Dear Glenn et. al.,
I am developing a simple model for salinity contamination in an extraction well in a coastal region and would like a sanity check for our methodology of simulating freshwater extraction.
For context, the solver is running in RICHARDS mode, while the domain consists of a 2D transect with a dirichlet pressure condition on the left boundary, a 'far field' diriclet pressure condition on the right, and a 'surf' condition on part of the top boundary representing the shelf that sits below the water surface. An example frame of the salinity is shown below with the pressure condition highlighted in green and the neumann condition in light blue.
We are relatively confident that the subsurface model is correct, and now we would like to add extraction well representation via a point sink with volumetric extraction rate. The extraction rate will be set to be a percentage of the water content of the whole 2D slice. I was wondering if this is a reasonable approach, or if you see something that could be improved.
Here is the part of the input file defining the well:
REGION testwell
COORDINATE 0.000000 0.d0 0.000000
/
FLOW_CONDITION Injection_test
TYPE
RATE VOLUMETRIC_RATE
/
RATE -10.000000 m^3/day
/
TRANSPORT_CONDITION sink
TYPE EQUILIBRIUM
CONSTRAINT sink
CONCENTRATIONS
1e-10 T
/
/
END
SOURCE_SINK test
FLOW_CONDITION Injection_test
TRANSPORT_CONDITION sink
REGION testwell
/
I am also wondering if the concentration is relevant (since it's extracting) and if I could be enlightened on what the equilibrium transport condition does.
Thanks!
Kenton