Hi,
Does anyone know the best way of representing time-variant recharge of fresh-water (0 mg/l) into an aquifer that is originally brackish to saline ( up to 5000 mg/l)? Is it best to use injection wells to supply the recharge? The recharge occurs as individual high recharge events, between which there is zero recharge. If I use injection wells then how do I specify that the concentration of the water going in is 0 mg/l, rather than saline?
Cheers,
Gemma ???