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Study finds natural basalt weathering removes less CO2 than assumed

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GoKawiil Brief

Researchers compiled river chemistry data from basaltic watersheds worldwide to recalculate how much carbon dioxide is naturally absorbed through silicate rock weathering. They found that critical zone processes—such as atmospheric deposition, hydrothermal contamination and secondary mineral formation—reduce the alkalinity that actually reaches rivers, meaning basalt weathering contributes a smaller share of global CO2 drawdown than prior estimates suggested, roughly 0.3% of annual anthropogenic emissions.

Why It Matters

GoKawiil's interpretation of the reporting above, not reported fact.

This matters because basalt weathering is central to proposed enhanced weathering strategies for carbon removal, and if natural systems export less alkalinity than assumed, engineered approaches may need to account for similar losses. The findings suggest that scaling up basalt-based carbon capture could be less efficient than optimistic models imply, requiring more rigorous field validation before large-scale deployment.

Key Takeaways
Worth a Look

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Source: nature.com — Derry, 2026-08-26

Published there as: “Critical zone processes limit alkalinity export from natural basaltic systems”

Read the original report → The summary and analysis above are GoKawiil's own, written from reporting by the source above. Facts and quotes belong to the original publisher.