David Beerling
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Carbon dioxide regulation of Earth’s ecological weathering engine: from microorganisms to ecosystems
Open Date: 2013-06-01
Close Date: 2018-05-31
Grant: Close
Carbon dioxide regulation of Earth’s ecological weathering engine: from microorganisms to ecosystems
Open Date: 2013-06-01
Close Date: 2018-05-31
Articles (10)
Forestation is widely proposed for carbon dioxide (CO 2 ) removal, but its impact on climate through changes to atmospheric composition and surface albedo remains relatively unexplored. We assessed these responses using two Earth system models by comparing a scenario with extensive global forest expansion in suitable regions to other plausible futures. We found that forestation increased aerosol scattering and the greenhouse gases methane and ozone following increased biogenic organic emissions. Additionally, forestation decreased surface albedo, which yielded a positive radiative forcing (i.e., warming). This offset up to a third of the negative forcing from the additional CO 2 removal under a 4°C warming scenario. However, when forestation was pursued alongside other strategies that achieve the 2°C Paris Agreement target, the offsetting positive forcing was smaller, highlighting the urgency for simultaneous emission reductions.
Year:
2024
Terrestrial enhanced weathering (EW) of silicate rocks, such as crushed basalt, on farmlands is a promising scalable atmospheric carbon dioxide removal (CDR) strategy that urgently requires performance assessment with commercial farming practices. We report findings from a large-scale replicated EW field trial across a typical maize-soybean rotation on an experimental farm in the heart of the United Sates Corn Belt over 4 y (2016 to 2020). We show an average combined loss of major cations (Ca 2+ and Mg 2+ ) from crushed basalt applied each fall over 4 y (50 t ha −1 y −1 ) gave a conservative time-integrated cumulative CDR potential of 10.5 ± 3.8 t CO 2 ha −1 . Maize and soybean yields increased significantly ( P < 0.05) by 12 to 16% with EW following improved soil fertility, decreased soil acidification, and upregulation of root nutrient transport genes. Yield enhancements with EW were achieved with significantly ( P < 0.05) increased key micro- and macronutrient concentrations (including potassium, magnesium, manganese, phosphorus, and zinc), thus improving or maintaining crop nutritional status. We observed no significant increase in the content of trace metals in grains of maize or soybean or soil exchangeable pools relative to controls. Our findings suggest that widespread adoption of EW across farming sectors has the potential to contribute significantly to net-zero greenhouse gas emissions goals while simultaneously improving food and soil security.
Year:
2024
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2024
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2024
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2024
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2024
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2023
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2023
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2023
Year:
2023
Collaborators (23)
Steven A. Banwart
University of Leeds
David Greenwood
Professor
Brandon University
Morgan Schaller
Associate Professor
Rensselaer Polytechnic Institute
James Keeble
University of Lancaster
Dan Breecker
Associate Professor
University of Texas at Austin
Bernhard Naafs
Proleptic senior lecturer
University of Bristol
Ying Cui
Assistant Professor
Montclair State University
Maria Val Martin
University of Sheffield
Ross Whiteford
University of St. Andrews
Ethan Hyland
Asst. Professor
North Carolina State University
Daniel Grosvenor
University of Leeds
Tom Reershemius
Lecturer
Newcastle University
Pratigya Polissar
Associate Professor
University of California, Santa Cruz
Wolfram Michael Kürschner
Professor
University of Oslo
James King
University of Sheffield
Gabriel Bowen
Professor
University of Utah
Nathan Sheldon
University of Michigan
Michael Henehan
University of Bristol
Matthew Kohn
University Distinguished Professor
Boise State University
Dana Royer
Wesleyan University
Daniel L. Sanchez
University of California
Andy Ridgwell
University of Bristol
James Weber
University of Reading
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