Sediment Transport: Difference between revisions

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==Lund-CIRP==
==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.  
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== Watanabe ==
== Watanabe ==
 
The total load sediment transport rate of Watanabe (1987) is given by
{{Equation|<math> q_{t*} = A \biggl[ \frac{(\tau_{b,max} - \tau_{cr}) U_c }{\rho g } \biggr]^{2.4}  </math>|2=6}}


== Soulsby-van Rijn ==
== Soulsby-van Rijn ==
The equilibrium sediment concentration is calculated as (Soulsby 1997)
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}}
{{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=7}}


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Revision as of 03:10, 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

  qb(s1)gd3=acθcθcwexp(bcθcrθcw) (1)

Suspended load

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

  qs(s1)gd3=UcRϵws[1exp(wsdϵ)] (2)

The reference sediment concentration is obtained from

  cR=AcRexp(4.5θcrθcw) (3)

where the coefficient AcR is given by

  AcR=3.5x103exp(0.3d*) (4)

with d*=d(s1)gν2 being the dimensionless grain size and ν the kinematic viscosity of water.

The sediment mixing coefficient is calculated as

  ϵ=h(kb3Db+kc3Dc+kw3Dwρ)1/3 (5)

van Rijn

Watanabe

The total load sediment transport rate of Watanabe (1987) is given by

  qt*=A[(τb,maxτcr)Ucρg]2.4 (6)

Soulsby-van Rijn

The equilibrium sediment concentration is calculated as (Soulsby 1997)

  C*=Asb+Assh[(Uc2+0.018Urms2Cd)0.5ucr]2.4 (7)

Symbol Description Units
qbc Bed load transport rate m3/s
s Relative density -
θc Shields parameter due to currents -
θcw Shields parameter due to waves and currents -
θcw Critical shields parameter -
ac Empirical coefficient -
bc Empirical coefficient -
Uc 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.