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Table 2 Value ranges and statistical distributions of the input parameters for the sensitivity analysis

From: Global sensitivity analysis and uncertainty quantification for design parameters of shallow geothermal systems

Parameter

Unit

Value range

Distribution

Min

Reference

Max

Measurements

 \(L_{BHE}\)

m

70

100

150

Normal

 \(d_{BHE}\)

m

0.12

0.152

0.2

Normal

 \(d_{po}\)

m

0.025

0.032

0.04

Normal

Pipe material

 \(\lambda _{p}\)

\({{\textrm{W}}\,{\textrm{m}}^{-1}\,{\textrm{K}}^{-1}}\)

0.4

0.4

2

Normal

Refrigerant

 \(\rho _{rf}\)

\({{\mathrm{kg\,m}}^{-3}}\)

960

1052

1195

Normal

 \(c_{rf}\)

\({{\mathrm{J \, kg}}^{-1} \,{\textrm{K}}^{-1}}\)

3050

3795

4250

Normal

 \(\lambda _{rf}\)

\({{\textrm{W}}\,{\textrm{m}}^{-1}\,{\textrm{K}}^{-1}}\)

0.44

0.48

0.57

Normal

 \(\mu _{rf}\)

\({{\textrm{kg}}\,{\textrm{m}}^{-1}\,{\textrm{s}}^{-1}}\)

0.0016

0.0052

0.0108

Normal

Grout

 \(\lambda _{gr}\)

\({{\textrm{W}}\,{\textrm{m}}^{-1}\,{\textrm{K}}^{-1}}\)

0.6

2

4

Normal

 \(c_{vgr}\)

\({{\mathrm{kJ \, m}}^{-3} \, {\textrm{K}}^{-1}}\)

1610

1910

2210

Normal

Subsurface

 \(n_{Peff}\)

0

0.125

0.25

Uniform

 \(\lambda _{s}\)

\({{\textrm{W}}\,{\textrm{m}}^{-1}\,{\textrm{K}}^{-1}}\)

1

2.5

5

Normal

 \(c_{vs}\)

\({{\mathrm{kJ \, m}}^{-3} \, {\textrm{K}}^{-1}}\)

500

1700

3800

Normal

 \(t_{aqf}\)

–*

0

0.25

1

Uniform

 \(z_{aqf}\)

–*

0

0.25

1

Uniform

Initial and boundary conditions

 \({\dot{V}}_{rf}\)

\({{\textrm{m}}^3 \,{\textrm{s}}^{-1}}\)

\(2.39 \cdot 10^{-4}\)

\(7.4\cdot 10^{-4}\)

\(1.24\cdot 10^{-3}\)

Uniform

 Q

MWh

7.2

18

28.8

Normal

 \(v_f\)

\({{\mathrm{m \, s}}^{-1}}\)

0

\(4.75 \cdot 10^{-7}\)

\(3\cdot 10^{-5}\)

Normal

 \(\Delta T_{geo}\)

\({{\mathrm{K \, m}}^{-1}}\)

0

0.032

0.045

Normal

 \(T_{geo}\) **

K

− 4.64

0

4.44

Normal

  1. *Relative value related to the length of the BHE reduced by 15 m \({L_{BHE}}^*\)
  2. **Parameter refers to the change of the curve shown in Fig. 17 as well as the temperature profile of the initial condition for subsurface temperature