The term ‘geothermal energy’ refers to any heat derived from the ground, from depths of a few metres to multiple kilometres beneath the Earth’s surface.
Low-grade heat stored in the shallow subsurface (less than 200 m) is largely derived from solar radiation that is absorbed by the ground and distributed via natural groundwater systems and artificial structures such as flooded coal mines. The ground acts as a solar battery and, for this heat, utilisation usually requires a heat pump. This energy is widely described as ‘ground-source energy’ or ‘shallow geothermal energy’.
There is no strict definition for ‘deep geothermal energy’, but the UK Government has adopted the term to refer to heat resources derived from depths of >500 m. The heat of the Earth increases with depth, a phenomenon described as the geothermal gradient. This heat is partly the primordial heat from when the Earth was formed and partly heat generated from within the Earth’s crust from the decay of mildly radioactive elements. This upward heat flux varies across the globe, but in the UK is around 27°C/km (Busby, 2014). Assuming an average annual air temperature of 12°C, this means that subsurface temperatures at 1000 m, 3000 m and 5000 m are around 39°C, 89°C and 139°C, respectively.
Geothermal energy technologies
Ground source heating and cooling
Exploitation of this low-grade, ground-source heat resource requires use of ground-source heat pump (GSHP) systems (Figure 2). These extract heat from the ground either via ground heat exchangers (i.e. pipes installed in the ground through which a heat carrier fluid is circulated: ‘closed-loop’ systems) or from pumped groundwater stored in aquifers (‘open-loop’ systems) and mines. These systems utilise a heat pump to extract the low-grade heat from the fluid and upgrade it to more useful temperatures (>40°C) required for the heating of buildings. The cold carrier fluid/groundwater is then returned to the subsurface.
Ground-source heat pumps can be used for heating, cooling or both, i.e. heating during winter and cooling during summer.
The availability of different types of GSHP systems (closed-loop; open-loop; hybrid; mine water systems) and flexible design options mean that deployment of these systems is feasible almost anywhere in the UK.
Geothermal heat and power
Subsurface temperatures in the UK are around 39°C, 89°C and 139°C at 1000 m, 3000 m and 5000 m, respectively. While these temperatures (classed as low enthalpy) are below the economic threshold for conventional (steam turbine) power generation (which is >160°C), they are sufficiently high to provide heat for direct-use space heating as well as for a variety of heat-intensive industrial processes and agricultural applications.
In conventional hydrothermal systems (Figure 2), the heat is transported by natural groundwater, circulating within deep aquifers. It is exploited via a so-called ‘doublet system’ consisting of two deep boreholes drilled over a range of depths down to 5 km: one is for abstracting the hot water and the other is for re-injecting the cooled water back into the geothermal system. Various regions exist within the UK onshore where such hydrothermal systems could provide a geothermal resource. These often coincide with areas of high heat demand; for many areas of the UK it would be technically feasible to exploit geothermal resources for space heating using district energy schemes.
Medium-enthalpy geothermal potential exists in the UK in areas where geological anomalies, e.g. the presence of radiogenic granites, have resulted in increased heat flows, e.g. Cornwall; northern England; Scotland. Temperatures at economically drillable depths (around 5 km) are sufficiently high for power generation with binary-cycle power plants or for industrial and residential (direct-use) heating, but granites are not naturally porous — they typically have less than one per cent pore space — or water-bearing. The heat is abstracted by injecting water into the system and circulating it between two deep boreholes through existing or enhanced fluid pathways, creating what is known as an engineered geothermal system (EGS).
Geothermal research at the BGS
- Geothermal road map
- Geothermal potential of Carboniferous basins
- Subsurface urban heat sources
Science briefing papers
- Who owns geothermal heat? (November 2018)
- What lies beneath
- Shallow geothermal
Geothermal fact sheets
- Geothermal potential of the Carboniferous limestone
- Geothermal potential of the Coal Measures
Beamish, D, and Busby, J. 2016. The Cornubian geothermal province: heat production and flow in SW England: estimates from boreholes and airborne gamma-ray measurements. Geothermal Energy, Vol. 4(4), 25.
Busby, J. 2014. Geothermal energy in sedimentary basins in the UK. Hydrogeology Journal, Vol. 22(1), 129–141.
Busby, J, and Terrington, R. 2017. Assessment of the resource base for engineered geothermal systems in Great Britain. Geothermal Energy, Vol. 5(1), 18.
Busby, J, Lewis, M, Reeves, H, and Lawley, R. 2009. Initial geological considerations before installing ground source heat pump. Quarterly Journal of Engineering Geology and Hydrogeology, Vol. 42(3), 295–306.
- Carbonisation to decarbonisation and the role of geoscience by Mike Stephenson, 29 August 2019
- How to heat a city: a new 3D geological model by Laura James, 16 July 2019
- How to heat a city…and decarbonise it using heat pumps by David Boon and Gareth Farr, 18 February 2019
- Feeling the heat: exploring the potential for geothermal energy by Chris Rochelle, 5 December 2018
- Clean coal is a myth. Clean heat from coal mines isn’t by Corinna Abesser and Ashley Patton, 16 October 2018
- Do coal mines have an eco-friendly future? Guest blog by Prof John Underhill, 19 October 2018
- The BGS sets its eyes (and ears) on a clean energy future by David Schofield, 26 February 2018
- Abandoned mines provide low carbon heating by Gareth Farr, 20 May 2015
- Gas sampling near hell by Gemma Purser and Tom Barlow, 30 September 2015
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