sandbox/geoffroy/sourceterm/darcy.h
Friction term : Darcy in saint venant
When the Reynolds number is high (>2000), the stream becomes turbulent. In this case, the friction term can’t be easily solved analytically. Darcy and Weisbach found an empirical law describing this term, it can be written in its full form as : \displaystyle Cf = \frac{f}{8} \frac{q|q|}{h^2}, where f is a free-parameter wich depends on the nature of the soil.
The overloading process is fully explained in poiseuille.h
// Darcy coefficient
double f = 0.5;
We define the function which will replace the update function in the predictor-corrector
void updatedarcy(scalar * evolving, scalar * sources, double dtmax, int numbersource ){
// We first recover the evolving fields
scalar h = evolving[0];
vector u = { evolving[1], evolving[2] };
// Updates for evolving quantities
vector dshu = { sources[1], sources[2] };
foreach(){
if(h[] > dry){
Computing the new field u with an implicit scheme. The term u^2 is linearised.
double s = dtmax*norm(u)*f/(8*h[]);
foreach_dimension()
dshu.x[] -= h[]*u.x[]*s/(1+s)/dtmax;
}
}
}
// Calling of the next source term
numbersource++;
updatesource[numbersource](evolving,sources,dtmax,numbersource);
}
// Overloading
event initdarcy (i = 0){
updatesource[numbersource]=updatedarcy;
numbersource++;
updatesource[numbersource] = fnull;
}