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Boundary conditions problems in transient heat transfer
Posted 2 feb 2018, 10:07 GMT-5 Heat Transfer & Phase Change, Modeling Tools & Definitions, Parameters, Variables, & Functions 2 Replies
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Hello,
I tried to make a time dependent 3D heat transfer to the ground simulation for a period of one year. Boundary conditions: h = 24 W/m2K, Te = linear interpolation function, defined at Global Definitions section based on hourly registered real temperatures (introduced as heat flux boundary condition - Robin?..). T ground = 9 deg C (introduced as temperature boundary condition - Dirichlet).
I made 3 different simulations starting with the same steady-state initialization, at the time-step with different simulation periods: 24 h (calculation step 0.2), 760 h, 8760 h (one year). I analised the boundary temperatures (Tsi), heat fluxes during the first 24 h for each simulation and the values were different for the three simulations. Why do I not get the same results?
Is there a limit for the number of input values used for the interpolation function, which may have an effect on the imposed boundary conditions on different time steps?
For the heat flux there are different values for inward heat flux and the normal total heat flux (extracted from Derived Values -> Surface Integration), for the same simulation. Can anyone explain the meaning of the two terminologies?
Kind regards, Ancuta Magurean
Hello Ancuta Magurean
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