Sediment Transport: Difference between revisions

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=== Suspended load ===
=== Suspended load ===
The current-related suspended load transport with wave stirring is given by
The current-related suspended load transport with wave stirring is given by
{{Equation|<math> \frac{q_s}{\sqrt{ (s-1) g d^3 }} = U c_R \frac{\epsilon}{\w_s} \biggl[ \biggr] </math>|2=2}}
{{Equation|<math> \frac{q_s}{\sqrt{ (s-1) g d^3 }} = U c_R \frac{\epsilon}{w_s} \biggl[ 1 - \exp{ \biggl( - \frac{w_s d}{\epsilon}} \biggr) \biggr] </math>|2=2}}
 
<math> 1 - \exp{ \biggl( - \frac{w_s d}{\epsilon}} \biggr)</math>


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Revision as of 21:46, 15 October 2010

Lund-CIRP Transport Equations

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