recarbono

Biochar

What is biochar?

A stable, porous carbon made by heating biomass without oxygen. It locks carbon away for centuries, brings soil back to life, and is also built into construction materials such as concrete and mortars.

The idea

Carbon, taken out of the fast cycle

Plants capture CO₂ as they grow, but when they rot or burn, nearly all of it returns to the air within years. Biochar interrupts that loop: convert the biomass to stable carbon first, and what took a season to capture stays captured for centuries.

2,000 years of evidence

Terra preta knew first

In the Amazon basin, patches of earth called terra preta are darker and more fertile than anything around them, enriched with charred biomass by farmers more than 2,000 years ago. The carbon is still there. Modern biochar is that discovery, engineered: the same chemistry, now measured and verified.

How it's made

Heat it where fire can't follow

Deprived of oxygen, biomass can't burn. Heated to 450–700 °C it pyrolyses instead: volatiles leave as energy-rich gas, and the carbon left behind reorganises into stable aromatic structures. The result is porous, black and durable: biochar.

01

Biomass

Fire-risk forestry & agricultural residue

02

Pyrolysis

450–700 °C · no oxygen · energy released

03

Biochar

Stable carbon + heat as co-product

See the full journey of a tonne

The journey of a tonne

From residual biomass to stable carbon in the soil

An olive branch with fruit and pruned twigs, half photograph and half fine teal wireframe of the same branch with leader lines: the feedstock as a measured study.

FIG. 012 · OLEA EUROPAEA

01Capture

A residue that would otherwise burn or rot: olive prunings, olive stones from the mills (around 150,000 t a year in Portugal), forest thinnings, cork oak. Photosynthesis already pulled the carbon out of the air; the only question left is whether it goes back.

A single branch in three states: photographic raw wood on the left dissolving into a fine teal wireframe lattice mid-length, re-emerging as glossy porous black biochar on the right.

FIG. 002 · PYROLYSIS · 450–700 °C

02Transform

Heated to 450–700 °C without oxygen, the material does not burn. Its carbon reorganises into stable aromatic structures that resist decomposition.

Black biochar granules pouring from a steel chute, dissolving mid-fall into fine teal wireframes of the same porous granules with schematic CO₂ molecules locked inside their pores.

FIG. 003 · POROUS STRUCTURE · LOCKED CO₂

03Lock

What emerges is porous, glassy and stubborn. Permanence is measured from this structure itself (the H/C ratio, read by accredited laboratories), not inferred from the settings of the machine that made it.

A seedling in a soil cross-section, photographic topsoil with biochar fragments dissolving downward into fine teal wireframe strata where porous fragments hold water droplets among the roots.

FIG. 004 · SOIL RETURN · WATER HELD

04Return

Into the soil, where it holds water and nutrients, and holds its carbon for centuries. The terra preta soils of the Amazon still carry theirs after two thousand years.

What it does

Carbon removed. Soils enriched.

For the climate

Removal, not avoidance

A tonne of biochar holds carbon equivalent to roughly 2.9 tonnes of CO₂ gross (measured from its carbon content, not assumed) and about 1.9–2.3 tonnes net once permanence factors and lifecycle emissions are deducted. We claim the net figure, not the gross one.

Energy as a co-product

Pyrolysis releases energy-rich gases: process heat that can power the plant or a partner instead of fossil fuels.

Fire risk becomes feedstock

The residue that would fuel the next fire season becomes the input: removal that also protects the landscape.

For the soil

Water retention

The porous structure holds water where roots can reach it: measurable drought resilience in dry summers.

Nutrients stay put

Charged surfaces hold nutrients in the root zone instead of leaching into groundwater, so you get more from every unit of fertiliser.

A home for soil life

Millions of pores make ideal habitat for beneficial microbes and fungi, the engine of healthy soil structure and pH.

Why it doesn't come back

Durability, assessed from the material

Pyrolysis converts carbon into aromatic structures that microbes can't easily break down. Chemists track this with the hydrogen-to-carbon ratio: below 0.7 counts as biochar, and the lower it goes, the longer the carbon tends to last. It's also why one gram can hold hundreds of square metres of internal surface, like a tennis court folded into your palm.

2,000+

yrs of terra preta evidence

< 0.7

H/C ratio threshold

200–400 m²

surface area per gram · varies by feedstock

Illustration of biochar's porous honeycomb microstructurePore-structure image
Illustrative rendering of biochar's pore structure. Real micrographs arrive with laboratory analysis.

Beyond the field

Where biochar goes to work

Agriculture & soils

The classic use: soil amendment that improves fertility, water balance and yields, and the anchor of insetting programmes.

Construction & materials

Blended into concrete, asphalt and composites: carbon locked into the built environment while improving material properties.

Filtration & remediation

Its adsorbent surface treats water and air and helps recover contaminated soils: the activated-carbon family of uses.

Energy & engineered carbons R&D

Process heat as a co-product today; activated and engineered carbons as exploratory R&D, with no partner or programme yet. Today, the removal is the product.

Common questions

Asked and answered

Now see it become a credit

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