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Response: Enhanced mineral weathering

Weathered basalt, Reynisfjara, Iceland – image: Sonny Whitelaw

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Enhanced mineral weathering

Summary

“Biogeochemical improvement of soils by adding crushed, fast-reacting silicate rocks to croplands is one such CO2-removal strategy. This approach has the potential to improve crop production, increase protection from pests and diseases, and restore soil fertility and structure.”Beerling et al, 2022.


How does it work?

The following is an extract from Carbon Brief: How ‘enhanced weathering’ could slow climate change and boost crop yields’ (Fig. 1)

Chemical weathering is a natural process that continuously erodes away rocks and stores atmospheric CO2 over millions of years. As natural rock weathering absorbs around 0.3% of global fossil fuel emissions, enhanced weathering can provide a boost to remove even more CO2 from our atmosphere.

The process begins with rain, which is usually slightly acidic having absorbed CO2 from the atmosphere on its journey to the ground. The acidic rain reacts with rocks and soils, gradually breaking them down into rock grains, forming bicarbonate in the process. Eventually, this bicarbonate washes into the oceans, where the carbon is stored in dissolve form for hundreds of thousands of years or locked up on the sea floor.

Enhanced weathering scales up this process. Pulverising silicate rocks such as basalt – left over from ancient volcanic eruptions – bypasses the slow weathering action because power has a greater surface area that large rocks, so it absorbs carbon much faster.

As enhanced weathering makes water more alkaline, it can help counteract ocean acidification.

When spread on large areas of agricultural land, plant roots and microbes in the soil speed up the chemical reactions, boosting nutrient levels, improving crop yields and helping restore degraded agricultural soils (Video 1).

Home > Climate wiki > Response > Enhanced mineral weathering

Summary

“Biogeochemical improvement of soils by adding crushed, fast-reacting silicate rocks to croplands is one such CO2-removal strategy. This approach has the potential to improve crop production, increase protection from pests and diseases, and restore soil fertility and structure.”Beerling et al, 2022.

How does it work?

The following is an extract from Carbon Brief: How ‘enhanced weathering’ could slow climate change and boost crop yields’. (Fig. 1)

Chemical weathering is a natural process that continuously erodes away rocks and stores atmospheric CO2 over millions of years. As natural rock weathering absorbs around 0.3% of global fossil fuel emissions, enhanced weathering can provide a boost to remove even more CO2 from our atmosphere.

The process begins with rain, which is usually slightly acidic having absorbed CO2 from the atmosphere on its journey to the ground. The acidic rain reacts with rocks and soils, gradually breaking them down into rock grains, forming bicarbonate in the process. Eventually, this bicarbonate washes into the oceans, where the carbon is stored in dissolve form for hundreds of thousands of years or locked up on the sea floor.

Enhanced weathering scales up this process. Pulverising silicate rocks such as basalt – left over from ancient volcanic eruptions – bypasses the slow weathering action because power has a greater surface area that large rocks, so it absorbs carbon much faster.

As enhanced weathering makes water more alkaline, it can help counteract ocean acidification.

When spread on large areas of agricultural land, plant roots and microbes in the soil speed up the chemical reactions, boosting nutrient levels, improving crop yields and helping restore degraded agricultural soils (Video 1).

Fig. 1: Advanced rock weather to drawdown carbon dioxide and improve soils (image: Carbon Brief)
Fig. 1: Advanced rock weather to drawdown carbon dioxide and improve soils (image: Carbon Brief)
Video 1: Concept and testing in different parts of the world to determine viability and efficiency at scale.