Enhanced rock weathering: Potential UK greenhouse gas removal

16 Aug 2024 12:14 PM

This POSTnote outlines the benefits and challenges of using enhanced rock weathering as a GGR approach for addressing emissions from UK hard-to-abate sectors.

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DOI: https://doi.org/10.58248/PN726 

The UK has committed to reaching Net Zero greenhouse gas (GHG) emissions by 2050. While emissions will be mitigated where possible, the Intergovernmental Panel on Climate Change (IPCC) stated that Greenhouse Gas Removal (GGR) is required to remove final emissions from hard–to–abate sectors. GGR involves removing GHGs, such as CO2, directly from the atmosphere, as opposed to capture from industrial sources.

Rock weathering is a natural process that removes carbon dioxide from the atmosphere, at a rate of ~1100 Mt CO2/year. Enhanced rock weathering (ERW aims) to accelerate this process in order to help address climate change. Fine rock particles are created, increasing the reactive surface area of the rock. This is then spread over land. When the rainwater and rock dust react, the resulting chemical products are released into the soil. Over time, these dissolved products may be taken up by plants, remain in the soil, or be transported to a sink, such as the ocean. Here, the products may react to form a solid carbonate mineral over thousands of years, which is then stable in the ocean for 10,000 years.

Academic studies suggest that ERW has the potential to contribute 6-30 Mt CO2/year removal, and there are several ongoing UK field trials. Several uncertainties remain with ERW, including the rate of CO2 removal, timescales involved, and the efficiency of transport to the ocean, with the potential for some carbon to be re-released. For the highest scale up scenarios, there are challenges for scaling up rock extraction, crushing and transport and there would likely be adverse environmental impacts due to the extent of quarrying required, such as destruction of habitats, noise, water and air pollution. However, ERW has potential benefits for agricultural soils and may increase crop and forestry yields.

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Acknowledgements

POSTnotes are based on literature reviews and interviews with a range of stakeholders and are externally peer reviewed. POST would like to thank interviewees and peer reviewers for kindly giving up their time during the preparation of this briefing, including: 

Members of the POST Board*

Dr Grace Andrews, Hourglass Climate 

Dr Catherine Bayliss, Environment Agency* 

Professor David Beerling, University of Sheffield* 

Dr Rob Brown, Bangor University 

Dr Frances Buckingham, Department for Energy Security & Net Zero* 

Dr Anne Cotton, University of Manchester* 

Matthew Davis, Environment Agency 

Dr Christiana Dietzen, University of Copenhagen* 

Dr Jessica Elias, Natural England 

Luke Greicius, Evident Global 

Garrett Guard, Evident Global 

Dr Kirsty Harrington, Heriot-Watt University 

Victoria Harvey, BeZero Carbon 

Dr Scott Hawley, Department for Environment, Food & Rural Affairs* 

Professor Rachael James, University of Southampton 

Gregory Jones, Imperial College London* 

Professor Guy Kirk, Cranfield University 

Dr Christina Larkin, InPlanet 

Dr Jonathan Lindsell, Department for Energy Security & Net Zero* 

Dr Mohammad Madankan, Heriot-Watt University  

Dr Joseph Mankelow, British Geological Survey 

Professor David Manning, Newcastle University* 

Dr Jennifer Mills, Cascade Climate 

Charles Nicholls, The Carbon Community* 

Mark North, Mineral Products Association 

Professor Nick Pidgeon, Cardiff University 

Theo Platts-Dunn, Evident Global 

Professor Noah Planavsky, Yale University 

Dr Alan Radbourne, UKCEH* 

Professor Phil Renforth, Heriot-Watt 

Professor Minik Rosing, University of Copenhagen 

Mark Russell, Mineral Products Association 

Dr Kate Scott, Department for Energy Security & Net Zero* 

Dr Jonathan Scurlock, National Famers’ Union* 

Dr Mark Workman, Imperial College London 

Dr Julia Woitischek, BeZero Carbon*

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