CMS-Flow:Transport Formula: Difference between revisions

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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. These are refered to as the Lund-CIRP transport formulas. The general transport formulas can be used for both symmetric and asymmetric waves but for simplicity the waves are assumed to be symmetric in CMS. The bed load transport rate including the stirring effect of waves is given by

{\frac {q_{b}}{\sqrt {(s-1)gd_{50}^{3}}}}=a_{c}{\sqrt {\theta _{c}}}\theta _{cw,m}\exp {{\biggl (}-b_{c}{\frac {\theta _{cr}}{\theta _{cw}}}}{\biggr )}

(1)

where $q_{b}$ is in m^2/s, $d_{50}$ is the median grain size, $s$ is the sediment specific gravity or relative density, $g$ is gravitational constant, $\theta _{cw,m}$ and $\theta _{cw}$ are the mean and maximum Shields parameters due to waves and currents respectively, $\theta _{c}$ , $\theta _{cr}$ is the critical Shields parameter due to currents, $a_{c}$ and $b_{c}$ are empirical coefficients.

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

{\frac {q_{s}}{\sqrt {(s-1)gd_{50}^{3}}}}=Uc_{R}{\frac {\varepsilon }{\omega _{s}}}{\biggl [}1-\exp {{\biggl (}-{\frac {w_{s}h}{\varepsilon }}}{\biggr )}{\biggr ]}

(2)

where $U$ is the depth-averaged current velocity, $h$ is the total water depth, $\omega _{s}$ is the sediment fall velocity, $\varepsilon$ is the sediment diffusivity, and $c_{R}$ is the reference bed concentration. The reference bed concentration is calculated from

c_{R}=A_{cR}\exp {{\biggl (}-4.5{\frac {\theta _{cr}}{\theta _{cw}}}}{\biggr )}

(3)

where the coefficient $A_{cR}$ is given by

A_{cR}=3.5\times 10^{3}\exp {{\bigl (}-0.3D_{*}}{\bigr )}

(4)

where $\nu$ the kinematic viscosity of water, and $D_{*}$ the dimensionless grain size

D_{*}=d_{50}{\biggl [}{\frac {(s-1)g}{\nu }}{\biggr ]}

(5)

The sediment fall velocity is calculated using the formula by Soulsby (1997)

$\omega _{s}={\frac {\nu }{d}}{\bigg [}{\big (}10.36^{2}+1.049D_{*}^{3}{\big )}^{1/2}-10.36{\bigg ]}$

(6)

The sediment mixing coefficient is calculated as

\epsilon =h{\biggl (}{\frac {k_{b}^{3}D_{b}+k_{c}^{3}D_{c}+k_{w}^{3}D_{w}}{\rho }}{\biggr )}^{1/3}

(7)

where $k_{b},k_{c},andk_{w}$ are coefficients, $D_{b}$ is the wave breaking dissipation, and $D_{c}$ and $D_{w}$ are the bottom friction dissipation due to currents and waves respectively. For more details see Camenen and Larson (2008).

van Rijn

The van Rijn (1984ab) transport equations are used with the recalibrated coefficients of van Rijn (2007ab) are given by

q_{b}=0.015\rho _{s}Uh{\biggl (}{\frac {U_{e}-U_{cr}}{\sqrt {(s-1)gd_{50}}}}{\biggr )}^{1.5}{\biggl (}{\frac {d_{50}}{h}}{\biggr )}^{1.2}

(8)

q_{s}=0.012\rho _{s}Ud_{50}{\biggl (}{\frac {U_{e}-U_{cr}}{\sqrt {(s-1)gd_{50}}}}{\biggr )}^{2.4}D_{*}^{-0.6}

(9)

where $U_{cr}$ is the critical depth-averaged velocity for initiation of motion, $U_{e}$ is the effective depth averaged velocity calculated as $U_{e}=U+0.4U_{w}$ in which $U_{w}$ is the peak orbital velocity based on the significant wave height

The critical velocity is estimated as

U_{cr}=\beta U_{crc}+(1-\beta )U_{crw}

(10)

where $U_{crc}$ and $U_{crw}$ are the critical velocity for currents and waves respectively. As in van Rijn (2007), the critical velocity for currents and waves are calculated based on Komar and Miller (1975):

U_{crc}={\begin{cases}0.19(d_{50})^{0.1}\log {_{10}{\big (}{\frac {4h}{d_{90}}}{\big )}},&{\text{for }}0.1\leq d_{50}\leq 0.5mm\\8.5(d_{50})^{0.6}\log {_{10}{\big (}{\frac {4h}{d_{90}}}{\big )}},&{\text{for }}0.5\leq d_{50}\leq 2.0mm\end{cases}}

(11)

U_{crw}={\begin{cases}0.24[(s-1)g]^{0.66}(d_{50})^{0.33}T_{p}^{0.33},&{\text{for }}0.1\leq d_{50}\leq 0.5mm\\0.95[(s-1)g]^{0.57}(d_{50})^{0.43}T_{p}^{0.14},&{\text{for }}0.5\leq d_{50}\leq 2.0mm\end{cases}}

(12)

According to van Rijn (2007) bed load transport formula predicts transport rates with a factor of 2 for velocities higher than 0.6 m/s, but underpredicts transports by a factor of 2-3 for velocities close to initiation of motion.

Watanabe

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

q_{t}=A_{w}{\biggl [}{\frac {(\tau _{b,max}-\tau _{cr})U}{\rho g}}{\biggr ]}

(13)

where $\tau _{b,max}$ is the maximum shear stress, $\tau _{cr}$ is the critical shear stress of incipient motion, and $A$ is an empirical coefficient typically ranging from 0.1 to 2.

The critical shear stress is determined using

\tau _{cr}=(\rho _{s}-\rho )gd\phi _{cr}

(14)

In the case of currents only the bed shear stress is determined as $\tau _{c}={\frac {1}{8}}\rho gf_{c}U_{c}^{2}$ where $f_{c}$ is the current friction factor. The friction factor is calculated as $f_{c}=0.24log^{-2}(12h/k_{sd})$ where $k_{sd}$ is the Nikuradse equivalent sand roughness obtained from $k_{sd}=2.5d_{50}$ .

If waves are present, the maximum bed shear stress $\tau _{b,max}$ is calculated based on Soulsby (1997)

Failed to parse (unknown function "\tag"): {\displaystyle \tag{15} \tau_{max} = \sqrt{(\tau_m + \tau_w \cos{\phi})^2 + (\tau_w \sin{\phi})^2 } }

(15)

where $\tau _{m}$ is the mean shear stress by waves and current over a wave cycle, math> \tau_w </math> is the mean wave bed shear stress, and $\phi$ is the angle between the waves and the current. The mean wave and current bed shear stress is

\tau _{m}=\tau _{c}{\biggl [}1+1.2{\biggl (}{\frac {\tau _{w}}{\tau _{c}+\tau _{c}}}{\biggr )}^{3.2}{\biggr ]}

(16)

The wave bed shear stress is given by $\tau _{w}={\frac {1}{2}}\rho gf_{w}U_{w}^{2}$ where $f_{w}$ is the wave friction factor, and $U_{w}$ is the wave orbital velocity amplitude based on the significant wave height.

The wave friction factor is calculated as (Nielsen 1992) $f_{w}=\exp {5.5R^{-0.2}-6.3}$ where $R$ is the relative roughness defined as $R=A_{w}/k_{sd}$ and $A_{w}$ is semi-orbital excursion $A_{w}=U_{w}T/(2\pi )$ .

Soulsby-van Rijn

Soulsby (1997) proposed the following equation for the total load sediment transport rate under currents and waves

q_{t}=A_{s}U{\biggl [}{\biggl (}U^{2}+0.018{\frac {U_{rms}^{2}}{C_{d}}}{\biggr )}^{0.5}-U_{cr}{\biggr ]}^{2.4}

(20)

where $U_{rms}$ is the root-mean-squared wave orbital velocity, and $C_{d}$ is the drag coefficient due to currents alone and the coefficient $A_{s}=A_{sb}+A_{ss}$ . The coefficients $A_{sb}$ and $A_{ss}$ are related to the bed and suspended transport loads respectively and are given by

A_{sb}={\frac {0.005h(d_{50}/h)^{1.2}}{[(s-1)gd_{50}]^{1.2}}}

(21)

A_{s}={\frac {0.012d_{50}D_{*}^{-0.6}}{[(s-1)gd_{50}]^{1.2}}}

(22)

The current drag coefficient is calcualted as

C_{d}={\biggl [}{\frac {0.4}{\ln {(h/z_{0})}-1}}{\biggr ]}^{2}

(23)

with a constant bed roughness length $z_{0}$ set to 0.006 m.

Symbol	Description	Units
$q_{bc}$	Bed load transport rate	m³/s
$s$	Relative density	-
$\theta _{c}$	Shields parameter due to currents	-
$\theta _{cw}$	Shields parameter due to waves and currents	-
$\theta _{cw}$	Critical shields parameter	-
$a_{c}$	Empirical coefficient	-
$b_{c}$	Empirical coefficient	-
$U_{c}$	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. (2007). "A unified sediment transport formulation for coastal inlet applications", ERDC/CHL-TR-06-7, US Army Engineer Research and Development Center, Coastal and Hydraulics Laboratory, Vicksburg, MS.
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.
van Rijn, L. C. (1984a). "Sediment transport. Part I: Bed load transport", Journal of Hydraulic Engineering, 110(10), 1431–1456.
van Rijn, L. C. (1984b). "Sediment transport. Part II: Suspended loadtransport", Journal of Hydraulic Engineering, 110(11), 1613–1641.
van Rijn, L.C., (2007a). "Unified View of Sediment Transport by Currents and Waves. I: Initiation of Motion, Bed Roughness, and Bed-load Transport", Journal of Hydraulic Engineering, 133(6), 649-667.
van Rijn, L.C., (2007b). "Unified View of Sediment Transport by Currents and Waves. II: Suspended Transport", Journal of Hydraulic Engineering, 133(6), 668-689.
Watanabe, A. (1987). "3-dimensional numerical model of beach evolution," Proceedings Coastal Sediments '87, ASCE, 802-817.

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@@ Line 1: / Line 1: @@
 =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. These are refered to as the Lund-CIRP transport formulas. The general transport formulas can be used for both symmetric and asymmetric waves but for simplicity the waves are assumed to be symmetric in CMS. The bed load transport rate including the stirring effect of waves is given by
+{{Equation|<math>
-\begin{equation} \tag{1}
+  \frac{q_{b}}{\sqrt{(s-1) g d_{50}^3}} = a_c \sqrt{\theta_c} \theta_{cw,m}\exp{  \biggl ( -b_c \frac{\theta_{cr}}{\theta_{cw}}} \biggr )
-  \frac{q_{b}}{\sqrt{(s-1) g d_{50}^3}} = a_c \sqrt{\theta_c} \theta_{cw,m}\exp{  \biggl ( -b_c \frac{\theta_{cr}}{\theta_{cw}}} \biggr )
+</math>|1}}
-\end{equation}
 where <math>q_{b}</math> is in m^2/s, <math>d_{50}</math> is the median grain size, <math>s</math> is the sediment specific gravity or relative density, <math>g</math> is gravitational constant, <math>\theta_{cw,m}</math> and <math>\theta_{cw}</math> are the mean and maximum Shields parameters due to waves and currents respectively, <math>\theta_{c}</math>, <math>\theta_{cr}</math> is the critical Shields parameter due to currents, <math>a_c</math> and <math>b_c</math> are empirical coefficients.
 The current-related suspended load transport with wave stirring is given by
-\begin{equation} \tag{2}
+{{Equation|<math>
   \frac{q_s}{\sqrt{ (s-1) g d_{50}^3 }} = U c_R \frac{\varepsilon}{\omega_s} \biggl[ 1  - \exp{ \biggl( - \frac{w_s h}{\varepsilon}} \biggr) \biggr]
-\end{equation}
+</math>|2}}
 where <math>U</math> is the depth-averaged current velocity, <math>h</math> is the total water depth, <math>\omega_s</math> is the sediment fall velocity, <math>
 \varepsilon </math> is the sediment diffusivity, and <math>c_R</math> is the reference bed concentration. The reference bed concentration is calculated from
-\begin{equation} c_R = A_{cR}  \exp{ \biggl( - 4.5 \frac{\theta_{cr}}{\theta_{cw}}}  \biggr) \end{equation}
+{{Equation|<math>c_R = A_{cR}  \exp{ \biggl( - 4.5 \frac{\theta_{cr}}{\theta_{cw}}}  \biggr)</math>|3}}
 where the coefficient <math>A_{cR}</math> is given by
-\begin{equation} A_{cR} = 3.5 \times 10^3 \exp{ \bigl( - 0.3 D_{*} } \bigr) \end{equation}
+{{Equation|<math>A_{cR} = 3.5 \times 10^3 \exp{ \bigl( - 0.3 D_{*} } \bigr) </math>|4}}
 where <math> \nu </math> the  kinematic viscosity of water, and <math>D_{*} </math>the dimensionless grain size
-\begin{equation} \tag{5} D_{*} = d_{50} \biggl[ \frac{(s-1) g}{ \nu} \biggr] \end{equation}
+{{Equation|<math>D_{*} = d_{50} \biggl[ \frac{(s-1) g}{ \nu} \biggr] </math>|5}}
 The sediment fall velocity is calculated using the formula by Soulsby (1997)
-\begin{equation} \tag{6}
+{{Equation|
- \omega_s = \frac{\nu}{d} \bigg[ \big( 10.36^2 + 1.049 D_{*}^3 \big)^{1/2} -10.36  \bigg]
+<math>
-\end{equation}
+\omega_s = \frac{\nu}{d} \bigg[ \big( 10.36^2 + 1.049 D_{*}^3 \big)^{1/2} -10.36  \bigg]
+</math>|6}}
 The sediment mixing coefficient is calculated as
-\begin{equation} \tag{7}
+{{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>|7}}
- \epsilon = h \biggl( \frac{k_b^3 D_b + k_c^3 D_c + k_w^3 D_w}{\rho} \biggr)^{1/3}
-\end{equation}
 where <math>k_b, k_c, and k_w</math> are coefficients, <math>D_b</math> is the wave breaking dissipation, and <math>D_c</math> and <math>D_w</math> are the bottom friction dissipation due to currents and waves respectively. For more details see Camenen and Larson (2008).
@@ Line 37: / Line 35: @@
 = van Rijn =
 The van Rijn (1984ab) transport equations are used with the recalibrated coefficients of van Rijn (2007ab) are given by
-\begin{equation} \tag{8}
+{{Equation|<math>
-  q_b = 0.015 \rho_s U h
+q_b = 0.015 \rho_s U h
-   \biggl( \frac{U_e - U_{cr} }{ \sqrt{(s-1) g d_{50}} } \biggr)^{1.5}
+  \biggl( \frac{U_e - U_{cr} }{ \sqrt{(s-1) g d_{50}} } \biggr)^{1.5}
-   \biggl( \frac{d_{50}}{h} \biggr)^{1.2}
+  \biggl( \frac{d_{50}}{h} \biggr)^{1.2}
-\end{equation}
+</math>|8}}
-\begin{equation} \tag{9}
+{{Equation|<math>
    q_s = 0.012 \rho_s U d_{50}
    \biggl( \frac{U_e - U_{cr} }{ \sqrt{(s-1) g d_{50}}} \biggr)^{2.4}
    D_{*}^{-0.6}
-\end{equation}
+</math>|9}}
 where <math>U_{cr}</math> is the critical depth-averaged  velocity for initiation of motion, <math>U_e</math> is the  effective depth averaged velocity calculated as  <math>U_e = U + 0.4 U_w</math> in which <math> U_w</math> is the peak orbital velocity based on the significant wave height
 The critical velocity is estimated as
-\begin{equation} \tag{10} U_{cr} = \beta U_{crc} + (1-\beta) U_{crw} \end{equation}
+{{Equation|<math>U_{cr} = \beta U_{crc} + (1-\beta) U_{crw} </math>|10}}
 where <math>U_{crc}</math> and <math>U_{crw}</math> are the critical velocity for currents and waves respectively. As in van Rijn (2007), the critical velocity for currents and waves are calculated based on Komar and Miller (1975):
-\begin{equation} \tag{11}
+{{Equation|<math>
    U_{crc} =
    \begin{cases}
@@ Line 62: / Line 60: @@
 .5 (d_{50})^{0.6} \log{_{10} \big( \frac{4h}{d_{90}} \big) }, & \text{for } 0.5 \le d_{50} \le 2.0 mm
    \end{cases}
-\end{equation}
+</math>|11}}
-\begin{equation} \tag{12}
+{{Equation|<math>
    U_{crw} =
    \begin{cases}
@@ Line 70: / Line 68: @@
 .95 [(s-1)g]^{0.57} (d_{50})^{0.43} T_p^{0.14}, &  \text{for } 0.5 \le d_{50} \le 2.0 mm
    \end{cases}
-\end{equation}
+</math>|12}}
 According to van Rijn (2007) bed load transport formula predicts transport rates with a factor of 2 for velocities higher than 0.6 m/s,  but underpredicts transports by a factor of 2-3 for velocities close to  initiation of motion.
@@ Line 76: / Line 74: @@
 = Watanabe =
 The equilibrium total load sediment transport rate of Watanabe (1987) is given by
-\begin{equation} \tag{13}
+{{Equation|<math>
- q_{t} = A_w \biggl[ \frac{(\tau_{b,max} - \tau_{cr}) U }{\rho g } \biggr]
+q_{t} = A_w \biggl[ \frac{(\tau_{b,max} - \tau_{cr}) U }{\rho g } \biggr]
-\end{equation}
+</math>|13}}
 where  <math> \tau_{b,max} </math> is the maximum shear stress,  <math> \tau_{cr} </math> is the critical shear stress of  incipient motion, and <math> A </math> is an empirical  coefficient typically ranging from 0.1 to 2.
 The critical shear stress is determined using
-\begin{equation} \tag{14} \tau_{cr} = (\rho_s - \rho) g d \phi_{cr} \end{equation}
+{{Equation|<math>\tau_{cr} = (\rho_s - \rho) g d \phi_{cr} </math>|14}}
 In  the case of currents only the bed shear stress is determined as  <math> \tau_{c} = \frac{1}{8}\rho g f_c U_c^2 </math> where  <math> f_c </math> is the current friction factor. The  friction factor is calculated as <math> f_c =  0.24log^{-2}(12h/k_{sd}) </math> where <math> k_{sd}  </math> is the Nikuradse equivalent sand roughness obtained from  <math> k_{sd} = 2.5d_{50} </math>.
 If waves are present, the maximum bed shear stress <math>\tau_{b,max} </math> is calculated based on Soulsby (1997)
-\begin{equation}
+{{Equation|<math>
- \tag{15} \tau_{max} = \sqrt{(\tau_m + \tau_w \cos{\phi})^2  + (\tau_w \sin{\phi})^2 }
+\tag{15} \tau_{max} = \sqrt{(\tau_m + \tau_w \cos{\phi})^2  + (\tau_w \sin{\phi})^2 }
-\end{equation}
+</math>|15}}
 where  <math> \tau_m </math> is the mean shear stress by waves and  current over a wave cycle, math> \tau_w </math> is the mean  wave bed shear stress, and <math> \phi </math> is the angle  between the waves and the current. The mean wave and current bed shear  stress is
-\begin{equation} \tag{16}
+{{Equation|<math>
    \tau_{m} = \tau_c \biggl[ 1 +  1.2 \biggl( \frac{\tau_w}{\tau_c + \tau_c} \biggr)^{3.2} \biggr]
-\end{equation}
+</math>|16}}
 The wave bed shear stress is given  by <math> \tau_{w} = \frac{1}{2}\rho g f_w U_w^2 </math>  where <math> f_w </math> is the wave friction factor, and  <math> U_w </math> is the wave orbital velocity amplitude  based on the significant wave height.
@@ Line 103: / Line 101: @@
 = Soulsby-van Rijn =
 Soulsby (1997) proposed the following equation for the total load sediment transport rate under currents and waves
-\begin{equation} \tag{20}
+{{Equation|<math>
    q_t = A_s U \biggl[ \biggl( U^2 + 0.018  \frac{U_{rms}^2}{C_d} \biggr)^{0.5} - U_{cr} \biggr]^{2.4}
-\end{equation}
+</math>|20}}
 where <math>U_{rms}</math> is the root-mean-squared wave orbital velocity, and <math>C_d</math> is the drag coefficient due to currents alone and the coefficient <math> A_{s} = A_{sb} + A_{ss} </math>. The coefficients <math>A_{sb}</math> and <math>A_{ss}</math> are related to the bed and suspended transport loads respectively and are given by
-\begin{equation} \tag{21} A_{sb} = \frac{ 0.005 h (d_{50}/h)^{1.2} }{ [(s-1)g d_{50} ]^{1.2} } \end{equation}
+{{Equation|<math>A_{sb} = \frac{ 0.005 h (d_{50}/h)^{1.2} }{ [(s-1)g d_{50} ]^{1.2} } </math>|21}}
-\begin{equation} \tag{22} A_{s} = \frac{ 0.012 d_{50} D_{*}^{-0.6} }{ [(s-1)g d_{50} ]^{1.2} } \end{equation}
+{{Equation|<math>A_{s} = \frac{ 0.012 d_{50} D_{*}^{-0.6} }{ [(s-1)g d_{50} ]^{1.2} } </math>|22}}
 The current drag coefficient is calcualted as
-\begin{equation} \tag{23} C_d =  \biggl[ \frac{0.4}{\ln{(h/z_0)}-1 } \biggr]^2 \end{equation}
+{{Equation|<math>C_d =  \biggl[ \frac{0.4}{\ln{(h/z_0)}-1 } \biggr]^2 </math>|23}}
 with a constant bed roughness length <math>z_0 </math> set to 0.006 m.

CMS-Flow:Transport Formula: Difference between revisions

Revision as of 15:23, 22 October 2012

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Lund-CIRP

van Rijn

Watanabe

Soulsby-van Rijn

References

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CMS-Flow:Transport Formula: Difference between revisions

Revision as of 15:23, 22 October 2012

Lund-CIRP

van Rijn

Watanabe

Soulsby-van Rijn

References

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