beccs hero portrait

How it works:

Bioenergy Carbon
Capture and Storage

Bioenergy with Carbon Capture and Storage (BECCS) is one of the most effective ways to permanently remove CO2 from the atmosphere.

  • Biomass

    Biomass
  • CO₂ emitter

    Emitter
  • Capture

    Capture
  • Liquefaction
& buffer storage

    Liquefaction
& buffer storage
  • Transportation

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  • Permanent storage

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Our BECCS projects are built with the highest safety and integrity standards to ensure every tonne of captured CO2 is securely and permanently stored underground.

Step-by-step breakdown of how we capture, transport, and store CO₂ safely and reliably.

beccs forest webp

CO₂ is absorbed by trees

Trees naturally pull CO₂ from the air as they grow, storing carbon in their wood. By managing forests sustainably, we can use wood and forestry residues to create products and generate energy, reducing our reliance on fossil fuels.

HOFOR biomass

Biomass waste is turned into energy

At bioenergy facilities, sustainably sourced biomass—such as forestry residues—is used to produce heat and power. During combustion, biogenic CO₂ is released, but instead of entering the atmosphere, it’s captured from the plant’s flue gases using proven technology. This process shifts the system from carbon-neutral to carbon-negative.

How it works

CO₂ is prepared for transport

Once captured, the CO₂ gas is cooled and compressed to make it compact and stable, essential for safe and efficient transportation. In this liquid-like state, it can be stored in tanks until it’s ready to be moved.

boat how it works

CO₂ is transported to a storage site

The liquified CO₂ is then shipped to its permanent storage location by pipeline, train, or specialized vessel under stringent safety measures that ensure secure handling at every step.

water

CO₂ is stored deep underground

Upon arrival at the storage site, the CO₂ is injected deep underground into geological reservoirs called deep saline aquifers—often located beneath the North Sea. These reservoirs lie beneath a thick, impermeable rock layer that prevents the CO₂ from migrating upwards.

Within the aquifer, the CO₂ is trapped in tiny pore spaces, dissolves into the salty water, and over time forms solid minerals. This natural barrier of rock, combined with these processes, keeps the CO₂ securely locked away for more than a thousand years.