.AixLib.BoundaryConditions.GroundTemperature.GroundTemperatureKusuda

Information

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

Revisions


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