Articles | Volume 23, issue 21
https://doi.org/10.5194/bg-23-7727-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-23-7727-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Enhanced weathering of glacial rock flour drives coupled inorganic and organic carbon sequestration in a five-year field experiment
Christiana Dietzen
CORRESPONDING AUTHOR
Globe Institute, University of Copenhagen, 1350 Copenhagen, Denmark
Malgorzata Rizzi
Globe Institute, University of Copenhagen, 1350 Copenhagen, Denmark
Tim Jesper Suhrhoff
Yale Center for Natural Carbon Capture, Yale University, New Haven, CT, 06511, USA
Department of Earth & Planetary Sciences, Yale University, New Haven, CT, 06511, USA
Minik Thorleif Rosing
Globe Institute, University of Copenhagen, 1350 Copenhagen, Denmark
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Arthur Vienne, Patrick Frings, Jet Rijnders, Lucilla Boito, Jens Hartmann, Harun Niron, Reinaldy Poetra, Miguel Portillo Estrada, Tom Reershemius, Laura Steinwidder, Tim Jesper Suhrhoff, and Sara Vicca
SOIL, 12, 421–440, https://doi.org/10.5194/soil-12-421-2026, https://doi.org/10.5194/soil-12-421-2026, 2026
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Our study explores Enhanced Weathering (EW) using basalt rock dust to combat climate change. We treated maize-planted mesocosms with varying basalt amounts and monitored them for 101 d. Surprisingly, we found no significant realized inorganic CO2 removal. However, rock weathering was evident through increased exchangeable bases. While inorganic CO2 removal was not realized within this experiment, basalt amendment may enhance soil health and potentially long-term carbon sequestration.
Jelle Bijma, Mathilde Hagens, Jens S. Hammes, Noah Planavsky, Philip A. E. Pogge von Strandmann, Tom Reershemius, Christopher T. Reinhard, Phil Renforth, Tim J. Suhrhoff, Sara Vicca, Arthur Vienne, and Dieter Wolf-Gladrow
Biogeosciences, 23, 53–75, https://doi.org/10.5194/bg-23-53-2026, https://doi.org/10.5194/bg-23-53-2026, 2026
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Enhanced rock weathering is a nature based negative emission technology, that permanently stores CO2. It requires rock-flour to be added to arable land with the help of farmers. To be eligible for carbon credits calls for a simple but scientifically solid, so called, Monitoring, Reporting & Verification” (MRV). We demonstrate that the commonly used carbon-based accounting is ill-suited to close the balance in open systems such as arable land, and argue for cation-based accounting strategy.
Samuel Shou-En Tsao, Tim Jesper Surhoff, Giuseppe Amatulli, Maya Almaraz, Jonathan Gewirtzman, Beck Woollen, Eric W. Slessarev, James E. Saiers, Christopher T. Reinhard, Shuang Zhang, Noah J. Planavsky, and Peter A. Raymond
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-411, https://doi.org/10.5194/essd-2025-411, 2025
Revised manuscript accepted for ESSD
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We created the first detailed map of how much agricultural lime has been used across the United States from 1930 to 1987. Lime helps improve soil health and crop growth. Our study shows that how and where lime is used depends on climate, soil, and farming practices. By using machine learning, we found patterns that help explain these differences. This work helps us better understand the environmental role of lime and its impact on farming and climate.
Clara R. Vives, Jørgen Bendtsen, Rasmus D. Dahms, Niels Daugbjerg, Kristina V. Larsen, and Minik T. Rosing
The Cryosphere, 19, 3107–3121, https://doi.org/10.5194/tc-19-3107-2025, https://doi.org/10.5194/tc-19-3107-2025, 2025
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Glacial rock flour (GRF) from Greenlandic glaciers transports silicate and trace metals into fjords, influencing marine biogeochemistry. Trace metal concentrations are high in riverine and low-salinity waters but decrease sharply as salinity increases, challenging estimates based on freshwater input alone. Silicate rises due to GRF weathering but declines in fjords due to mixing. Uranium and molybdenum originate from the ocean, highlighting complex trace metal and nutrient dynamics.
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Editorial statement
Enhanced rock weathering (ERW) is an emerging climate change mitigation strategy. Quantifying the carbon dioxide removal associated with ERW is a major challenge in the field. This study presents results from a uniquely long-term (five-year) agricultural ERW field trial and provides direct field evidence that substantial silicate weathering and associated carbon dioxide removal can occur in temperate sandy soils, such as those found in Northern Europe. It combines this with an investigation of changes in soil organic carbon, another topic of great interest in the ERW community, to better understand carbon dynamics and sequestration potential in agricultural fields.
Enhanced rock weathering (ERW) is an emerging climate change mitigation strategy. Quantifying...
Short summary
Enhanced rock weathering involves spreading ground silicate rock on farmland to remove atmospheric CO₂ as the rock dissolves. Soil samples taken five years after Greenlandic glacial rock flour was applied to a Danish field showed that over half the applied material had dissolved, yet the increase in soil organic carbon was substantially greater than the estimated inorganic carbon uptake through weathering. This highlights the importance of considering both pathways when assessing climate impact.
Enhanced rock weathering involves spreading ground silicate rock on farmland to remove...
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