Geothermal Power Generated from UK Granites (GWatt)

Lead Research Organisation: Heriot-Watt University
Department Name: Sch of Energy, Geosci, Infrast & Society

Abstract

Decarbonising power generation is a challenge for the UK, requiring an 80% reduction in greenhouse gas emissions by 2050, relative to 1990 levels. Carbon-free, renewable sources are attractive, but wind and solar generation are intermittent. In contrast, geothermally generated electricity is available all the time (i.e. is 'base load'). In the UK this can be developed with Engineered Geothermal Systems (EGS) whereby very hot water is accessed from depth via deep boreholes (4km or more) and is used to drive a turbine. Pioneering research has shown that permeable rocks (those through which fluid can flow) at depth are often associated with natural fracture systems. However, exploitation of the UK underground thermal resource has been held back by; 1) knowledge gaps about permeability and fluid/heat flow within the fractured hot rocks, and 2) a perception that the uncertainty associated with drilling problems or limited fluid flow from deep boreholes are too high for the potential financial reward. This project, Geothermal PoWer GenerATed from UK GraniTes (GWatt), seeks to address these barriers to uptake of EGS by:
- Increasing knowledge of the geological conditions needed for deep fracture-controlled fluid flow within granitic rocks.
- Developing a quantitative understanding of the heat resource and sustainability of the geothermal reservoir.
- Constructing robust geological risk assessments based on well-established oil & gas uncertainty quantification and optimisation methods, with a view to reducing perceived risks.
- Applying the integrated results of site-specific research to new geothermal exploration models for other granites, particularly those in SW England.

A particular strength of GWatt is the link with the developing United Downs Deep Geothermal Power (UDDGP) project, an £18M, 2 borehole EGS in the Carnmenellis granite in Cornwall. This will provide a unique resource; downhole fluids, rock samples, geophysical logs, flow data and seismic data. GWatt will maximise the scientific potential from these data, and carry out innovative further analyses and interpretation, combining site-specific observations with regional studies and state-of-the-art uncertainty quantification, to address the challenges associated with EGS development within SW England. Other UK crystalline basement rocks show fracture-controlled groundwater flow, so the lessons learned from GWatt will ultimately benefit understanding of the rest of the UK deep subsurface.

The project consortium comprises research, business and local government partners. The British Geological Survey, the University of Exeter Camborne School of Mines and Heriot Watt University provide complimentary skills in deep geothermal resource assessments, deep fracture fluid flow, rock/fluid interactions, reservoir modelling, detailed knowledge of the geology of SW England and the quantification of geological uncertainties. Geothermal Engineering Ltd. and Geoscience Ltd. are developing the UDDGP project and provide a wealth of experience delivering UK geothermal projects. Computer Modelling Group Ltd. will provide advanced heat and fluid flow modelling software. The Cornwall and Isles of Scilly Local Enterprise Partnership and Cornwall Council will facilitate outreach and dissemination activities, both to local people and the business community.

Beneficiaries include local communities through the creation of EGS combined heat and power plants that will be important hubs for renewable energy networks, supplying carbon-free heat and power. The heat can be used for space heating, industrial drying, balneology, greenhouse heating, fish farms etc., all of which will generate local jobs. Local industry will also benefit from the regional scale uptake of EGS within SW England and a potential revival of the minerals industry arising from technological solutions to extracting metals from the deep geothermal brines.

Planned Impact

In order to meet statuary greenhouse gas emission reduction targets, UK electrical power generation must be decarbonised. Carbon-free renewable generation is currently dominated by wind and solar, but these two technologies produce intermittent supply. Geothermal power generation, via engineered geothermal system (EGS) technology, produces a continuous base-load of carbon-free supply that meets the energy trilemma of security, affordability and sustainability. The beneficiaries of the proposed EGS research include:

1) Local communities, regional and national governments: A fully developed 2 borehole EGS system loop could generate up to 10 MWe as well as tens of MWth of heat. Through directional drilling technology, several EGS loops could feed a single Combined Heat and Power (CHP) plant. These CHP plants would be important hubs of renewable energy networks, supplying carbon-free heat and power to local communities and playing an important role in meeting regional and national renewable energy targets. The heat can be used for space heating, industrial drying, balneology, greenhouse heating, fish farms etc., all of which will generate local jobs. The Cornwall & Isles of Scilly Local Enterprise Partnership (CIoS LEP) estimate that a 100 MWe of installed geothermal power could provide electricity to c. 150,000 Cornish homes. Based on a study by the Geothermal Energy Association, 100 MWe will involve 1,400-1,700 high quality, long-term FTE jobs. GWatt will help early development of this industry, and thus help job creation, through direct employment and indirectly through 'spin off' industries.

2) The geothermal industry: The basic concepts of EGS (including older descriptors; HDR - Hot Dry Rock, and HWR - Hot Wet Rock) have been proposed for over 40 years. Take-up of the technology by industry requires an increased understanding of heat exchange / transport at depth, both facilitated by GWatt research. Extrapolation of the research findings from site- to regional-scale will enable the creation of more EGS operations. This is especially promising for granites in SW England, as they have a common geological source and bear many similarities to each other. An increased understanding of the regional fracture networks and deep fluid flow within them will enable the location of EGS systems to be more widespread and nearer locations of heat demand, substantially increasing the revenue of a CHP plant.

3) Financiers, investment trusts and venture capitalists: One of the identified barriers to EGS development has been the problem of raising finance to drill deep boreholes; the risk is often perceived as being too high. By quantifying EGS uncertainty using analysis techniques from the hydrocarbons industry, the research findings of GWatt will determine risk in a robust form and one that energy financiers are well versed in. This could potentially unlock the financial reserves to overcome this significant barrier.

4) The minerals industry: Identifying the scientific and technological solutions to extracting metals from deep brines can create another revenue stream for EGS and so help its economics, and it will reinvigorate the mineral extraction industry in SW England without the need for large mining operations. The hot geothermal brines carry a certain amount of dissolved metals, especially given the highly mineralised nature of the rocks in SW England. Modern electrochemical extraction technologies can be fitted to surface plant to capture these metals (e.g. strategically important metals to new technologies such as lithium, but also more traditionally important metals such as copper) as the hot brine is recirculated through the EGS flow loop. GWatt will quantify metal concentrations in solution, which when combined with fluid flow data, will provide constraints on amounts of metals than can be recovered.
 
Description 2021 update: The past 12 months have been difficult, with the impact of Covid-19 and 3 periods of lockdown, plus very bad weather limiting costal work during the late winter/spring of 2019/20. This has resulted in fewer observations of field exposures (analogue systems for deep underground), and a year delay to site operations (plus knock-on effects on the lab experimental programme). As a consequence of the above however, some opportunities opened up. One project partner mitigated Covid impacts to some extent through extended use of remote sensing data and literature reviews - resulting in 2 papers. Also, enforced lockdown and slow-down of test site activities enabled collection of microseismic data over a much longer period than originally anticipated (from 1 year to at least 2 years), which will be a fantastic scientific resource. Alongside the above, planned work did produce results approximately on schedule: we held a 'BowTie workshop' to help assess uncertainties; and analysis of borehole logging data has been completed, and is being used to create initial fracture models of the site.
2022 update: Covid-19 has impacted the project for the last 2 years, which has made progress difficult and added delays. Added to this has been very bad weather limiting costal work during the late winter/spring of 2019/20. This has resulted in fewer observations of field exposures (analogue systems for deep underground), and over 12 months of delay to site operations (plus knock-on effects on the lab experimental programme).
Not all has been negative however, and new opportunities have arrisen. One project partner mitigated Covid impacts to some extent through extended use of remote sensing data and literature reviews - resulting in 2 papers. Also, enforced lockdown and slow-down of test site activities enabled collection of microseismic data over a much longer period than originally anticipated (from 12 to 24 months - giving greater control on background levels) and which will ultimately be a fantastic scientific resource.
In terms of planned progress: a 'BowTie workshop' was held to to help assess uncertainties; analysis of borehole logging data has been completed and is being used to create initial fracture models of the site; 24-month deployment of surface microseismic stations; assistance with geochemical sampling when the United Downs number 1 borehole was put on first flow test; and predictive modelling of the flow of water and heat including building on structural models from elsewhere in the project.
Going forward, we aim to complete the more delayed parts of the project (e.g. lab experiments), further integrate the results of the different parts of the project to provide a fuller understanding of geothermal processes in the granites of SW England, and produce additional outputs and achieve further outreach of project findings.
Exploitation Route Several datasets (once completed) that will be lodged with the National Geosciences Data Centre will have long-term use for academic (and industry) study: 1) microseismic data of the response of the geothermal reservoir, 2) logging data and fracture interpretation of the UK's deepest onshore borehole, 3) geochemical data from production tests from the UK's deepest and hottest onshore borehole.
Sectors Energy,Environment

 
Description The first year of this project has seen the formulation of the research team, and the development of linkages between academic and 'industrial' partners. Whilst this process takes time, it is important in terms of data flow and working relationships - both of which are developing well. Field observations and sampling are ongoing, as is the collection of baseline microseismic data. Preparation of collected solid samples is ongoing, though collection of analytical data is still at an early stage. Development of methodologies for sampling of fluids, together with preparation of the necessary equipment, are ongoing for borehole testing scheduled for spring 2020. Where possible the project team have engaged in events aimed at raising the profile of the project - and as a consequence the broader objective of encouraging geothermal development in the UK in order to address social and economic needs. 2021 update: The past 12 months have been difficult, with the impact of Covid-19 and 3 periods of lockdown, plus very bad weather limiting costal work during the late winter/spring of 2019/20. This has resulted in fewer observations of field exposures (analogue systems for deep underground), a year delay to site operations (plus knock-on effects on the lab experimental programme), and furlough of one PDRA (and delays as a result). One project partner mitigated the impact of these to some extent through extended use of remote sensing data and literature reviews. Also, enforced lockdown and slow-down of test site activities did enable collection of microseismic data over a much longer period than originally anticipated (from 1 year to at least 2 years) which will give a better dataset. But in spite of the above delays, research paper are being submitted, and the project is still going to produce excellent outputs towards achieving the goals intended (albeit slower than originally anticipated). 2022 update: The past 12 months has again proved challenging, with the presence of Covid limiting what we have been able to do (either directly with reduced access to labs and the field, or indirectly as a consequence of supplier delays or industry partner delays). This has impacted the originally-planned programme, and we have had to adopt a more flexible 'do what we can' approach. The impact of the above has, however, not been uniform across the project, which has led to variable progress: For example: lab geochemistry experiments have been very delayed and field sampling much curtailed; Modelling work and interpretation of remote sensing data has continued more or less on track; and microseismic monitoring stations have gained additional data because they were left on site for about twice as long as originally anticipated. Due to the delays, a 12-month no-cost extension request was submitted - and approved. Some written outputs have been published, and others are in progress, but we acknowledge we are behind where hoped to be in our original (pre-Covid) plan. We tried to mitigate such delays and improve within-project communication by holding monthly Zoom meetings rather than the originally-anticipated 6-monthly 'in-person' meetings, and these have worked very well. Some key positive steps forward over the past 12 months: - GWatt researchers bringing together structural information at both borehole-scale and regional scales (=> 2, or possibly 3 papers). - Increasing return to 'normality', and return of access to labs and field visits as Covid restrictions eased. Also restarting of 'in-person' conferences, and greater ability to spread GWatt outputs. - Working with industry during flow testing of the GEL-owned UD-1 borehole, and collection/preservation/analyses of a number of samples. These are the deepest and hottest onshore groundwater samples ever produced in the UK and so are both noteworthy and unique. - Recovery of 10 surface microseismic stations from around United Downs after 24 months of monitoring. This was double the duration anticipated pre-Covid, but has resulted in a very large dataset which will be a valuable resource for both GWatt and later projects. - Young researchers transitioning out of GWatt and into new jobs, taking the skills learned ultimately to support science and industry in the UK.
First Year Of Impact 2022
Sector Electronics,Energy,Environment
Impact Types Societal,Economic

 
Title Bowtie risk assessment scheme 
Description We developed a concept for botue risk assessment that is relevant and specific for the United Downs geothermal project 
Type Of Material Data analysis technique 
Year Produced 2021 
Provided To Others? No  
Impact The bowtie risk assessment captures the potential threats of deep geothermal and provides barriers to mitigate these threats. Threats could be loss of injectivity, induced seismicity etc. This might help future and similar projects to mitigate risks. 
 
Description Experimental work at the British Geological Survey 
Organisation British Geological Survey
Country United Kingdom 
Sector Academic/University 
PI Contribution PDRA Nathaniel Forbes Inskip has performed experiments part of the GWatt project at BGS Keyworth.
Collaborator Contribution BGS Keyworth has contributed the experimental facilities and expertise.
Impact None yet, at least one paper expected.
Start Year 2021
 
Description Experimental work at the University of Liverpool 
Organisation University of Liverpool
Country United Kingdom 
Sector Academic/University 
PI Contribution PhD student Nick Harpers has performed experimental work (friction experiments) at the University of Liverpool. These experiments contribute to the GWatt objectives.
Collaborator Contribution The University of Liverpool provided the experimental facilities and expertise.
Impact None yet. At least one paper expected.
Start Year 2021