Articles | Volume 23, issue 21
https://doi.org/10.5194/bg-23-7727-2026
https://doi.org/10.5194/bg-23-7727-2026
Research article
 | Highlight paper
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04 Nov 2026
Research article | Highlight paper |  | 04 Nov 2026

Enhanced weathering of glacial rock flour drives coupled inorganic and organic carbon sequestration in a five-year field experiment

Christiana Dietzen, Malgorzata Rizzi, Tim Jesper Suhrhoff, and Minik Thorleif Rosing

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2026-2760', Anonymous Referee #1, 27 Jun 2026
    • AC1: 'Reply on RC1', Christiana Dietzen, 04 Aug 2026
  • RC2: 'Comment on egusphere-2026-2760', Anonymous Referee #2, 23 Jul 2026
    • AC2: 'Reply on RC2', Christiana Dietzen, 04 Aug 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (07 Aug 2026) by Mike Rowley
AR by Christiana Dietzen on behalf of the Authors (30 Sep 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (04 Oct 2026) by Mike Rowley
RR by Anonymous Referee #1 (04 Oct 2026)
ED: Publish as is (05 Oct 2026) by Mike Rowley
AR by Christiana Dietzen on behalf of the Authors (20 Oct 2026)
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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.
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.
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