Readme.txt

A few introductory runs to the double porous equivalent layer hydrological model
launching the ElmerGrid command allows the build up of the mesh and the compilation of the code
It is running as the basal boundary condition of a small cube.

The runs are :
- SedOnly.sif :
Take into account only the sediment layer by using the "Dirichlet condition = FALSE" in the solver params. for the rest, the input is constant on all the domain, no flux on all but one boundary where a water head is given.
This allow an analytic solution : h(x)=(x^2-2Lx)*(-Q/2T) ;
		L is the size of the domain, Q the input and the the sediment transmitivity

- Coupled.sif :
The same as the preceding but this time with an upper boundary for the sediment layer water head.
This settings allow to use the two layers of the system

How to compile & execute the test:
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ElmerGrid 1 2 cube.grd -boundbound 1 5 7 -boundbound 2 5 7 -boundbound 3 5 7 -boundbound 4 5 8
ElmerSolver SedOnly.sif

Results established:
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19.03.2015
Laure Tavard,LGGE
Froggy cluster (CIMENT: Grenoble University HPC centre)
Revision 58f71b4