Science – Society – Technology
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 |