Enhanced weathering with agriculture for atmospheric carbon dioxide removal

17 - 18 November 2025 09:00 - 17:00 The Royal Society Free Watch online
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Enhanced weathering header

Discussion meeting organised by Professor David Beerling FRS, Professor Rachael James, Professor Noah Planavsky and Dr Christopher Reinhard.

This meeting will discuss advances and uncertainties in terrestrial enhanced weathering, a key carbon dioxide removal strategy for climate change mitigation. Recent discoveries and R&D investment are accelerating the prospect of large-scale EW implementation, but uncertainties remain. The goal of this meeting is to provide a much-needed balanced discussion on the scientific and societal challenges ahead.

Programme

The programme, including speaker biographies and abstracts, will be available soon. Please note the programme may be subject to change.

Poster session

There will be a poster session from 17:00 on Monday 17 November 2025. If you would like to present a poster, please submit your proposed title, abstract (up to 200 words), author list, and the name of the proposed presenter and institution no later than 19 October 2025.

Attending the event

This event is intended for researchers in relevant fields.

  • Free to attend
  • Both virtual and in-person attendance is available. Advance registration is essential. Please register via Eventbrite for a ticket
  • Lunch is available on both days of the meeting for an optional £25 per day. There are plenty of places to eat nearby if you would prefer purchase food offsite. Participants are welcome to bring their own lunch to the meeting

Enquiries: Scientific Programmes team.

Image credit: ©️David Beerling

Organisers

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    Professor David Beerling, University of Sheffield, UK

    Professor David Beerling FRS is the Sorby Professor of Natural Sciences and Director of the Leverhulme Centre for Climate Change Mitigation, a newly established Research Centre funded by the Leverhulme Trust.

  • Professor Rachael James

    Professor Rachael James

    Rachael James is Professor of Geochemistry and Director of the NERC IGNITE Doctoral Landscape Award in the School of Ocean and Earth Science at the University of Southampton, UK. She is renowned for the development and application of novel chemical and isotopic techniques to improve understanding of ocean and earth processes and to address critical environmental and societal challenges. As part of the Leverhulme Centre for Climate Change Mitigation she leads the development of methodologies for removing CO2 from the atmosphere by enhanced rock weathering. Rachael serves on the scientific advisory councils of the GFZ Helmholtz Centre for Geosciences and the multi-institute research mission Marine Carbon Sinks in Decarbonisation Pathways and is a member of the awards committee of the European Association of Geochemistry (EAG). She was awarded a Philip Leverhulme Prize in 2006, an EAG Distinguished Lectureship in 2014 and was the Marie Tharp Lecturer in 2022.

  • Professor Noah Planavsky

    Professor Noah Planavsky

    Noah Planavsky is an Assistant Professor in the Department of Geology and Geophysics at Yale University. He studies the connections between the evolution of Earth-system processes, biological innovation, and ecosystem change—foremost in Earth’s early history. His research integrates field, petrographic, and geochemical work. A central theme of his research has been trying to piece together the history and effects of Earth’s oxygenation. He has also worked on reconstructing the evolution of atmospheric carbon dioxide levels through Earth’s history. Current projects include coupling paleoredox proxies, calibrating novel metal isotope systems in modern aqueous systems and disentangling the distribution and diagenetic history of traces metals in sedimentary rocks.

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    Dr Chris Reinhard

    Dr Chris Reinhard is an Associate Professor of Biogeochemistry and Georgia Power Chair in the School of Earth and Atmospheric Sciences at Georgia Tech, where his research focuses on greenhouse gas biogeochemistry, Earth system science, and carbon dioxide removal. Dr Reinhard was awarded the Alfred P. Sloan Fellowship in Ocean Sciences in 2015, a Sigma Xi Young Faculty Award in 2020, and the James B. Macelwane Medal from the American Geophysical Union in 2021. Much of his current work focuses on the mechanisms, monitoring, and verification of carbon removal technologies that manipulate Earth’s alkalinity cycle, in parallel with exploration of holistic incentives for responsible greenhouse gas mitigation and carbon management.

Schedule

Chair

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Professor David Beerling, University of Sheffield, UK

09:00-09:05 Welcome by the Royal Society and lead organiser
09:05-09:30 Talk title TBC
09:30-09:45 Discussion
09:45-10:15 Enhanced rock weathering drives soil carbon sequestration and nutrient cycling: Evidence from Chinese plantations and global meta-analysis

Enhanced rock weathering (ERW) is a promising carbon dioxide removal (CDR) strategy for soil carbon sequestration and climate mitigation. This study integrates a 2-year field monitoring in Chinese tropical rubber plantations and global meta-analysis to examine ERW via crushed rock amendments on soil carbon dynamics and ecosystem functions. Field study show ERW increased soil organic carbon (SOC) and mineral-associated organic carbon (MAOC) in tropical regions, elevated carbon-fixation genes while reducing carbon-degradation genes in soil microbes (enhancing SOC retention), and improved nitrogen cycling, root phosphorus acquisition, and ecosystem multifunctionality. Furthermore, a global meta-analysis of 74 studies indicates crushed rocks increased SOC (3.8%), MAOC (6.1%), and particulate organic carbon (7.5%) on average, with no impact on other fractions. SOC accrual was driven by exchangeable calcium, microbial biomass, and soil structure, co-controlled by local climate. Machine learning simulations of global croplands reveal strong site-dependency in ERW’s SOC effects: positive in low-latitude regions (40°N-40°S) but negative in high-latitude areas. Models also indicate an optimal ERW application range of 50-500 g m-1 for maximizing SOC sequestration, beyond which positive effects diminish and negative ones intensify. This empirical synthesis supports ERW, particularly with Ca-rich amendments, is an effective strategy for CDR by enhancing SOC stabilization and long-term CO2 sequestration via mineral-organic interactions and indirectly driving biological carbon sequestration process. Maximizing ERW’s positive CDR effects requires comprehensive consideration of site-specific climatic and soil characteristics, alongside appropriate application rates and durations.

Dr Tongtong Xu

Dr Tongtong Xu

Northwestern Polytechnical University, China

10:15-10:30 Discussion
10:30-11:00 Break
11:00-11:30 Enhanced rock weathering for improved farmer welfare in the Global South: An at-scale case study for rice agriculture in India

Mati Carbon uses basalt-based Enhanced Rock Weathering (ERW) to supplement the income of smallholder farmers while promoting climate resilience. In facilitating future participation in carbon markets for smallholder farmers, Mati provides opportunities for agronomic benefits for individual partnered farmers while paving the way towards economically viable, gigaton scale CDR in regions throughout the Global South.

Currently, Mati operates at scale at centralized locations within Chhattisgarh and Madhya Pradesh. For each deployment, Mati monitors the crop yield for all enrolled farmers. Many of our partnered farmers do not deploy basalt on all of their fields, which allows for comparison of the crop yield in deployed versus control plots.  Along with biomass measurements and crop density estimations, we conduct detailed farmer surveys to monitor the agricultural practices of each enrolled farmer and the performance of their crops after ERW deployment.

In 2024 Mati deployed 49,880 metric tons of basalt with 711 farmers and 7,898 metric tons with 293 farmers in 2023 in Chhattisgarh.  Here, we compare mean yield changes for rice production across the Kharif (summer monsoonal season).  We report significant mean production increases for rice yield.  Throughout the Chhattisgarh Kharif in 2023 the mean increase for rice productivity (kg/ac) was 14.39% (n=162).  In the 2024 Kharif, the mean increase in rice yield at Chhattisgarh was 27.79% (n=44).

Mr Shantanu Agarwal

Mr Shantanu Agarwal

Mati Carbon PBC, US

11:30-11:45 Discussion
11:45-12:15 Organic carbon cycle feedbacks determine the climate mitigation potential of enhanced rock weathering in a forestry context

Enhanced rock weathering (ERW) for climate change mitigation is usually considered in the context of croplands. Yet rock dust can also be deployed to intensively managed (i.e. planted) forests. These forests now occupy 300 million hectares and frequently have appropriate infrastructure for rock dust deployment; they also occur in climatic zones that are favourable for rock weathering. A key question is whether the presence of trees (as opposed to crops) accelerates the weathering process, and whether long-lived vegetation serves as a sink for weathering products. To address this knowledge gap, we conducted a large-scale (12 ha) ERW trial in a newly planted forest. The ERW treatment was crossed in a fully factorial design with the addition of a forest soil inoculum, intended to re-establish populations of beneficial microbes which were presumably lost during the site’s multi-century prior use as a sheep pasture. We found that although rock dissolution proceeded relatively rapidly, most of the weathering products were either sorbed to soil exchange sites or taken up by plants, resulting in a significant increase in carbon sequestration into wood. Application of rock dust also enhanced soil respiration; as a result, more soil carbon was released to the atmosphere than was captured via weathering. Unexpectedly, introducing forest soil microbes to the site significantly slowed rock dissolution. Thus, plant and microbial responses determined both the sign and magnitude of weathering-related carbon dioxide fluxes five years after the first rock dust application.

Dr Bonnie Waring

Dr Bonnie Waring

Imperial College London, UK

12:15-12:30 Discussion

Chair

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Dr Chris Reinhard

Georgia Institute of Technology, US

13:30-14:00 EW and Brazilian agriculture

Terradot is leading science-based farm trials to evaluate the agronomic benefits of basalt rock dust application across diverse farming systems in Brazil. This work supports the scaling of Enhanced Rock Weathering (ERW) as a carbon dioxide removal (CDR) strategy, while also delivering improvements in soil health and crop yields for farmers. Brazil’s diverse climates, soil types, and cropping systems provide an ideal environment for assessing the potential of basalt to enhance soil fertility and agricultural productivity.

Field trials are being conducted across multiple partner farms to evaluate the effects of basalt on key agronomic indicators, including soil pH, base saturation, nutrient availability, and crop yield. These trials span a variety of environmental conditions and were designed to generate field-specific insights into how local factors—such as precipitation, elevation, and soil texture—influence basalt dissolution and its agronomic performance. Particular attention is being given to the spatial and temporal variability of soil indicators across different soil textures.

Preliminary data from selected farms will be presented, including comparisons between basalt-treated and untreated control fields. While detailed results are still being collected and analysed, the presentation will highlight emerging trends and outline the methodological framework used to assess agronomic outcomes and co-benefits.

This work contributes to the expanding body of evidence supporting ERW’s dual role in carbon removal and agricultural enhancement, and lays the foundation for scaling rock dust applications tailored to the Brazilian agricultural landscape.

Dr Jonathan Ojeda

Dr Jonathan Ojeda

Terradot, Argentina

14:00-14:15 Discussion
14:15-14:45 River catchments as natural monitors of Enhanced Weathering: evidence from the Mississippi River

Accurately quantifying carbon dioxide removal (CDR) is critical for scaling enhanced weathering (EW) as a climate solution. River catchments serve as natural integrators for monitoring EW impacts at scale, capturing both spatially distributed application and downstream transport of weathering products. Using a large USGS dataset of US river chemistry, we simulate the silicate rock applications rates needed to observe a two SD signal above baseline. We find that EW signals are more likely to emerge in larger catchments with a high proportion of agricultural area, demonstrating the potential of this approach to monitor CDR from EW at scale.

We use carbonate addition to the Mississippi River Basin—one of the largest agricultural catchments globally—as a case study and historical analog for EW. Compiling over a century of agricultural, chemical, and hydrological data, we show that ~75% of lime added to soils has been exported as alkalinity, indicating that liming has acted as a net CO₂ sink. This challenges current greenhouse gas accounting frameworks, such as those of the IPCC, which treat liming as a CO₂ source and rather suggests that carbonate-rock-based EW can be an efficient path to achieving CDR. Attributing emissions to acidity addition instead enables a more geochemically accurate and policy-relevant understanding of CO2 emissions. Moreover, we find that acid-base reactions in soils may contribute more to agricultural CO2 emissions than currently recognized. These findings highlight the utility of riverine fluxes as a robust, scalable proxy for EW-based CDR and call for a revision of agricultural carbon accounting protocols.

Dr Tim Jesper Suhrhoff

Dr Tim Jesper Suhrhoff

Yale Center for Natural Carbon Capture, US

14:45-15:00 Discussion
15:00-15:30 Break
15:30-16:00 Towards net-zero chocolate: Enhanced weathering in tropical cocoa agri- ecosystems

Theobroma cacao, “Food of the God’s” has profound social and economic status as a food, drink and medicine for 5,300 years (Zarrillo et al., 2018). Cacao is typically grown on highly weathered, nutrient-poor, acidic soils (oxisols). These soils are infertile because of low pH, calcium (Ca), magnesium (Mg), and potassium (K) levels but high aluminium (Al) content. The warm climate conditions of Brazilian soils are ideal for carbon dioxide removal by EW and generating agricultural and soil co-benefits. 

A field trial spanning three years has been designed to evaluate EW deployment on cacao under field conditions. Within Brazil, specifically Bahia, cacao is often grown using the traditional Cabruca system. This system has cultural and environmental significance, often cited for its preservation of endemic trees (Cassano et al., 2008). This field trial will investigate EW on both traditional and modern agroforestry systems to determine potential synergies and additive effects. Carbon removal rates (CDR), soil fertility and agronomic co-benefits have been assessed.

Here, we present the outcome of this trial after one year of EW (basalt) application and a parallel trial assessing the potential for a novel iron chelating biotechnology to accelerate EW and CDR rates in a field setting.

Miss Issi Steeley

Miss Issi Steeley

Leverhulme Centre for Climate Change Mitigation, UK

16:00-16:15 Discussion
16:15-16:45 Effects of enhanced weathering on fundamental soil properties

Enhanced weathering (EW) is an intuitively attractive carbon dioxide removal strategy that involves the application of highly weatherable silicate rock powder (usually basalt) to soils to accelerate natural chemical weathering. While primarily developed for its potential in mitigating climate change by capturing atmospheric CO2, EW also has the potential to fundamentally alter soil biogeochemistry and pedogenesis. In this talk, we outline mechanisms through which EW may impact soil properties and functions. Using recent results from an EW field trial initiated in 2020 in vineyard of western Switzerland, we explore the effect of a single twenty ton per hectare basalt powder application on soil physical, mineralogical, chemical, and biological properties. Findings show that the basalt application stimulated soil biological activity and led to the formation of poorly crystalline secondary aluminosilicates and oxides. Altogether, these results indicate that soil-forming processes are significantly modified by the basalt powder addition. While the increase in biogeochemical reactivity of basalt-amended soils could be beneficial in many cases, many unknowns remain regarding the long-term sustainability of the practice. Overall, the integration of EW into sustainable agricultural practices may present a promising avenue for improving soil fertility in some agroecosystems, but could also pose significant risks for some soils and climate zones. Investment in long-term field studies is necessary to provide a full understanding of environmental consequences of EW and optimize implementation strategies.

Dr Stephanie Grand

Dr Stephanie Grand

University of Lausanne, Switzerland

16:45-17:00 Discussion
17:00-18:15 Poster session

Chair

Professor Rachael James

Professor Rachael James

University of Southampton, UK

09:00-09:30 Role of models in tracking carbon removal by EW
Dr Chris Reinhard

Dr Chris Reinhard

Georgia Institute of Technology, US

09:30-09:45 Discussion
09:45-10:15 Rivers, EW and C-cycling
Dr Pete Raymond

Dr Pete Raymond

Yale University, US

10:15-10:30 Discussion
10:30-11:00 Break
11:00-11:30 EW soil processes
Professor Isabel Montanez NAS

Professor Isabel Montanez NAS

University of California, Davis, US

11:30-11:45 Discussion
11:45-12:15 Atmospheric carbon dioxide removal via mineral-based ocean alkalinization

Conventional mitigation measures alone will be insufficient to limit global warming below 2°C, necessitating gigaton-scale atmospheric carbon dioxide removal (CDR). Oceans play a critical role in the global carbon cycle, absorbing 25 to 30% of anthropogenic CO2 emissions. The chemical weathering of carbonate and silicate rocks significantly contributes to atmospheric CO2 drawdown over geological time scales. Mineral-based ocean alkalinity enhancement (OAE) is a CDR technique that seeks to accelerate this natural process by distributing finely ground reactive minerals (e.g. olivine, lime) into suitable coastal and shelf environments. Laboratory experiments have demonstrated the potential of some silicate minerals, such as basalt and olivine, to be used as source material. In a similar fashion, some waste streams of the current mining industry have been examined for their potential. It remains to be tested, however, whether the dissolution rates obtained in these controlled experiments can be translated to the real world. In recent years, a number of dedicated mesocosm experiments and restricted field trials have been conducted to assess the sequestration potential and technology feasibility of mineral-based ocean alkalinity enhancement under more realistic, natural conditions. This presentation will provide an overview of the current state of knowledge.

Professor Filip Meysman

Professor Filip Meysman

University of Antwerp, Belgium

12:15-12:30 Discussion

Chair

Professor Noah Planavsky

Professor Noah Planavsky

Yale University, US

13:30-14:00 Public acceptability of enhanced weathering in the global north and global south

In order to conduct responsible research and innovation well-engaged and informed communities must be embedded within the research process contributing to the decisions made about carbon dioxide removal approaches to tackle climate change. Using mixed methods we extensively explored how publics perceive enhanced weathering in the UK, US, Australia and Malaysia including nationally representative surveys (UK, US and Australia) alongside deliberative workshops in the UK, US and Malaysia. Findings illustrated that enhanced weathering was an unfamiliar strategy and produced a range of common concerns in all participants. Some of the environmental and social impacts included those on the marine environment, human health, and concerns regarding mining (particularly within Malaysia). The dependency of smallholders’ livelihoods on agriculture also resulted in questions about long-term impacts on crops and soils. In the Malaysian groups the economy was a prevalent topic, especially for more rural participants, with interest in how the strategy could be financially beneficial to smallholders including possible co-benefits on their crops. Overall our research shows participatory processes can and should be used to ensure socially responsible upscaling of enhanced weathering with our participants producing meaningful insights and directions for future research. However public acceptance will be dependent on meaningful deep emissions reductions being made, having suitable governance in place and serious consideration of appropriate economic and social costs if enhanced weathering is to be utilised.

Dr Elspeth Spence

Dr Elspeth Spence

Cardiff University, UK

14:00-14:15 Discussion
14:15-14:45 A Taxonomy of Enhanced Weathering Policy Opportunities

There is scientific consensus that, in addition to mitigation of ongoing emissions,  gigatons of carbon dioxide must be removed from the atmosphere to remain in alignment with the goals of the Paris Agreement. Scaling carbon removal (CDR) will require concerted efforts across national governments, sub-national governments, and supra-national institutions. Here we present an overview of the current state of CDR policy development and discuss possible future directions, with an emphasis on terrestrial enhanced weathering. First, we discuss current policy advocacy efforts, which focus on innovation (funding for research and development to bring technology to market) and market creation (voluntary certification schemes and integration in compliance markets). We note that the current approach assumes carbon credit trading as the dominant paradigm for scaling CDR and EW. Next, we propose a complementary approach to identify novel policy support mechanisms for enhanced weathering that (1) focus on co-benefits and (2) leverage existing regulatory and subsidy schemes.  As an illustrative example, we describe how agricultural liming subsidies are structured in different jurisdictions and how these distinct policy mechanisms could support enhanced weathering. Lastly, we discuss how contextualized monitoring, reporting, and verification (MRV) for enhanced weathering under different policy scenarios can support integration of large-scale open system CDR into national GHG inventories and nationally determined contributions (NDCs) under the Paris Agreement.

Ms Anu Khan

Ms Anu Khan

Carbon Removal Standards Initiative, US

14:45-15:00 Discussion
15:00-15:30 Break
15:30-16:00 Panel discussion I: Engaging local communities
Professor Karen Henwood

Professor Karen Henwood

Cardiff University, UK

Dr Livia Fritz

Dr Livia Fritz

Aarhus University, Denmark

Professor Nick Pidgeon

Professor Nick Pidgeon

Cardiff University, UK

Professor Susan Owens OBE FBA

Professor Susan Owens OBE FBA

University of Cambridge, UK

16:00-16:15 Discussion
16:15-17:00 Panel discussion II: EW-MRV: future opportunities
Professor Rachael James

Professor Rachael James

University of Southampton, UK

Dr Matthew Clarkson

Dr Matthew Clarkson

InPlanet GmbH, UK

Dr Zeke Hausfather

Dr Zeke Hausfather

Stripe, Inc., US

Professor Noah Planavsky

Professor Noah Planavsky

Yale University, US