1999
DOI: 10.1080/00221686.1999.9628254
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A geometrical method for computing the distribution of boundary shear stress across irregular straight open channels

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Cited by 79 publications
(34 citation statements)
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“…This implies an additional sub-model to the 1D model. Based on the merged perpendicular method (noted MP method hereafter, see Khodashenas & Paquier, 1999), the bed shear stress is estimated across the section neglecting transverse bottom slope. Thus, the local hydraulic radius equals the vertical distance from the bottom to the first delimiter, which is either a bissector (geometrical division line between the flow influenced by the bank roughness and the flow influenced by the main channel roughness) or the water surface.…”
Section: Distribution Of Bed Shear Stress Throughout the Sectionmentioning
confidence: 99%
“…This implies an additional sub-model to the 1D model. Based on the merged perpendicular method (noted MP method hereafter, see Khodashenas & Paquier, 1999), the bed shear stress is estimated across the section neglecting transverse bottom slope. Thus, the local hydraulic radius equals the vertical distance from the bottom to the first delimiter, which is either a bissector (geometrical division line between the flow influenced by the bank roughness and the flow influenced by the main channel roughness) or the water surface.…”
Section: Distribution Of Bed Shear Stress Throughout the Sectionmentioning
confidence: 99%
“…With the exception of the methods outlined by Lundgren and Jonnson (1964), Yang and Lim (1997), Zheng and Jin (1998) and Khodashenas and Paquier (1999), the majority of approaches require either a large amount of computer resources or reliance on certain contentious assumptions. The aim of this paper is to examine the possibility of using Shannon's (1948) entropy concept in order to predict the boundary shear stress in open channel flow.…”
Section: Introductionmentioning
confidence: 97%
“…This method fails when channel walls have a steep slope, because the intersection of normal occurs below the water surface. To solve this problem, Khodashenas and Paquier [11] extended the normal area method and predicted shear stress distribution in an irregular cross section of a channel. The shear stress distribution was calculated as follows:…”
Section: Khodashenas and Paquier's Methods (Kpm)mentioning
confidence: 99%
“…Studies have shown that it is di cult to determine the boundary shear stress distribution in an open channel [4][5][6][7][8][9]. To overcome this di culty, empirical, analytical, and simpli ed computational methods have been conducted by several researchers [10][11][12][13][14][15][16][17][18][19][20][21]. Still, even with sophisticated turbulence models, it is challenging to accurately calculate local shear stress values.…”
Section: Introductionmentioning
confidence: 99%
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