UZF-GWET term on volume budget #1904
Replies: 4 comments 18 replies
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Not sure what is going on here, but i see in your list file that a bunch of cells went dry. In theory, that might be okay if rewetting is on and the answer is good, but in practice a bunch of dry cells is not ideal. I'd suggest you turn on NEWTON and try solving this problem differently. The positive UZF-GWET term is strange, and something doesn't seem right so if that persists we should have a look. |
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If, after making the previously suggested changes, you are still seeing such a large percent discrepancy in the UZF budget, it might be worth adding the |
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An update on this which might be interesting: I did two model runs where the only difference is that one is SQUARE GWET
volume budgetUZF BUDGET FOR ENTIRE MODEL AT END OF TIME STEP 1, STRESS PERIOD 1
PERCENT DISCREPANCY = -35.07 PERCENT DISCREPANCY = -35.07 VOLUME BUDGET FOR ENTIRE MODEL AT END OF TIME STEP 1, STRESS PERIOD 1
PERCENT DISCREPANCY = 13.28 PERCENT DISCREPANCY = 13.28 LINEAR GWET
volume budgetUZF BUDGET FOR ENTIRE MODEL AT END OF TIME STEP 1, STRESS PERIOD 1
PERCENT DISCREPANCY = -136.24 PERCENT DISCREPANCY = -136.24 VOLUME BUDGET FOR ENTIRE MODEL AT END OF TIME STEP 1, STRESS PERIOD 1
PERCENT DISCREPANCY = 98.52 PERCENT DISCREPANCY = 98.52 With the |
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Hey @martclanor, you mention that you are seeing this behavior for both steady state and transient simulations. UZF behaves very differently for these two cases. For steady state simulations, UZF does not track waves and instead does a simple calculation as described in the UZF1 Documentation, shown in italics below. Steady state can be specified for the initial stress period of a simulation when using the UZF1 Package. When steady state is specified for the initial stress period, the ground-water recharge rate computed in UZF1 is set equal to the infiltration rate and ET is not removed from the unsaturated zone. The water content is constant within each model cell during steady state. The specified ET rate is subtracted from the infiltration rate to calculate a steady-state recharge rate. ET can also occur from ground water when the water table is above the ET extinction depth. A uniform water content profile is computed for each active cell, which is used automatically as the initial conditions for a following transient stress period. Steady-state water content profiles may be printed to a file for specified locations. Initial water content values are not required when the initial stress period is specified as steady state. Thus, initial water-content values must not be specified within the UZF1 input file when the first stress period is steady state. Another option for developing initial water content profiles is to run the model for several years while repeating a cycle of infiltration rates. This step may be carried out subsequent to a steady-state simulation. I assume the budget table for each uzf reach shown above is for a steady state simulation. If so, this is why the infiltration exactly equals the GWF term (which is recharge to the water table) and why storage is zero. I would expect this to look differently for a transient run. Sorry if I've misunderstood your situation. By the way, @emorway-usgs is the probably the best person to help with this. I see he's been responding, but he is also on vacation, so we should keep that in mind. |
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Hello all. Perhaps a long shot but I was wondering if anyone can help me make sense how come the UZF-GWET is an inflow instead of an outflow. What does that mean in practice? What could have possibly caused this?
This is the Volume Budget section of my LST file (I'm also attaching the file itself, in case it can help test_uzf.zip):
And also if
UZF BUDGET: OUT: GWF
=VOLUME BUDGET: IN: UZF-GWRCH
=119562.4045
then where is:
VOLUME BUDGET: IN: UZF-GWET
=308195.3352
in
UZF BUDGET: OUT
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