Unconfined calculation with perched water table #2459
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Hello, For a complex problem where multiple confined (and some unconfined) aquifers are overlaying an unconfined aquifer I would like to calculate the correct flux from the overlaying confined layer to the unconfined layer. On the most complex locations we have a total of 3 perched water tables in the soil column. From what I gather, there is an option in MODFLOW 6 for the correct calculation of fluxes from a confined layer to an underlying unconfined layer, namely the PERCHED option in the NPF package for calculation of fluxes (instead of taking the head difference between the two layers, taking difference between the head in the overlaying layer and the bottom of that layer). However as these kind of complex unconfined models are often difficult to converge, it is almost always necessary to use the Newton Rhapson formulation. Unfortunately, the Newton Rhapson formulation does not support the PERCHED option. Is there another way to correctly model the flux from a perched water table in MF6 using the Newton Rhapson formulation or am I simply missing something? In the past (MF2005) we've modelled perched water tables by adjusting the resistance below the confined layer. As this is a MODFLOW 6 model and the vertical conductance between cells is calculated based on both the k33 of the confined and unconfined cell this does not seem possible (as changing the k33 value would also inherently change the incoming flux to the confined cell (from the overlaying layer)). |
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Hi @martinveenvliet, I'm afraid that at the moment we don't have anything that will work for your particular case. There are two things that may help in the future.
Apologies for not having anything that can provide immediate relief. |
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Hi @martinveenvliet, I'm afraid that at the moment we don't have anything that will work for your particular case. There are two things that may help in the future.
Apolo…