional shallow water equations with dispersion terms are used to discuss the instability of steady nonuiform flows over sinusoidal bed. Floquet's theory shows that quasi-periodic eigenfunctions with respect to spacial variables can be introduced to solve the equation for an infinitesimal disturbance. Here, two physically important spatial patterns, such as Peak-valley structure and Staggered pattern, are investigated and their unstable regions are plotted in the phase plane of Froude number and the wavenumber of the bottom surface. Furthermore, the frequency of the waves observed at the waterside in the rapids will be discussed.
Journal
-
- Doboku Gakkai Ronbunshu
-
Doboku Gakkai Ronbunshu 1996 (539), 69-78, 1996-05-21
Japan Society of Civil Engineers
- Tweet
Details 詳細情報について
-
- CRID
- 1390282680285273344
-
- NII Article ID
- 10001791231
-
- NII Book ID
- AN10014020
-
- ISSN
- 18827187
- 02897806
-
- NDL BIB ID
- 3975035
-
- Data Source
-
- JaLC
- NDL
- Crossref
- CiNii Articles
-
- Abstract License Flag
- Disallowed