Difference between revisions of "MPM BL"

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<div class="title">Meyer-Peter Müeller Bedload Formulation</div>
<div class="title">Meyer-Peter Müeller Bedload Formulation</div>
<wikitex>
 
The [[Bibliography#Meyer-PeterE_1948a | Meyer-Peter Müeller (1948)]] formulation is
The [[Bibliography#Meyer-PeterE_1948a | Meyer-Peter Müeller (1948)]] formulation is
$$
\Phi  = \max \left[ {8\left( {\theta _{sf}  - \theta _c } \right)^{1.5} ,\quad 0} \right]
$$
where $\Phi$ is the magnitude of the non-dimensional transport rate for each sediment class,$\theta _{sf}$ is the non-dimensional Shields parameter for skin stress
$$
\theta _{sf}  = \frac{{\tau _{sf} }}{{\left( {s - 1} \right)gD_{50} }}
$$


$\theta _c  = 0.047$ is the critical Shields parameter, and $\tau _{sf}$ is the magnitude of total skin-friction component of bottom stress computed from
<math display="block">\Phi  = \max \left[ {8\left( {\theta _{sf}  - \theta _c } \right)^{1.5} ,\quad 0} \right]</math>
$$
 
\tau _{sf}  = \left( {\tau _{bx}^2  + \tau _{by}^2 } \right)^{0.5}  
where <math>\Phi</math> is the magnitude of the non-dimensional transport rate for each sediment class, <math>\theta _{sf}</math> is the non-dimensional Shields parameter for skin stress
$$
 
where ${\tau _{bx}}^2$ and ${\tau _{bx}}^2$ are the skin-friction components of bed stress, from currents alone or the maximum wave-current combined stress, in the $x$ and $y$ directions. These are computed at cell faces ($u$ and $v$ locations) and then interpolated to cell centers ($\rho$ points). The bedload transport vectors are partitioned into $x$ and $y$ components based on the magnitude of the bed shear stress as
<math display="block">\theta _{sf}  = \frac{{\tau _{sf} }}{{\left( {s - 1} \right)gD_{50} }}</math>
$$
 
q_{blx}  = q_{bl} \frac{{\tau _{bx} }}
<math>\theta _c  = 0.047</math> is the critical Shields parameter, and <math>\tau _{sf}</math> is the magnitude of total skin-friction component of bottom stress computed from
 
<math display="block">\tau _{sf}  = \left( {\tau _{bx}^2  + \tau _{by}^2 } \right)^{0.5}</math>
 
where <math>{\tau _{bx}}^2</math> and <math>{\tau _{bx}}^2</math> are the skin-friction components of bed stress, from currents alone or the maximum wave-current combined stress, in the <math>x</math> and <math>y</math> directions. These are computed at cell faces (<math>u</math> and <math>v</math> locations) and then interpolated to cell centers (<math>\rho</math> points). The bedload transport vectors are partitioned into <math>x</math> and <math>y</math> components based on the magnitude of the bed shear stress as
 
<math display="block">q_{blx}  = q_{bl} \frac{{\tau _{bx} }}
{{\tau _{sf} }};\quad \quad q_{bly}  = q_{bl} \frac{{\tau _{by} }}
{{\tau _{sf} }};\quad \quad q_{bly}  = q_{bl} \frac{{\tau _{by} }}
{{\tau _{sf} }}
{{\tau _{sf} }}</math>
$$
</wikitex>

Latest revision as of 12:02, 18 May 2016

Meyer-Peter Müeller Bedload Formulation

The Meyer-Peter Müeller (1948) formulation is

where is the magnitude of the non-dimensional transport rate for each sediment class, is the non-dimensional Shields parameter for skin stress

is the critical Shields parameter, and is the magnitude of total skin-friction component of bottom stress computed from

where and are the skin-friction components of bed stress, from currents alone or the maximum wave-current combined stress, in the and directions. These are computed at cell faces ( and locations) and then interpolated to cell centers ( points). The bedload transport vectors are partitioned into and components based on the magnitude of the bed shear stress as