Model help:SteadyStateAg: Difference between revisions
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==Main equations== | ==Main equations== | ||
::::{| | ::::{| | ||
|width=500px|<math> | |width=500px|<math>S_{u}= {\frac{R C_{f} ^ \left ( {\frac{1}{2}}\right )} {\alpha _{EH} \tau _{form} ^*}} {\frac{Q_{tbf,feed}}{Q_{bf}}} </math> | ||
|width=50px align="right"|(1) | |width=50px align="right"|(1) | ||
|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>{\frac{S}{S_{u}}} = \left ( 1 - \beta x | |width=500px|<math>{\frac{S}{S_{u}}} = \left ( 1 - \beta \hat{x}\right ) </math> | ||
|width=50px align="right"|(2) | |width=50px align="right"|(2) | ||
|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>\eta | |width=500px|<math>\hat{\eta} = {\frac{\eta_{dev}}{L}} </math> | ||
|width=50px align="right"|(3) | |width=50px align="right"|(3) | ||
|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>x | |width=500px|<math>\hat{x} = {\frac{x}{L}} </math> | ||
|width=50px align="right"|(4) | |width=50px align="right"|(4) | ||
|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>\beta = {\frac{ \left (1 - \lambda _{p} \right ) B_{f} \xi _{d} L}{I_{f} \Omega \left ( 1 + \Lambda \right ) Q_{tbf,feed}}} </math> | |width=500px|<math>\beta = {\frac{ \left (1 - \lambda _{p} \right ) B_{f} \dot{\xi} _{d} L}{I_{f} \Omega \left ( 1 + \Lambda \right ) Q_{tbf,feed}}} </math> | ||
|width=50px align="right"|(5) | |width=50px align="right"|(5) | ||
|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>\eta | |width=500px|<math>\hat{\eta} = S_{u} [ \left ( 1 - {\frac{1}{2}} \beta \right ) - \hat{x} + {\frac{1}{2}} \beta \hat{x} ^2 ] </math> | ||
|width=50px align="right"|(6) | |width=50px align="right"|(6) | ||
|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>\eta = \xi _{do} + \xi _{d} t + \eta _{dev} \left ( x \right ) </math> | |width=500px|<math>\eta = \xi _{do} + \dot{\xi} _{d} t + \eta _{dev} \left ( x \right ) </math> | ||
|width=50px align="right"|(7) | |width=50px align="right"|(7) | ||
|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>{\frac{B_{bf}}{D}} = {\frac{C_{f}}{\alpha _{EH} \left ( | |width=500px|<math>{\frac{B_{bf}}{D}} = {\frac{C_{f}}{\alpha _{EH} \left ( \tau _{form} ^* \right ) ^ \left ( 2.5 \right ) }} {\frac{Q_{tbf}}{\sqrt { R g D } D^2}} </math> | ||
|width=50px align="right"|(8) | |width=50px align="right"|(8) | ||
|} | |} | ||
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|} | |} | ||
::::{| | ::::{| | ||
|width=500px|<math>{\frac{Q_{tbf}}{Q_{tbf,feed}}} = 1 - \beta x | |width=500px|<math>{\frac{Q_{tbf}}{Q_{tbf,feed}}} = 1 - \beta \hat{x} </math> | ||
|width=50px align="right"|(10) | |width=50px align="right"|(10) | ||
|} | |} | ||
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| time interval for plotting | | time interval for plotting | ||
| year | | year | ||
|- | |||
| xhat | |||
| dimensionless downstream coordinate | |||
| - | |||
|- | |||
| x | |||
| downstream coordinate | |||
| km | |||
|- | |||
| Q<sub>tbf</sub> | |||
| volume bed material transport during flood stage | |||
| m<sup>3</sup> / s | |||
|- | |||
| Sl | |||
| bed slope | |||
| - | |||
|- | |||
| ξ<sub>hat</sub> | |||
| dimensionless deviatoric bed elevation | |||
| - | |||
|- | |||
| ξ<sub>dev</sub> | |||
| deviatoric bed elevation | |||
| m | |||
|- | |||
| B<sub>bf</sub> | |||
| bankfull channel width | |||
| m | |||
|- | |||
| H<sub>bf</sub> | |||
| bankfull channel depth | |||
| m | |||
|- | |||
| η | |||
| bed elevation | |||
| m | |||
|- | |||
| T | |||
| channel-forming Shields number | |||
| - | |||
|- | |||
| X | |||
| initial water surface elevation | |||
| m | |||
|- | |||
| t | |||
| time interval for plotting | |||
| yr | |||
|- | |||
| p | |||
| number of prints | |||
| - | |||
|- | |- | ||
|} | |} | ||
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</div> | </div> | ||
==Notes== | ==Notes== | ||
Revision as of 14:07, 2 May 2011

SteadyStateAg
This model is a calculator for approach to equilibrium in recirculating and feed flumes
Model introduction
This program implements the calculation for steady-state aggradation of a sand-bed river in response to sea level rise at a constant rate.
Model parameters
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
<math>S_{u}= {\frac{R C_{f} ^ \left ( {\frac{1}{2}}\right )} {\alpha _{EH} \tau _{form} ^*}} {\frac{Q_{tbf,feed}}{Q_{bf}}} </math> (1)
<math>{\frac{S}{S_{u}}} = \left ( 1 - \beta \hat{x}\right ) </math> (2)
<math>\hat{\eta} = {\frac{\eta_{dev}}{L}} </math> (3)
<math>\hat{x} = {\frac{x}{L}} </math> (4)
<math>\beta = {\frac{ \left (1 - \lambda _{p} \right ) B_{f} \dot{\xi} _{d} L}{I_{f} \Omega \left ( 1 + \Lambda \right ) Q_{tbf,feed}}} </math> (5)
<math>\hat{\eta} = S_{u} [ \left ( 1 - {\frac{1}{2}} \beta \right ) - \hat{x} + {\frac{1}{2}} \beta \hat{x} ^2 ] </math> (6)
<math>\eta = \xi _{do} + \dot{\xi} _{d} t + \eta _{dev} \left ( x \right ) </math> (7)
<math>{\frac{B_{bf}}{D}} = {\frac{C_{f}}{\alpha _{EH} \left ( \tau _{form} ^* \right ) ^ \left ( 2.5 \right ) }} {\frac{Q_{tbf}}{\sqrt { R g D } D^2}} </math> (8)
<math>{\frac{H}{D}} = {\frac{\alpha _{EH} \left ( \tau _{form} ^* \right ) ^2}{C_{f} ^ \left ({\frac{1}{2}} \right )}} {\frac{Q_{bf}}{Q_{tbf}}} </math> (9)
<math>{\frac{Q_{tbf}}{Q_{tbf,feed}}} = 1 - \beta \hat{x} </math> (10)
Nomenclature
Symbol | Description | Unit |
---|---|---|
Gt,feed | mean annual bed material sediment feed rate | Mt / year |
L | reach length (downchannel distance) | km |
Lv | reach length (downvalley distance) | km |
dξd / dt | rate of sea level rise | mm / year |
Qbf | bankfull water discharge | m3 / s |
Bf | floodplain width | km |
D | grain size | mm |
Λ | fraction wash load deposited per unit material load deposited | kg/m3 |
Qtbf,feed | volume bed material sediment transport rate during flood time | - |
C | volume concentration of bed material load | - |
BMSS | flood concentration of bed material load | mg / L |
Su | upstream slope | - |
β | an coefficient to adjust L to make sure that this parameter < 1. If β> 1 then the sediment transport drops to 0 before reaching the delta | - |
τform * | channel-forming Shields number | - |
αEH | coefficient in Engelund-Hansen bed material load relation | - |
λp | bed porosity | - |
If | flood intermittency | - |
Cz | Chezy resistance coefficient | - |
Ω | channel sinuosity | - |
R | submerged specific gravity of sediment | - |
ξdo | water surface elevation at t = 0 | - |
Δt | time interval for plotting | year |
xhat | dimensionless downstream coordinate | - |
x | downstream coordinate | km |
Qtbf | volume bed material transport during flood stage | m3 / s |
Sl | bed slope | - |
ξhat | dimensionless deviatoric bed elevation | - |
ξdev | deviatoric bed elevation | m |
Bbf | bankfull channel width | m |
Hbf | bankfull channel depth | m |
η | bed elevation | m |
T | channel-forming Shields number | - |
X | initial water surface elevation | m |
t | time interval for plotting | yr |
p | number of prints | - |
Notes
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:
- Upload file: http://csdms.colorado.edu/wiki/Special:Upload
- Create link to the file on your page: [[Image:<file name>]].
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.