Wave Equation and Some Solutions on Intermittent Debris flow

M. Arai
{"title":"Wave Equation and Some Solutions on Intermittent Debris flow","authors":"M. Arai","doi":"10.13101/IJECE.10.39","DOIUrl":null,"url":null,"abstract":"Intermittent surges of debris flows are frequently observed in mountain regions. This type of flow is considered to be characterized by developing roll waves (surges) due to flow instabilities and by weak sediment concentrations. For an understanding of fluctuation of the flow depth, wave equations are needed. It was presented a wave equation of roll waves based on shallow water momentum equation, and analytical solution on an initial and boundary condition and some numerical solutions were shown in this paper. These results show an improved understanding of the phenomena of intermittent debris flow.","PeriodicalId":378771,"journal":{"name":"International Journal of Erosion Control Engineering","volume":"307 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2017-03-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Journal of Erosion Control Engineering","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.13101/IJECE.10.39","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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Abstract

Intermittent surges of debris flows are frequently observed in mountain regions. This type of flow is considered to be characterized by developing roll waves (surges) due to flow instabilities and by weak sediment concentrations. For an understanding of fluctuation of the flow depth, wave equations are needed. It was presented a wave equation of roll waves based on shallow water momentum equation, and analytical solution on an initial and boundary condition and some numerical solutions were shown in this paper. These results show an improved understanding of the phenomena of intermittent debris flow.
间歇泥石流的波动方程及若干解
在山区经常观察到间歇性的泥石流。这种类型的流动被认为是由于流动不稳定和沉积物浓度较低而形成翻滚波(浪涌)的特征。为了理解流深的波动,需要有波动方程。在浅水动量方程的基础上,提出了横摇波的波动方程,给出了初始和边界条件下的解析解,并给出了一些数值解。这些结果表明对间歇性泥石流现象的认识有所提高。
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