Model help:SubsidingFan: Difference between revisions

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|-
|-
| I<sub>f</sub>
| I<sub>f</sub>
| intermittency
| flood intermittency
| -
| -
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| Mprint
| Mprint
| number of printouts
| number of printouts
| -
|-
| T
| fan angle
| degrees
|-
| a
| coefficient in the Engelund-Hansen relation
| -
|-
| n
| exponent in the Engelund-Hansen relation
| -
|-
| S
| channel-forming Shields number (sand)
| -
|-
| P
| coefficient in Parker relation
| -
|-
| N
| exponent in Parker relation
| -
|-
| c
| critical Shields number
| -
|-
| G
| channel-forming Shields number (gravel)
| -
|-
| R
| submerged specific gracity
| -
|-
| t
| time step
| yr
|-
| i
| number of intervals per print
| -
|-
| p
| number of prints
| -
| -
|-
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==Notes==
==Notes==
<span class="remove_this_tag">Any notes, comments, you want to share with the user</span>
For a grain size of < 2 mm the Engelund-Hansen formulation will be used for the bedload, and for a grain size of ≥ 2 mm the Parker bedload formulation will be used, aside from this the diameter is not taken into account for the calculation.
 
In the case of a gravel bed, the wash load is assumed to be sand, and in the case of a sand bed the wash load is assumed to be silt.
 
The initial bed is assumed to be horizontal.


<span class="remove_this_tag">Numerical scheme</span>
The downstream boundary condition is one of vanishing sediment transport, and therefore it is one of vanishing slope.





Revision as of 14:21, 2 May 2011

The CSDMS Help System

SubsidingFan

This model is an calculator for evolution of profiles of fans in subsiding basins.

Model introduction

This model is the calculation of Sediment Deposition in a Fan-Shaped Basin, undergoing Piston-Style Subsidence.

Model parameters

Parameter Description Unit
First parameter Description parameter [Units]
Parameter Description Unit
First parameter Description parameter [Units]

Uses ports

This will be something that the CSDMS facility will add

Provides ports

This will be something that the CSDMS facility will add

Main equations

A list of the key equations. HTML format is supported; latex format will be supported in the future

Notes

For a grain size of < 2 mm the Engelund-Hansen formulation will be used for the bedload, and for a grain size of ≥ 2 mm the Parker bedload formulation will be used, aside from this the diameter is not taken into account for the calculation.

In the case of a gravel bed, the wash load is assumed to be sand, and in the case of a sand bed the wash load is assumed to be silt.

The initial bed is assumed to be horizontal.

The downstream boundary condition is one of vanishing sediment transport, and therefore it is one of vanishing slope.


Examples

An example run with input parameters, BLD files, as well as a figure / movie of the output

Follow the next steps to include images / movies of simulations:

See also: Help:Images or Help:Movies

Developer(s)

Name of the module developer(s)

References

Key papers

Links

Any link, eg. to the model questionnaire, etc.