Hi there,
I am using feflow6.2 now, I would like to set up a groundwater system with hydraulic links between different aquifers. I have several aquifers and inbetween aquitards. For example, bottom aquifer may get recharge from the top unconfined aquifer cause there is a fault. Or when pumping a single aquifer, those other aquifers which have hydraulic link to it will also have water heads variations. I tried to define the same hydraulic heads bc but as long as there is an aquitard between, the water table did not change at all, means no influence happens between two aquifers. Anyone who knows how to realize that in feflow? My topic is in fact a dewatering problem for several layers, but those layers are all potential water sources and they are also influencing each other.
Thanks in advance.