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Freedom251 › Blog › carbon removal

Native Grassland Restoration vs. Tree Planting for Carbon Removal: How to Choose the Right Ecosystem

By Freedom251 Team · · 10 min read

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Neither trees nor grass are a universal carbon-removal winner. Restore native grassland where grassland or savanna naturally belongs; plant trees where the site is degraded former forest or another place where woodland is ecologically appropriate. Planting trees on naturally open grassland can reduce soil carbon, biodiversity and water availability, while well-designed grassland restoration can build soil carbon and recover habitat. The correct choice depends on the site’s original ecosystem, land-use history, climate, species, water balance, carbon pools and monitoring period.

Why ecosystem identity comes before a carbon target

Carbon projects often begin with a simple question: which intervention removes more carbon, restoring grass or planting trees? That framing is too broad to be reliable. A naturally open prairie, steppe, savanna or tropical grassland has different soils, roots, fire regimes, wildlife and water flows from a forest. Replacing that system with trees changes more than the amount of woody biomass visible above ground.

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The IPCC’s Climate Change and Land report states that afforestation of native grassland can reduce soil-carbon stocks. Losses in soil may reduce or even negate gains in tree biomass, dead wood and litter. The IPCC also notes that forests and non-forest ecosystems differ in surface reflectance and evapotranspiration, so the climate effect is not captured by counting trunks alone.

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The Sixth Assessment Report similarly warns that increasing woody vegetation in grassy ecosystems may provide some carbon increase but is expected to decrease biodiversity and water availability and alter services such as grazing and wood provision. Extensive tree planting on land that was naturally grassland or savanna can therefore produce carbon losses, biodiversity losses and water-balance damage.

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By contrast, a cleared or degraded site that was historically forest may be a good candidate for native forest regeneration or tree planting. The same intervention can be appropriate in one landscape and harmful in another. A credible decision starts with ecological identity, not a preconceived preference for trees or grass.

What “carbon removal” means in this comparison

The evidence available for this topic describes carbon storage and sequestration in vegetation and soil. It does not provide one standardized, head-to-head lifecycle comparison of native-grassland restoration against tree planting. Published figures therefore cannot be treated as a universal annual removal rate.

A complete carbon account should identify each pool and the time period measured:

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  • Soil organic carbon: carbon held in soil layers, including depth and sampling method.
  • Roots: living and dead root biomass, which can be substantial in perennial grasslands.
  • Above-ground vegetation: stems, leaves and, for trees, woody biomass.
  • Litter and dead wood: fallen leaves, standing dead material and woody debris.
  • Emissions and reversals: preparation, fertilizer, fire, drought, grazing changes, harvest, clearing or tree mortality.

Soil results are especially sensitive to depth. A claim measured only in the top 30 centimetres cannot be compared directly with one measured to 1 metre. Nor should a percentage change in soil carbon be presented as tonnes of carbon dioxide without stating the conversion and assumptions. The figures below remain tonnes of carbon (C), not tonnes of carbon dioxide equivalent.

How tree planting can perform on naturally grassy land

Soil-carbon losses can offset biomass gains

When trees are established on native grassland, soil disturbance, altered root inputs, changed moisture and the loss of deep-rooted grasses can reduce existing soil-carbon stocks. The IPCC reports that this reduction may offset or negate the apparent gain from above-ground biomass, litter and dead wood. A tree inventory that excludes the original soil stock can therefore overstate net removal.

Water use and streamflow change

Woody vegetation generally changes evapotranspiration and the movement of water through a landscape. In water-limited grasslands, additional trees can draw down soil moisture, reduce groundwater recharge or alter streamflow. The Sixth Assessment Report identifies reduced water availability as an expected risk of woody increases in grassy ecosystems, although the direction and magnitude depend on climate, species, soils and landscape position.

Open-habitat biodiversity can decline

Many species require open grassland rather than tree cover. Converting a grassland to woodland can remove nesting sites, forage and movement areas for grassland birds, pollinators and other organisms. It can also change fire behavior and grazing patterns. More carbon in trunks does not establish that the original ecosystem has been restored.

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Tree encroachment is not the same as forest restoration

Natural woody expansion may increase carbon in some settings, but that does not make it a universally beneficial restoration strategy. A 2020 field study in Baringo, Kenya, found that invasion by Prosopis juliflora increased soil carbon mainly in the upper 30 centimetres while suppressing herbaceous vegetation. The authors emphasize that outcomes depend on prior land use, climate and species. Invasive or poorly matched trees can create a carbon trade-off rather than a climate solution.

What native grassland restoration can do for carbon

Perennial roots place carbon below ground

Grasslands can store substantial carbon in roots and soil. Restoring perennial species, plant cover and functioning soil processes can increase carbon inputs while reducing erosion and bare ground. Gains are not automatic: results depend on species diversity, rainfall, soil texture, prior disturbance and management.

A 22-year diversity experiment

Yang and colleagues followed restoration on abandoned agricultural land for 22 years. During years 13–22, the treatment with the highest plant diversity had an annual soil-carbon storage rate 200% greater than natural succession at that site and 70% greater than monocultures. The later-period gains were associated with greater above-ground production, greater root biomass and mixtures that included multiple species, particularly C4 grasses and legumes.

Those are relative comparisons within one experiment, not a global rate. The site’s soil was more than 90% sand, had low organic matter and had experienced substantial disturbance, including herbicide use, some soil removal, plowing and disking. A wetter, clay-rich pasture or an intact rangeland would not necessarily show the same trajectory.

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A conditional FAO scenario

The Food and Agriculture Organization’s 2023 global assessment gives a scenario of 0.3 tonnes of carbon per hectare per year if available grasslands increased soil organic carbon in the 0–30 cm layer by 0.3% after 20 years of management practices intended to enhance sequestration. This is a modeled, conditional potential, not a direct comparison with trees and not a universal observed field rate.

FAO also highlights practical limits: farmers need incentives to adopt practices, and accurately measuring soil-carbon stocks and changes is difficult. A project using the scenario should disclose the assumed soil layer, 20-year period and management conditions rather than presenting 0.3 tonnes C/ha/year as a guaranteed creditable outcome.

A semi-arid Kenya field result

In Baringo, Kenya, a Scientific Reports study reported that 30 years of degraded-grassland restoration replenished soil organic carbon to 1 m depth at 1.4% per year and restored herbaceous biomass to levels found in pristine grassland. Plant biodiversity, however, remained low. The result demonstrates why a carbon or biomass improvement alone does not prove that the full ecosystem has recovered, and why a single semi-arid case should not be generalized to other regions.

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Side-by-side comparison

Decision axis Native grassland restoration Tree planting or woodland restoration
Best ecological fit Sites that were historically and naturally grassland, prairie, steppe or savanna and have lost native cover or function. Degraded land that was formerly forest or woodland, or locations where native woodland is demonstrably the natural ecosystem.
Carbon pools Soil, roots, herbaceous biomass and litter are central; changes must be measured at a stated depth. Above-ground and below-ground woody biomass, soil, litter and dead wood all matter; original soil-carbon losses must be counted.
Water implications Can improve infiltration and ground cover when matched to local rainfall and soils; outcomes are site-specific. May increase evapotranspiration and reduce water availability or streamflow in grassy, water-limited landscapes.
Biodiversity Supports open-habitat species when native diversity and structure are restored. Can benefit forest species on suitable sites but may displace grassland species when planted on open ecosystems.
Major reversal risks Drought, fire, overgrazing, invasive plants, cultivation and loss of management continuity. Drought, fire, pests, browsing, harvesting, invasive species and failure of planted trees to survive.
Evidence limits Measured rates vary strongly by soil, climate, species and history; no universal rate exists. Visible biomass can conceal soil-carbon, albedo, water and biodiversity costs on native grassland.

A site-selection framework

1. Establish what ecosystem belongs there

Use historical vegetation records, remnant native communities, local ecological knowledge, soil and climate data, fire history and landscape context. Ask whether trees were naturally present at the proposed density, not merely whether they can survive there. Distinguish a naturally open savanna with scattered trees from a forest site cleared for agriculture.

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2. Document the land-use history

Record cultivation, plowing, grazing intensity, fertilizer, herbicide, erosion, mining, soil removal, drainage and previous tree clearing. A former cropland may have depleted soil carbon and respond strongly to diverse perennial cover; an intact native grassland may already hold a large soil stock that tree planting could damage.

3. Define the carbon boundary before choosing an intervention

Specify the baseline, accounting depth, measurement intervals and included pools. For grassland, include roots and soil as well as shoots. For trees, include soil, litter and dead wood and subtract preparation emissions and expected losses. Keep carbon (C) separate from carbon dioxide (CO2); if a project converts units, it should state the stoichiometric factor and all assumptions.

4. Screen water and biodiversity constraints

Map groundwater dependence, seasonal streams, wetlands, recharge areas and downstream users. Identify open-habitat species and legally protected communities. A project that increases measured carbon while reducing water availability or eliminating priority habitat may fail its broader restoration objective.

5. Select locally appropriate native species

For grassland, use species and genetic provenance suited to the site’s rainfall, soils, disturbance and grazing regime. A native prairie seed mix can be a useful physical-product category, but no universal commercial blend is appropriate for every region. Confirm local provenance, species fit and invasive-plant controls with regional restoration practitioners or native-seed suppliers.

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6. Set a realistic permanence and management plan

State how long the intervention is expected to persist and who will manage it. Include fire, grazing, drought, invasive species, pest outbreaks and possible land-use conversion. Grassland restoration may require adaptive grazing or periodic disturbance; tree projects need survival checks, protection from browsing and plans for fire and drought.

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Monitoring that can distinguish real gains from misleading signals

Build a baseline before intervention

Sample representative plots before planting or restoration. Record vegetation composition, cover, above-ground biomass, root indicators, soil-carbon concentration, bulk density, soil depth, moisture and erosion. Without baseline and bulk-density data, a later change in soil concentration may not represent a change in carbon stock.

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Measure soil by depth and over time

Report sampling layers such as 0–30 cm or 0–1 m, the number and location of cores, laboratory method and uncertainty. Repeat measurements on a schedule long enough to detect change; annual variation in rainfall and plant growth can obscure a trend. Do not compare a 30-centimetre scenario with a one-metre field result as though they measured the same pool.

Track ecological outcomes alongside carbon

  • Native species richness and functional diversity.
  • Herbaceous biomass and tree or shrub cover.
  • Invasive-species abundance.
  • Groundwater, soil moisture, streamflow or spring persistence where relevant.
  • Grazing capacity, forage quality and access for local users.
  • Fire frequency, severity and post-fire recovery.

The Kenya study shows why this broader dashboard matters: herbaceous biomass and soil carbon recovered while plant biodiversity remained low.

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Use controls where possible

Reference plots, untreated controls or paired sites help separate restoration effects from rainfall cycles and regional trends. A project should disclose whether its result is an observed field measurement, a model scenario or a relative comparison within an experiment.

Common mistakes and how to correct them

Mistake: counting tree biomass as the whole climate result

Correction: include soil-carbon change, litter, dead wood, roots, preparation emissions, water effects and reversal risks. On native grassland, soil losses can offset the biomass increase.

Mistake: treating the 0.3-tonne FAO figure as a guaranteed rate

Correction: label it as FAO’s conditional 2023 scenario for a 0.3% increase in soil organic carbon in the top 0–30 cm after 20 years of sequestration-enhancing management.

Mistake: transferring one experiment to every grassland

Correction: explain that the 22-year diversity experiment occurred on highly sandy, low-organic-matter, disturbed former agricultural soil. Use local trials or conservative estimates for other sites.

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Mistake: assuming more trees means better restoration

Correction: test whether the historical ecosystem was open, assess grassland-dependent species and model water effects before adding woody cover.

Mistake: declaring success from biomass alone

Correction: monitor native diversity, invasive plants, soil, water and services such as grazing. Carbon is one outcome, not the definition of ecosystem recovery.

Practical decision rules

  • Choose native grassland restoration when evidence shows the site is naturally grassland or savanna, especially where open-habitat biodiversity, grazing and water availability are priorities.
  • Choose native forest regeneration or tree planting when the site is demonstrably former forest or woodland and tree cover fits local soils, rainfall, biodiversity and water constraints.
  • Use a mixed design only where the natural system is mixed. A savanna or woodland–grassland mosaic should reflect its historical structure rather than applying uniform tree density.
  • Defer a carbon claim when baseline soil data, land-use history or permanence arrangements are insufficient to calculate net change.

Bottom line for project developers and land managers

Native grassland restoration is often the ecologically grounded carbon strategy on naturally grassy land because it protects existing soil carbon, open-habitat biodiversity and water functions while rebuilding below-ground carbon. Tree planting is better suited to degraded former forest or other sites where woodland is the natural endpoint. The strongest project is not the one with the most trees or the largest modeled number; it is the one that restores the right ecosystem, counts every relevant carbon pool, measures results at appropriate depths and time scales, and reports water, biodiversity and livelihood effects alongside carbon.

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