- This model is a simple model for undisturbed ground temperature
- It is used with district heating grids or LTN in order to model
thermal pipe losses
Main equations
Tground
=Tmean*Tamp*exp(-D*√(π/(365*α)))
*cos((2π/365)(t-tshift-(D/2)*√(365/(π*α))))
Assumption and limitations
The model does not model the influence of the pipe temperature loss
on the ground temperature. The ground temperature is only dependent
on the set parameters.
Typical use and important parameters
The model is used as a boundary condition for the thermal losses in
district heating pipes.
Differently then stated in the parameter description below
tshift needs to be declared in days and α needs to me
declared in m2/day! (The Modelica SI unit diffusivity does not
support m2/day as a display unit.)
A typical value for α is bewteen 0.03 and 0.05 m2/day.
Options
No options.
Validation
The validation was done by comparing simulation results (San
Francisco example) with the findings of the first given reference
below (Florides and Kalogirou,2005).
The
Potsdam Institute for Climate Impact Research provides
measurement data for a German site, which can be used for comparison.
Implementation
The model implements the equation given above and supplies the
undisturbed ground temperature via a heat port.
References
- Florides and Kalogirou, 2005, Annual ground temperature
measurements at various depths. In: 8th REHVA World Congress, Clima,
Lausanne, Switzerland Citeseer, 2005
- T. Kusuda, P. R. Achenbach, Earth temperature and thermal
diffusivity at selected stations in the united states, Tech. rep.,
DTIC Document (1965)
- Bünning F., 2017, Simulation-based investigation of bidirectional
low temperature district heating and cooling networks and their
control, Master thesis
- April 30, 2018, by Marcus Fuchs:
Update documentation (see issue 561).
-
May 2017, by Felix Buenning: Updated information window
according to documentation standards
-
October 2016, by Felix Buenning: Developed and implemented
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