AgDegNormalFault

E-book: Illustration of calculation of aggradation and degradation of a river reach using the normal flow approximation; with an extension for calculation of the response to a sudden fault along the reach.

bed variationfluvial morphodynamicsfault

true

Contributor(s)

Initial contribute: 2021-09-07

Authorship

:  
University of Illinois at Urbana-Champaign
:  
parkerg@illinois.edu
:  
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Classification(s)

Application-focused categoriesNatural-perspectiveLand regions
Application-focused categoriesNatural-perspectiveOcean regions

Detailed Description

English {{currentDetailLanguage}} English

This program computes 1D bed variation in rivers due to differential sediment transport in which it is possible to allow the bed to undergo a sudden vertical fault of a specified amount, at a specified place and time. Faulting is realized by moving all notes downstream of the specified point downward by the amount of the faulting.

The sediment is assumed to be uniform with size D. All sediment transport is assumed to occur in a specified fraction of time during which the river is in flood, specified by an intermittency. A Manning-Strickler formulation is used for bed resistance. A generic relation of the general form of that due to Meyer-Peter and Muller is used for sediment transport. The flow is computed using the normal flow approximation.

 

模型元数据

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Gary Parker (2021). AgDegNormalFault, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/2b2c5f4c-46b4-411d-b05e-34cfc99244ef
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Contributor(s)

Initial contribute : 2021-09-07

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Authorship

:  
University of Illinois at Urbana-Champaign
:  
parkerg@illinois.edu
:  
View
Is authorship not correct? Feed back

History

Last modifier
Yihan Zhang
Last modify time
2021-09-18
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