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Table 1 Summary of the physical properties adopted in the sediment–basement model

From: Assessment of the resource base for engineered geothermal systems in Great Britain

 

Min

Max

Mean

Sediment thermal conductivity (W m−1 K−1)

 Palaeogene–Permian

2.04

3.22

2.37

 Carboniferous–Devonian

2.25

2.98

2.68

Sediment heat production (μ Wm−3)

0.45

1.86

1.17

Basement thermal conductivity (W m−1 K−1)

 Non-granitic

2.03

4.43

3.06

 Granitic

2.88

3.65

3.3

Basement heat production (μ Wm−3)

 Non-granitic

0.3

3.0

1.46

 Granitic

  

5 km depth

10 km depth

  Southwest England

  

4.6

4.6

  Northern England

  

3.06

2.46

  Southern Uplands

  

1.87

1.5

  East Grampians

  

2.98

1.9

  Other Scottish

  

1.34

1.08

Basement density (kg m−3)

2270

3270

2800

Basement specific heat (J kg−1 K−1)

540

1347

887

  1. The methodology for the adoption of these properties across the grids of the model are described in the text. It should be noted that the thermal conductivities in the table are at laboratory temperatures and are corrected for temperatures at depth when attributed to the model