Carbon sequestration from soils
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Summary
As well as enhancing soil health and condition, an important reason to accumulate soil carbon is the potential to offset greenhouse gas emissions and reduce the deleterious effects of climate change through carbon sequestration in soils.
This page will help you understand:
- soil carbon sequestration processes and calculations
- the benefits of soil carbon sequestration and carbon farming
- soil carbon credit schemes and how to access calculators and supporting tools.
Carbon sequestration
Soil carbon sequestration is the process of transferring atmospheric carbon dioxide into soils through plants, plant residues, and other organic solids. By enhancing soil organic carbon (SOC) storage, land managers can help mitigate climate change whilst improving soil health, and boost agricultural productivity. Carbon farming and carbon credit schemes act as a practical method for reducing the agricultural sector’s carbon footprint while building soil resilience.
Potential environmental benefits:
- Increased soil fertility, productivity and health – through increased soil organic matter (SOM) and soil organic carbon levels.
- Improved water retention from increased SOM and therefore improved crop water use efficiency.
- Support greater diversity and productivity of soil microbes.
Potential economic benefits:
- Additional income through the Australian Carbon Credits Unit (ACCU).
- Reduced input costs, due to improved soil fertility and water retention capacity.
- Increased crop yields from improved soil productivity.
The Australian Carbon Credit Unit (ACCU) scheme supports projects that reduce gas emissions and/or sequester carbon from the atmosphere. This includes project that:
- implement changes in vegetation management to increase carbon storage
- change land use management practices to reduce/avoid greenhouse gas emissions
- use new technology or upgrade equipment to reduce energy use or emissions.
Scheme participants can earn a credit for every tonne of carbon dioxide equivalent (tCO2-e) emissions stored or reduced by their project.
Sequestering soil carbon can provide opportunities for land managers to participate in emissions reduction projects and receive financial remuneration.
Soil organic carbon is the form of carbon used to calculate sequestration. For carbon sequestration to occur, there needs to be transfer of carbon from the atmosphere (usually via plants) to storage in the soil. Conversely though, soil can also be a source of greenhouse gas emissions when exposed to soil disturbance such as through erosion, tillage or fire.
When soil organic carbon is sequestered from, or mineralised to, atmospheric CO2, a conversion factor of 3.67 is used to determine the change in mass due to the loss or gain of oxygen molecules. This is based on the ratio of the molecular weights of carbon (12) and carbon dioxide (44), that is: 44/12 = 3.67
Therefore 1 tonne of soil carbon = 3.67 tonnes of CO2 (sequestered or emitted).
Several carbon accounting calculators are available for use by farmers, agronomists and land managers in different sectors. These help identify sources of emissions, model different management scenarios for reducing emissions and optimising operations.
Some example calculators are presented below:
- Greenhouse Accounting Frameworks (GAF) for Australian Primary Industries – Primary Industries Climate Challenges Centre
- Cool Farm Tool – Cool Farm Alliance
- LOOC-C - CSIRO
- Australian Wine Carbon Calculator – Australian Wine Research Institute
- Full Carbon Accounting Model (FullCAM)
Grain Growers has prepared a report, which compares two commonly used calculators (Grains Greenhouse Gas Account Framework (G-GAF) and the Cool Farm Tool) and evaluates their suitability for supporting growers.
The inherent capacity of a soil to permanently store soil organic carbon can be increased with the addition of clay and sufficient organic matter, particularly legumes, manures and nutrients to support microbes to form soil organic carbon. However, soil organic matter and carbon can also be lost through erosion. There is a limit to the amount of organic matter and carbon that soils are able to retain, based on their mineralogy and annual rainfall.
DEW have calculated soil organic carbon benchmarks for common topsoil textures in different rainfall zones, to assist land mangers in assessing the capacity for increasing soil carbon sequestration and carbon content in their soils.
- S.O.C.R.A.T.E.S - a simple model for predicting long-term changes in soil organic carbon in terrestrial ecosystems.
- PLANR – helps you explore options for biodiversity credits (nature repair market) as well as carbon credits.
Find out more:
- Soil carbon
- Carbon accounting tools for the Australian grape and wine sector (document) - Wine Australia (2023)
- Offsetting greenhouse gas emissions through increasing soil organic carbon in SA clay-modified soils: knowledge gap analysis (report) - Goyder Institute for Water Research
- Carbon farming - PIRSA
- Australia's carbon sequestration potential - CSIRO
- Carbon calculators for different industries - carbon farming outreach program (document) - DCCEEW
- Opportunities for sequestration and emissions reduction from the NSW agricultural sector (report) - Department of Primary Industries (NSW)
- National soil strategy (report) - DAFF
Page Updated: April 2026
