Sediment Transport: Difference between revisions

From CIRPwiki
Jump to navigation Jump to search
No edit summary
Line 1: Line 1:
<big>
<big>
==Lund-CIRP Transport Equations==
==Lund-CIRP==
Camenen and Larson (2005, 2007, and 2008) developed a general sediment transport formula for bed and suspended load under combined waves and currents.  
Camenen and Larson (2005, 2007, and 2008) developed a general sediment transport formula for bed and suspended load under combined waves and currents.  


Line 22: Line 22:
{{Equation|<math> \epsilon = h \biggl( \frac{k_b^3 D_b + k_c^3 D_c + k_w^3 D_w}{\rho} \biggr)^{1/3}  </math>|2=5}}
{{Equation|<math> \epsilon = h \biggl( \frac{k_b^3 D_b + k_c^3 D_c + k_w^3 D_w}{\rho} \biggr)^{1/3}  </math>|2=5}}


=== Soulsby-van Rijn Transport Formula ===
== van Rijn ==


{{Equation|<math> C_{*} = \frac{A_{sb}+A_{ss}}{h} \biggl[ \bigl( U^2 + 0.018 \frac{U_{rms}^2}{C_d} \bigr)^{0.5} - u_{cr} \biggr]^{2.4}  </math>|2=6}}
 
== Watanabe ==
 
 
== Soulsby-van Rijn ==
The equilibrium sediment concentration is calculated as (Soulsby 1997)
{{Equation|<math> C_{*} = \frac{A_{sb}+A_{ss}}{h} \biggl[ \biggl( U_c^2 + 0.018 \frac{U_{rms}^2}{C_d} \biggr)^{0.5} - u_{cr} \biggr]^{2.4}  </math>|2=6}}


----
----
Line 32: Line 38:
|<math> q_{bc} </math> || Bed load transport rate || m<sup>3</sup>/s
|<math> q_{bc} </math> || Bed load transport rate || m<sup>3</sup>/s
|-
|-
|<math> s </math> ||  Relative density|| m
|<math> s </math> ||  Relative density || -
|-
|-
|<math> \theta_{c}  </math> || Shields parameter due to currents || -
|<math> \theta_{c}  </math> || Shields parameter due to currents || -
Line 43: Line 49:
|-
|-
|<math> b_c </math> || Empirical coefficient || -
|<math> b_c </math> || Empirical coefficient || -
|-
|<math> U_c </math> || Current magnitude || m/s
|}
|}
== References ==
* Camenen, B., and Larson, M. (2005). "A bed load sediment transport formula for the nearshore," Estuarine, Coastal and Shelf Science, 63, 249-260.
* Camenen, B., and Larson, M., (2008). "A General Formula for Non-Cohesive  Suspended Sediment Transport," Journal of Coastal Research, 24(3), 615-627. 
* Soulsby, D.H. (1997). "Dynamics of marine sands. A manual for practical applications," Thomas Telford Publications, London, England, 249 p.
* Watanabe, A. (1987). "3-dimensional numerical model of beach evolution," Proceedings Coastal Sediments '87, ASCE, 802-817.

Revision as of 03:07, 16 January 2011

Lund-CIRP

Camenen and Larson (2005, 2007, and 2008) developed a general sediment transport formula for bed and suspended load under combined waves and currents.

Bed load

The current-related bed load transport with wave stirring is given by

  (1)

Suspended load

The current-related suspended load transport with wave stirring is given by

  (2)

The reference sediment concentration is obtained from

  (3)

where the coefficient is given by

  (4)

with being the dimensionless grain size and the kinematic viscosity of water.

The sediment mixing coefficient is calculated as

  (5)

van Rijn

Watanabe

Soulsby-van Rijn

The equilibrium sediment concentration is calculated as (Soulsby 1997)

  (6)

Symbol Description Units
Bed load transport rate m3/s
Relative density -
Shields parameter due to currents -
Shields parameter due to waves and currents -
Critical shields parameter -
Empirical coefficient -
Empirical coefficient -
Current magnitude m/s

References

  • Camenen, B., and Larson, M. (2005). "A bed load sediment transport formula for the nearshore," Estuarine, Coastal and Shelf Science, 63, 249-260.
  • Camenen, B., and Larson, M., (2008). "A General Formula for Non-Cohesive Suspended Sediment Transport," Journal of Coastal Research, 24(3), 615-627.
  • Soulsby, D.H. (1997). "Dynamics of marine sands. A manual for practical applications," Thomas Telford Publications, London, England, 249 p.
  • Watanabe, A. (1987). "3-dimensional numerical model of beach evolution," Proceedings Coastal Sediments '87, ASCE, 802-817.