1952
DOI: 10.1061/taceat.0006641
|View full text |Cite
|
Sign up to set email alerts
|

Regime Theory for Self-Formed Sediment-Bearing Channels

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

1992
1992
2021
2021

Publication Types

Select...
3
2
1

Relationship

0
6

Authors

Journals

citations
Cited by 25 publications
(2 citation statements)
references
References 0 publications
0
2
0
Order By: Relevance
“…The channel-forming or dominant discharge theory stipulates that if there is a unique flow maintained in an alluvial river over a long period of time, it would produce the same bankfull morphology that is shaped by the natural sequence of flows. Even this concept is not an universally accepted method, most practitioners agree that this is applicable in perennial and ephemeral rivers (Blench, 1952;Ackers and Charlton, 1970;Bray, 1975;Biedenharn et al, 2000;USDA, 2001;Soar and Thorne, 2001).…”
Section: Channel-forming Dischargementioning
confidence: 99%
“…The channel-forming or dominant discharge theory stipulates that if there is a unique flow maintained in an alluvial river over a long period of time, it would produce the same bankfull morphology that is shaped by the natural sequence of flows. Even this concept is not an universally accepted method, most practitioners agree that this is applicable in perennial and ephemeral rivers (Blench, 1952;Ackers and Charlton, 1970;Bray, 1975;Biedenharn et al, 2000;USDA, 2001;Soar and Thorne, 2001).…”
Section: Channel-forming Dischargementioning
confidence: 99%
“…These approaches can be broadly classified into three methods, each using the same basic assumption of steady and uniform flow to achieve channel equilibrium. First, empirical equations of the regime have been obtained from the statistical rule/regression analysis of channel geometry data from different rivers (Thomas Blench 1952;Bray 1982;Hey and Thorne 1986a;Leopold and Wolman 1957;Wolman 1954). In these equations, flow discharge, bed shear stress and bedgrain diameters have been considered as the most effective parameters to predict the geometry of stable rivers (Deshpande and Kumar 2012;Parker et al 2007).…”
Section: Introductionmentioning
confidence: 99%