About Rock Weathering
- Rock weathering is a geo-chemical process where rocks break down into minerals over thousands of years. During this process, atmospheric carbon dioxide (CO2) reacts with minerals like calcium and magnesium, turning into bicarbonates.
- These bicarbonates eventually travel through aquifers and settle in the oceans, where the carbon is locked away for aeons.
- Natural rock weathering takes a long time—over thousands of years—to remove significant CO2 from the atmosphere.
Enhanced Rock Weathering
- It is a process that accelerates the natural weathering of rocks.
- Basaltic rock into fine powder increases the surface area of the rock dramatically, enhancing the reaction rate of carbon with minerals.
- This enhanced process can capture carbon 10 to 100 times faster than natural weathering, depending on environmental factors like soil, temperature, and proximity to rivers.
- The bicarbonates formed from the process can be flushed into oceans within a month.
Carbon Capture |
Carbon sequestration
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