Buildings.Fluid.HeatExchangers.Boreholes

Package with borehole heat exchangers

Information

Extends from Modelica.Icons.VariantsPackage (Icon for package containing variants).

Package Content

Name	Description
UTube	Single U-tube borehole heat exchanger
Examples	Example files for borehole heat exchanger
BaseClasses	Base classes for Borehole

Buildings.Fluid.HeatExchangers.Boreholes.UTube

Single U-tube borehole heat exchanger

Information

Model of a single U-tube borehole heat exchanger. The borehole heat exchanger is vertically discretized into n_seg elements of height h=h_Bor⁄n_seg. Each segment contains a model for the heat transfer in the borehole, for heat transfer in the soil and for the far-field boundary condition.

The heat transfer in the borehole is computed using a convective heat transfer coefficient that depends on the fluid velocity, a heat resistance between the two pipes, and a heat resistance between the pipes and the circumference of the borehole. The heat capacity of the fluid, and the heat capacity of the grout, is taken into account. The thermal resistance and capacity network inside the borehole is computed according to Bauer et al., (2011).

The heat transfer in the soil is computed using transient heat conduction in cylindrical coordinates for the spatial domain r_bor ≤ r ≤ r_ext. In the radial direction, the spatial domain is discretized into n_hor segments with uniform material properties. Thermal properties can be specified separately for each horizontal layer. The vertical heat flow is assumed to be zero, and there is assumed to be no ground water flow.

The far-field temperature, i.e., the temperature at the radius r_ext, is computed using a power-series solution to a line-source heat transfer problem. This temperature boundary condition is updated every t_sample seconds.

The initial far-field temperature T_ext,start, which is the temperature of the soil at a radius r_ext, is computed as a function of the depth z > 0. For a depth between 0 ≤ z ≤ z₀, the temperature is set to T_ext,0,start. The value of z₀ is a parameter with a default of 10 meters. However, there is large variability in the depth where the undisturbed soil temperature starts. For a depth of z₀ ≤ z ≤ h_bor, the temperature is computed as

Tⁱ_ext,start = T_ext,0,start + (zⁱ - z₀) dT ⁄ dz

with i ∈ {1, ..., n_ver}, where the temperature gradient dT ⁄ dz ≥ 0 is a parameter. As with z₀, there is large variability in dT ⁄ dz ≥ 0. The default value is set to 1 Kelvin per 100 meters. For the temperature of the grout, the same equations are applied, with T_ext,0,start replaced with T_fil,0,start, and Tⁱ_ext,start replaced with Tⁱ_fil,start. The default setting uses the same temperature for the soil and the filling material.

Implementation

Each horizontal layer is modeled using an instance of Buildings.HeatExchangers.Fluid.Boreholes.BaseClasses.BoreholeSegment. This model is composed of the model Buildings.Fluid.HeatExchangers.Boreholes.BaseClasses.HexInternalElement which computes the heat transfer in the pipes and the borehole filling, of the model Buildings.HeatTransfer.Conduction.SingleLayerCylinder which computes the heat transfer in the soil, and of the model Buildings.Fluid.HeatExchangers.Boreholes.BaseClasses.TemperatureBoundaryCondition which computes the far-field temperature boundary condition. The thermal resistor and capacitor network is computed in Buildings.Fluid.HeatExchangers.Boreholes.BaseClasses.singleUTubeResistances.

References

D. Bauer, W. Heidemann, H. Müller-Steinhagen, and H.-J. G. Diersch. Thermal resistance and capacity models for borehole heat exchangers . International Journal Of Energy Research, 35:312–320, 2011.

Extends from Buildings.Fluid.Interfaces.PartialTwoPortInterface (Partial model transporting fluid between two ports without storing mass or energy), Buildings.Fluid.Interfaces.TwoPortFlowResistanceParameters (Parameters for flow resistance for models with two ports), Buildings.Fluid.Interfaces.LumpedVolumeDeclarations (Declarations for lumped volumes).

Parameters

Connectors

Modelica definition