Schlagwort: Carbon Dioxide Removal

Shen et al. (2026): Atmospheric CO₂ drawdown during the Emeishan flood basalt volcanism

Jiaheng Shen, Yi Ge Zhang, Dong-Xun Yuan & Yi-Gang Xu, IN: Nature Communications, https://doi.org/10.1038/s41467-026-69600-z

The conventional model linking large igneous provinces (LIPs) to atmospheric CO₂ concentrations (pCO₂) predicts elevated CO₂ during volcanic emplacement, leading to biotic crises. However, this generalization requires testing. Here, the authors reconstruct pCO₂ variations throughout the Emeishan LIP emplacement (~260 Ma) using carbon isotopes from chlorophyll-derived compounds.

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Chen et al. (2026): Sustainability analysis of basalt enhanced weathering in China under the carbon neutrality pathway

Xinyu Chen, Xuan Wang, Xiaoping Jia, Siqi Wang, Raymond R. Tan, Bohong Wang, Fang Wang, IN: Environmental Impact Assessment Review, https://doi.org/10.1016/j.eiar.2026.108396

Enhanced weathering (EW) of basalt is a promising negative emission technology (NET) for carbon dioxide removal (CDR), yet its large-scale sustainability remains uncertain, particularly in energy-intensive economies like China. This work develops an environmentally extended input-output (EEIO) model to evaluate the economic and environmental impacts of basalt EW deployment under China’s carbon neutrality pathway. This framework integrates life-cycle emissions from mining, comminution, transportation, and cropland application, quantifying trade-offs between CDR potential and process-related carbon footprints.

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Schiedung et al. (2026): Uncertainties of enhanced rock weathering for climate-change mitigation

Marcus Schiedung, Kirsty J. Harrington, Xavier Dupla, Benjamin Möller, Ennio Facq, Tim Sweere, Axel Don, Robert G. Hilton, Sebastian Doetterl and Jordon D. Hemingway, IN: Nature Reviews Earth & Environment, https://doi.org/10.1038/s43017-026-00761-7

Enhanced rock weathering (ERW) on agricultural soils is under consideration as a long-term carbon dioxide removal (CDR) strategy. In this Perspective, the authors evaluate uncertainties related to ERW around feedstock availability, plant–soil system impacts, CDR efficiency along the land–ocean continuum and socio-economic considerations.

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Bishop et al. (2026): Cascading wood use into bioenergy with carbon capture and storage ensures continuous and enduring temperature reduction

George Bishop, Colm Duffy, Goran Berndes, Miguel Brandao, Annette Cowie, John Healey, Christiane Hennig, Kati Koponen, James Gaffey & David Styles, IN: Bangor University

Bioenergy with carbon capture and storage (BECCS) is a key component of pathways to net zero, yet potential interactions with forest carbon dynamics, cascading wood strategies, and progressive decarbonisation and CCS deployment are poorly represented in assessments. Here, using dynamic life cycle assessment, the authors explore these factors for sawmill residue-derived BECCS value chains over long, yet flexible, time-horizons.

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Watson & Bui (2026): Can temporary carbon dioxide removal fix a long-term climate problem? An analysis of equivalency ratios and the like-for-like approach

Charles Watson and Mai Bui, IN: Environmental Research: Climate, https://doi.org/10.1088/2752-5295/ae4058

Carbon dioxide removal (CDR) technologies are increasingly important for meeting climate targets. These can vary widely in terms of their permanence, with some methods temporarily storing carbon for decades and others storing carbon for millennia or longer. Economic equivalency ratios have been developed to understand and compare the value of CDR options in terms of permanence. These ratios enable the conversion of temporary carbon storage (i.e., low permanence) into an equivalent permanent value, using tools like discounting, time horizons, and damage functions. This study comparatively evaluates three key methods-the climate repair value, the social value of an offset, and discounted tonne-year accounting-by combining a Sobol sensitivity analysis with a critical qualitative assessment of their underlying assumptions.

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Tu et al. (2026): Scaling up enhanced rock weathering for equitable climate change mitigation

Ying Tu, Radine Rafols, Yangyang Xu, Natalia Butler, Linah Ababneh, Feng Tao, Veerabhadran Ramanathan, Benjamin Z. Houlton and Chuan Liao, IN: Communications Sustainability, https://doi.org/10.1038/s44458-026-00034-w

Enhanced rock weathering (ERW) is an emerging approach to remove carbon dioxide from the atmosphere while improving soil health and crop productivity. Yet its long-term climate impact remains uncertain due to limited understanding of how adoption will evolve across regions, income groups, and in response to a warming world. Here, the authors combine historical analogs of technological diffusion with a coupled human–nature feedback model to provide spatially explicit projections of global ERW adoption through 2100.

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Li et al. (2026): Alkaline materials for coastal ocean alkalinity enhancement: A comparative study of natural silicates and industrial byproducts

Xinyu Li, Zhe Zhou, Heng Xiao, Jiangtao Li and Shouye Yang, IN: Marine Pollution Bulletin, https://doi.org/10.1016/j.marpolbul.2026.119338

Coastal ocean alkalinity enhancement (OAE) is a promising ocean-based carbon dioxide removal (CDR) approach for mitigating climate change and counteracting ocean acidification. However, uncertainties persist regarding the efficacy and environmental safety of alkaline materials under realistic coastal conditions. This study comparatively investigated the CO₂ sequestration potential, geochemical processes, and environmental impacts of four alkaline materials—natural silicates (olivine, basalt) and industrial byproducts (fly ash, steel slag)—through laboratory incubations with natural seawater (filtered and unfiltered) and in situ deployments off the East China Sea.

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Brander et al. (2026): Clarifying what is meant by greenhouse gas ‘removals’ and categorising types of ‘removal-related activities’

Matthew Brander, Derik Broekhoff and Maurice Bryson, IN: Climate Policy, https://doi.org/10.1080/17583004.2026.2625956

There is broad recognition that removals of carbon dioxide and other greenhouse gases (GHGs) will be required for counter-balancing emissions from hard-to-abate sectors to achieve net zero, and will also be necessary in the increasingly likely event of an emissions overshoot in order to return atmospheric concentrations of GHGs and temperature change below target levels. However, the term “removal” is open to imprecise usage, which is likely to result in confusion over which activities policy-makers, investors and carbon credit buyers wish to support, and what project developers and technology providers actually deliver. This commentary paper aims to clarify what is meant by “removals” by analysing the definitions from prominent sources and by proposing a precise definition of the term.

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Hussain et al. (2026): High-Resolution Satellite-Driven Estimation of Photosynthetic Carbon Sequestration in the Sundarbans Mangrove Forest, Bangladesh

Nur Hussain, Md Adnan Rahman, Md Rezaul Karim, Parvez Rana, Md Nazrul Islam and Anselme Muzirafuti, IN: Remote Sensing, https://www.mdpi.com/2072-4292/18/3/401

Mangrove forests provide essential climate regulation and coastal protection, yet fine-scale quantification of carbon dynamics remains limited in the Sundarbans due to spatial heterogeneity and tidal influences. This study estimated canopy structural and photosynthetic dynamics from 2019 to 2023 by integrating 10 m spatial high-resolution remote sensing with a light use efficiency (LUE) modeling framework. Leaf Area Index (LAI) was retrieved at 10 m resolution using the PROSAIL radiative transfer model applied to Sentinel-2 data to characterize the canopy structure of the mangrove forest. LUE-based Gross Primary Productivity (GPP) was estimated using Sentinel-2 vegetation and water indices and MODIS fPAR with station observatory temperature data.

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Gholamahmadi & Kammann (2026): Biochar for durable carbon removal: soil erosion reduction as a key mechanism

Behrouz Gholamahmadi and Claudia Kammann, IN: Biochar, https://doi.org/10.1016/j.bmf.2026.100020

Soil erosion is a major pathway of physical soil organic carbon (SOC) loss and a critical threat to the permanence of land-based carbon dioxide removal (CDR). Biochar is widely recognised as a durable carbon sink, yet its hydrological effects and erosion-mitigation potential remain undervalued in CDR frameworks. Here the authors synthesise global evidence and long-term Mediterranean experiments to show that hydrological improvements—an enhanced soil sponge function—are not ancillary co-benefits but a core mechanism supporting carbon durability.

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