High-permanence carbon removal
The IPCC estimates that 10 to 20% of current GHG emissions cannot be avoided in the medium term, meaning that even with massive efforts to reduce emissions at the source, humanity will continue to emit 5 to 10 billion tonnes of CO2 equivalent every year by 2050, mainly from agriculture, transport, and some industrial processes. Removing an equivalent amount of carbon from the atmosphere will thus be necessary to reach climate-neutrality by mid-century.
Natural carbon removal solutions such as trees can play a significant part in this effort, but will not be enough given that:
- they carry intrinsic physical limitations such as land availability for reforestation programmes;
- they come with a non-negligeable risk of reversal, mainly because of wildfires, deforestation, and droughts.
Engineered carbon removal solutions are therefore necessary as a complement, and need to feature guaranteed high-permanence removal. Biochar is one of only a handful of such solutions. It allows for hundreds of years of guaranteed carbon removal, has a global sustainable removal capacity of up to 2 billion tonnes of CO2 equivalent a year, and is to date the most mature solution to be brought at scale, with already-available technology and very strong scientific backing.
Biochar is one of only a few long-term sequestration technologies, and the one at highest technology readiness level.
Biochar for climate
The global sustainable potential for negative emissions through biochar is between 1 and 2 GtCO2 per year.
Biochar's main chemical component is carbon. This carbon was originally captured by plants in the atmosphere through photosynthesis, and is then extracted and stabilised during the pyrolysis process. When put in the soil, this carbon remains there for at least hundreds of years. Thus, biochar is a high-permanence carbon removal solution.
According to the IPCC, when deployed at a global scale and taking into account sustainability constraints, biochar can remove every year up to 2 billion tonnes of CO2 from the atmosphere.