Articles | Volume 12, issue 1
https://doi.org/10.5194/soil-12-421-2026
© 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/soil-12-421-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Weathering without realizing inorganic CO2 removal revealed through base cation monitoring
Arthur Vienne
CORRESPONDING AUTHOR
Biobased Sustainability Engineering (SUSTAIN), Department of Bioscience Engineering, University of Antwerp, Antwerp, Belgium
Patrick Frings
GFZ German Research Centre for Geosciences, Section Earth Surface Geochemistry, Telegrafenberg, 14473 Potsdam, Germany
Jet Rijnders
Biobased Sustainability Engineering (SUSTAIN), Department of Bioscience Engineering, University of Antwerp, Antwerp, Belgium
Lucilla Boito
Biobased Sustainability Engineering (SUSTAIN), Department of Bioscience Engineering, University of Antwerp, Antwerp, Belgium
Jens Hartmann
Institute for Geology, Centre for Earth System Research and Sustainability (CEN), Universität Hamburg, Bundesstraße 55, 20146 Hamburg, Germany
Harun Niron
Biobased Sustainability Engineering (SUSTAIN), Department of Bioscience Engineering, University of Antwerp, Antwerp, Belgium
Reinaldy Poetra
Institute for Geology, Centre for Earth System Research and Sustainability (CEN), Universität Hamburg, Bundesstraße 55, 20146 Hamburg, Germany
Miguel Portillo Estrada
Biobased Sustainability Engineering (SUSTAIN), Department of Bioscience Engineering, University of Antwerp, Antwerp, Belgium
Tom Reershemius
School of Natural and Environmental Sciences, Newcastle University, Newcastle upon Tyne, UK
Laura Steinwidder
Biobased Sustainability Engineering (SUSTAIN), Department of Bioscience Engineering, University of Antwerp, Antwerp, Belgium
Tim Jesper Suhrhoff
Yale Center for Natural Carbon Capture, Yale University, New Haven, CT 06511, USA
Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06511, USA
Biobased Sustainability Engineering (SUSTAIN), Department of Bioscience Engineering, University of Antwerp, Antwerp, Belgium
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Arthur Vienne, Jennifer Newell, Jasper Roussard, Rory Doherty, Siobhan F. Cox, Gary Lyons, and Sara Vicca
Biogeosciences, 23, 1681–1695, https://doi.org/10.5194/bg-23-1681-2026, https://doi.org/10.5194/bg-23-1681-2026, 2026
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We explored whether adding crushed volcanic rock and charcoal to soil could help store inorganic carbon, improve plant growth and reduce harmful metals in crops. The crushed rock did not increase plant growth or inorganic carbon in soil and nutrients released from the rock may have moved into other stable soil forms rather than forming carbonates. In contrast, charcoal improved plant growth and reduced metal uptake. Using both rocks and charcoal together offered no extra observable benefits.
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.
Jens S. Hammes, Jens Hartmann, Johannes A. C. Barth, Tobias Linke, Ingrid Smet, Mathilde Hagens, Philip A. E. Pogge von Strandmann, Tom Reershemius, Bruno Casimiro, Arthur Vienne, Anna A. Stoeckel, Ralf Steffens, and Dirk Paessler
EGUsphere, https://doi.org/10.5194/egusphere-2025-5402, https://doi.org/10.5194/egusphere-2025-5402, 2025
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To test enhanced weathering's efficacy, we ran a two-year greenhouse study under warm, wet conditions, comparing several rock additives across farm soils. We tracked alkalinity and cation soil pools. Soil type was decisive: acidic, low-buffer soils exported more additional alkalinity, while alkaline or pH neutral soils retained it in cation pools. The results point to where enhanced weathering can deliver durable carbon removal and underscore the need for long, well-controlled trials.
Lucilla Boito, Jet Rijnders, Laura Steinwidder, Patrick Frings, Arthur Vienne, Mirthe Maes, Erik Verbruggen, and Sara Vicca
EGUsphere, https://doi.org/10.1101/2025.11.03.686277, https://doi.org/10.1101/2025.11.03.686277, 2025
This preprint is open for discussion and under review for SOIL (SOIL).
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We explored whether adding basalt and beneficial fungi to soil could improve soil health and crop growth. Basalt improved soil chemistry, confirming its role as a soil improver, while the fungi had little effect. Crop yield remained unchanged, showing that benefits depend on soil type. Our study helps clarify how soil amendments work and when they may support farming and climate solutions.
Jet Rijnders, Arthur Vienne, and Sara Vicca
Biogeosciences, 22, 2803–2829, https://doi.org/10.5194/bg-22-2803-2025, https://doi.org/10.5194/bg-22-2803-2025, 2025
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A mesocosm experiment was set up to investigate how maize responds to the application of basalt, concrete fines, and steel slag, using a dose–response approach. Biomass increased with basalt application but did not change with concrete fines or steel slag, except for increased tassel biomass. Mg, Ca, and Si generally increased in the crops, whereas toxic trace elements remained unaffected or even decreased in the plants. Overall, crops were positively affected by the application of silicate materials.
Arthur Vienne, Jennifer Newell, Jasper Roussard, Rory Doherty, Siobhan F. Cox, Gary Lyons, and Sara Vicca
Biogeosciences, 23, 1681–1695, https://doi.org/10.5194/bg-23-1681-2026, https://doi.org/10.5194/bg-23-1681-2026, 2026
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We explored whether adding crushed volcanic rock and charcoal to soil could help store inorganic carbon, improve plant growth and reduce harmful metals in crops. The crushed rock did not increase plant growth or inorganic carbon in soil and nutrients released from the rock may have moved into other stable soil forms rather than forming carbonates. In contrast, charcoal improved plant growth and reduced metal uptake. Using both rocks and charcoal together offered no extra observable benefits.
Jet Rijnders, Lucilla Boito, Laura Steinwidder, Jasper Roussard, Patrick Frings, Harun Niron, and Sara Vicca
EGUsphere, https://doi.org/10.5194/egusphere-2026-603, https://doi.org/10.5194/egusphere-2026-603, 2026
This preprint is open for discussion and under review for Biogeosciences (BG).
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Crushed volcanic rock has been proposed as a way to remove carbon dioxide from the air while improving soil quality. We tested this idea by growing maize in soil with and without the rock and with earthworms. The rock raised soil nutrients, and earthworms boosted these effects. Plant growth stayed similar, but some metals built up in roots. This approach could support farming and climate goals, yet food safety risks must be managed.
Charly A. Moras, Matias Saez Moreno, Peggy Bartsch, and Jens Hartmann
EGUsphere, https://doi.org/10.5194/egusphere-2025-6144, https://doi.org/10.5194/egusphere-2025-6144, 2026
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Ocean alkalinity enhancement has gained popularity to capture carbon dioxide. Yet, most laboratory experiments were run for short term, with strong mixing and without carbon dioxide exchange. In this research, a new setup tried to reproduce a more natural mixing. Overall, alkalinity remained stable for 6 months, thanks to the carbon dioxide invasion which differs from previous research. Hence, potential pitfalls identified in laboratory studies may not be at play in real world application.
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.
Wenche Aas, Thérèse Salameh, Robert Wegener, Heidi Hellén, Jean-Luc Jaffrezo, Pontus Roldin, Elisabeth Alonso-Blanco, Andres Alastuey, Crist Amelynck, Jgor Arduini, Benjamin Bergmans, Marie Bertrand, Agnes Borbon, Efstratios Bourtsoukidis, Laetitia Bouvier, David Butterfield, Iris Buxbaum, Darius Ceburnis, Anja Claude, Aurélie Colomb, Sophie Darfeuil, James Dernie, Maximilien Desservettaz, Elías Díaz-Ramiro, Marvin Dufresne, René Dubus, Mario Duval, Marie Dury, Anna Font, Kirsten Fossum, Evelyn Freney, Gotzon Gangoiti, Yao Ge, Maria Carmen Gomez, Francisco J. Gómez-Moreno, Marie Gohy, Valérie Gros, Paul Hamer, Bryan Hellack, Hartmut Herrmann, Robert Holla, Adéla Holubová, Niels Jensen, Tuija Jokinen, Matthew Jones, Uwe Käfer, Lukas Kesper, Dieter Klemp, Dagmar Kubistin, Angela Marinoni, Martina Mazzini, Vy Ngoc Thuy Dinh, Jurgita Ovadnevaite, Tuukka Petäjä, Miguel Portillo-Estrada, Jitka Přívozníková, Jean-Philippe Putaud, Stefan Reimann, Laura Renzi, Veronique Riffault, Stuart Ritchie, Chris Robins, Begoña Artíñano Rodríguez de Torres, Laurent Poulain, Julian Rüdiger, Agnieszka Sanocka, Estibaliz Saez de Camara Oleaga, Niels Schoon, Roger Seco, Ivan Simmons, Leïla Simon, David Simpson, Emmanuel Tison, August Thomasson, Svetlana Tsyro, Marsailidh Twigg, Toni Tykkä, Bert Verreyken, Ana Maria Yáñez-Serrano, Sverre Solberg, Karen Yeung, Ilona Ylivinkka, Karl Espen Yttri, Ågot Watne, and Katie Williams
EGUsphere, https://doi.org/10.5194/egusphere-2025-6166, https://doi.org/10.5194/egusphere-2025-6166, 2025
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A one-week intensive VOC and organic-tracer campaign during the 2022 European heatwave showed contributions from both biogenic and anthropogenic sources to ozone and SOA peaks, while model–observation differences underline the need for better characterization of sources and formation pathways.
Jens S. Hammes, Jens Hartmann, Johannes A. C. Barth, Tobias Linke, Ingrid Smet, Mathilde Hagens, Philip A. E. Pogge von Strandmann, Tom Reershemius, Bruno Casimiro, Arthur Vienne, Anna A. Stoeckel, Ralf Steffens, and Dirk Paessler
EGUsphere, https://doi.org/10.5194/egusphere-2025-5402, https://doi.org/10.5194/egusphere-2025-5402, 2025
Short summary
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To test enhanced weathering's efficacy, we ran a two-year greenhouse study under warm, wet conditions, comparing several rock additives across farm soils. We tracked alkalinity and cation soil pools. Soil type was decisive: acidic, low-buffer soils exported more additional alkalinity, while alkaline or pH neutral soils retained it in cation pools. The results point to where enhanced weathering can deliver durable carbon removal and underscore the need for long, well-controlled trials.
Lucilla Boito, Jet Rijnders, Laura Steinwidder, Patrick Frings, Arthur Vienne, Mirthe Maes, Erik Verbruggen, and Sara Vicca
EGUsphere, https://doi.org/10.1101/2025.11.03.686277, https://doi.org/10.1101/2025.11.03.686277, 2025
This preprint is open for discussion and under review for SOIL (SOIL).
Short summary
Short summary
We explored whether adding basalt and beneficial fungi to soil could improve soil health and crop growth. Basalt improved soil chemistry, confirming its role as a soil improver, while the fungi had little effect. Crop yield remained unchanged, showing that benefits depend on soil type. Our study helps clarify how soil amendments work and when they may support farming and climate solutions.
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Large-scale atmospheric pathways connecting climate across latitudes are poorly documented in the past. Using a high-resolution spatial and temporal reconstruction of the evolution of the Southern Hemisphere Westerlies since the Last Glacial Maximum and comparing it with the evolution of the Intertropical Convergence Zone, we identified the dominant atmospheric pathways that shaped past South American climate.
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 under review 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.
Jet Rijnders, Arthur Vienne, and Sara Vicca
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A mesocosm experiment was set up to investigate how maize responds to the application of basalt, concrete fines, and steel slag, using a dose–response approach. Biomass increased with basalt application but did not change with concrete fines or steel slag, except for increased tassel biomass. Mg, Ca, and Si generally increased in the crops, whereas toxic trace elements remained unaffected or even decreased in the plants. Overall, crops were positively affected by the application of silicate materials.
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Ocean alkalinity enhancement (OAE) is being assessed for its potential to absorb atmospheric CO2 and store it for a long time. OAE still needs comprehensive assessment of its safety and effectiveness. We studied an idealised OAE application in a natural low-nutrient ecosystem over 1 month. Our results showed that biogeochemical functioning remained mostly stable but that the long-term capability for storing carbon may be limited at high alkalinity concentration.
Niels Suitner, Jens Hartmann, Selene Varliero, Giulia Faucher, Philipp Suessle, and Charly A. Moras
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Alkalinity leakage limits the efficiency of ocean alkalinity enhancement. Drivers of this process remain unquantified, restricting accurate assessments. The induced runaway process can be modeled using surface area and aragonite oversaturation as key factors. This study proposes a framework for improving predictability of alkalinity loss due to runaway precipitation, emphasizing the need for field experiments to validate theoretical models concerning dilution and particle sinking processes.
Niels Suitner, Giulia Faucher, Carl Lim, Julieta Schneider, Charly A. Moras, Ulf Riebesell, and Jens Hartmann
Biogeosciences, 21, 4587–4604, https://doi.org/10.5194/bg-21-4587-2024, https://doi.org/10.5194/bg-21-4587-2024, 2024
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Recent studies described the precipitation of carbonates as a result of alkalinity enhancement in seawater, which could adversely affect the carbon sequestration potential of ocean alkalinity enhancement (OAE) approaches. By conducting experiments in natural seawater, this study observed uniform patterns during the triggered runaway carbonate precipitation, which allow the prediction of safe and efficient local application levels of OAE scenarios.
Annika Nolte, Ezra Haaf, Benedikt Heudorfer, Steffen Bender, and Jens Hartmann
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This study examines about 8000 groundwater level (GWL) time series from five continents to explore similarities in groundwater systems at different scales. Statistical metrics and machine learning techniques are applied to identify common GWL dynamics patterns and analyze their controlling factors. The study also highlights the potential and limitations of this data-driven approach to improve our understanding of groundwater recharge and discharge processes.
Nestor Gaviria-Lugo, Charlotte Läuchli, Hella Wittmann, Anne Bernhardt, Patrick Frings, Mahyar Mohtadi, Oliver Rach, and Dirk Sachse
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We analyzed how leaf wax hydrogen isotopes in continental and marine sediments respond to climate along one of the strongest aridity gradients in the world, from hyperarid to humid, along Chile. We found that under extreme aridity, the relationship between hydrogen isotopes in waxes and climate is non-linear, suggesting that we should be careful when reconstructing past hydrological changes using leaf wax hydrogen isotopes so as to avoid overestimating how much the climate has changed.
Nele Lehmann, Hugues Lantuit, Michael Ernst Böttcher, Jens Hartmann, Antje Eulenburg, and Helmuth Thomas
Biogeosciences, 20, 3459–3479, https://doi.org/10.5194/bg-20-3459-2023, https://doi.org/10.5194/bg-20-3459-2023, 2023
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Riverine alkalinity in the silicate-dominated headwater catchment at subarctic Iskorasfjellet, northern Norway, was almost entirely derived from weathering of minor carbonate occurrences in the riparian zone. The uphill catchment appeared limited by insufficient contact time of weathering agents and weatherable material. Further, alkalinity increased with decreasing permafrost extent. Thus, with climate change, alkalinity generation is expected to increase in this permafrost-degrading landscape.
Mingyang Tian, Jens Hartmann, Gibran Romero-Mujalli, Thorben Amann, Lishan Ran, and Ji-Hyung Park
Biogeosciences Discuss., https://doi.org/10.5194/bg-2023-131, https://doi.org/10.5194/bg-2023-131, 2023
Manuscript not accepted for further review
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Effective water quality management in the Elbe River from 1984 to 2018 significantly reduced CO2 emissions, particularly after Germany's reunification. Key factors in the reduction include organic carbon removal and nutrient management, with nitrogen control being more critical than phosphorus for the restoration of ecosystem capacity. Unpredictable influxes of organic carbon and the relocation of emissions from wastewater treatment can cause uncertainties for CO2 removals.
Matteo Willeit, Tatiana Ilyina, Bo Liu, Christoph Heinze, Mahé Perrette, Malte Heinemann, Daniela Dalmonech, Victor Brovkin, Guy Munhoven, Janine Börker, Jens Hartmann, Gibran Romero-Mujalli, and Andrey Ganopolski
Geosci. Model Dev., 16, 3501–3534, https://doi.org/10.5194/gmd-16-3501-2023, https://doi.org/10.5194/gmd-16-3501-2023, 2023
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In this paper we present the carbon cycle component of the newly developed fast Earth system model CLIMBER-X. The model can be run with interactive atmospheric CO2 to investigate the feedbacks between climate and the carbon cycle on temporal scales ranging from decades to > 100 000 years. CLIMBER-X is expected to be a useful tool for studying past climate–carbon cycle changes and for the investigation of the long-term future evolution of the Earth system.
Jens Hartmann, Niels Suitner, Carl Lim, Julieta Schneider, Laura Marín-Samper, Javier Arístegui, Phil Renforth, Jan Taucher, and Ulf Riebesell
Biogeosciences, 20, 781–802, https://doi.org/10.5194/bg-20-781-2023, https://doi.org/10.5194/bg-20-781-2023, 2023
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CO2 can be stored in the ocean via increasing alkalinity of ocean water. Alkalinity can be created via dissolution of alkaline materials, like limestone or soda. Presented research studies boundaries for increasing alkalinity in seawater. The best way to increase alkalinity was found using an equilibrated solution, for example as produced from reactors. Adding particles for dissolution into seawater on the other hand produces the risk of losing alkalinity and degassing of CO2 to the atmosphere.
Shuang Gao, Jörg Schwinger, Jerry Tjiputra, Ingo Bethke, Jens Hartmann, Emilio Mayorga, and Christoph Heinze
Biogeosciences, 20, 93–119, https://doi.org/10.5194/bg-20-93-2023, https://doi.org/10.5194/bg-20-93-2023, 2023
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We assess the impact of riverine nutrients and carbon (C) on projected marine primary production (PP) and C uptake using a fully coupled Earth system model. Riverine inputs alleviate nutrient limitation and thus lessen the projected PP decline by up to 0.7 Pg C yr−1 globally. The effect of increased riverine C may be larger than the effect of nutrient inputs in the future on the projected ocean C uptake, while in the historical period increased nutrient inputs are considered the largest driver.
Niel Verbrigghe, Niki I. W. Leblans, Bjarni D. Sigurdsson, Sara Vicca, Chao Fang, Lucia Fuchslueger, Jennifer L. Soong, James T. Weedon, Christopher Poeplau, Cristina Ariza-Carricondo, Michael Bahn, Bertrand Guenet, Per Gundersen, Gunnhildur E. Gunnarsdóttir, Thomas Kätterer, Zhanfeng Liu, Marja Maljanen, Sara Marañón-Jiménez, Kathiravan Meeran, Edda S. Oddsdóttir, Ivika Ostonen, Josep Peñuelas, Andreas Richter, Jordi Sardans, Páll Sigurðsson, Margaret S. Torn, Peter M. Van Bodegom, Erik Verbruggen, Tom W. N. Walker, Håkan Wallander, and Ivan A. Janssens
Biogeosciences, 19, 3381–3393, https://doi.org/10.5194/bg-19-3381-2022, https://doi.org/10.5194/bg-19-3381-2022, 2022
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In subarctic grassland on a geothermal warming gradient, we found large reductions in topsoil carbon stocks, with carbon stocks linearly declining with warming intensity. Most importantly, however, we observed that soil carbon stocks stabilised within 5 years of warming and remained unaffected by warming thereafter, even after > 50 years of warming. Moreover, in contrast to the large topsoil carbon losses, subsoil carbon stocks remained unaffected after > 50 years of soil warming.
Melanie S. Verlinden, Hamada AbdElgawad, Arne Ven, Lore T. Verryckt, Sebastian Wieneke, Ivan A. Janssens, and Sara Vicca
Biogeosciences, 19, 2353–2364, https://doi.org/10.5194/bg-19-2353-2022, https://doi.org/10.5194/bg-19-2353-2022, 2022
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Zea mays grows in mesocosms with different soil nutrition levels. At low phosphorus (P) availability, leaf physiological activity initially decreased strongly. P stress decreased over the season. Arbuscular mycorrhizal fungi (AMF) symbiosis increased over the season. AMF symbiosis is most likely responsible for gradual reduction in P stress.
Lore T. Verryckt, Sara Vicca, Leandro Van Langenhove, Clément Stahl, Dolores Asensio, Ifigenia Urbina, Romà Ogaya, Joan Llusià, Oriol Grau, Guille Peguero, Albert Gargallo-Garriga, Elodie A. Courtois, Olga Margalef, Miguel Portillo-Estrada, Philippe Ciais, Michael Obersteiner, Lucia Fuchslueger, Laynara F. Lugli, Pere-Roc Fernandez-Garberí, Helena Vallicrosa, Melanie Verlinden, Christian Ranits, Pieter Vermeir, Sabrina Coste, Erik Verbruggen, Laëtitia Bréchet, Jordi Sardans, Jérôme Chave, Josep Peñuelas, and Ivan A. Janssens
Earth Syst. Sci. Data, 14, 5–18, https://doi.org/10.5194/essd-14-5-2022, https://doi.org/10.5194/essd-14-5-2022, 2022
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We provide a comprehensive dataset of vertical profiles of photosynthesis and important leaf traits, including leaf N and P concentrations, from two 3-year, large-scale nutrient addition experiments conducted in two tropical rainforests in French Guiana. These data present a unique source of information to further improve model representations of the roles of N and P, and other leaf nutrients, in photosynthesis in tropical forests.
Cited articles
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Amann, T., Hartmann, J., Hellmann, R., Pedrosa, E. T., and Malik, A.: Enhanced weathering potentials – the role of in situ CO2 and grain size distribution, Front. Clim., 4, 929268, https://doi.org/10.3389/fclim.2022.929268, 2022.
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Short summary
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.
Our study explores Enhanced Weathering (EW) using basalt rock dust to combat climate change. We...