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Posted 15 years ago by Falk Händel
Hello,

I have a problem with the use of the automatic time step control.
I am modelling an 2 dimensional vertical unsaturated problem with steady flow and transient heat transport.
There is a steady recharge on atmospheric boundary and a time series for heat transport.
If automatic time step control is chosen, the flow of water in the unsaturated area isn´t computed correctly.
The results are unrealistic high hydraulic heads. Using constant time steps (1d) for the whole problem or only steady resp. transient ( time series of recharge) modelling of the flow problem results in realistic data of hydraulic heads.
So what can I do using the automatic time step control for combined flow and heat transport?
Thanks for responses.

Falk
Posted 15 years ago by Denim Umeshkumar Anajwala
Is the model (maybe by mistake) density-dependent or with varying viscosity? Then the time-stepping might have an influence on the resulting heads - even with steady-state flow. Otherwise I would like to ask you to send the model to support@dhi-wasy.de (up to 10 MB) for checking.

Peter
Posted 15 years ago by Falk Händel
Hi,

thanks for the answer.
All density and viscosity effects are on default settings.

Falk

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