Key Points

  • Total organic carbon is a measure of the carbon contained within soil organic matter.

  • Continuous pasture builds organic carbon quicker than other rotations.

  • Plant residue removal and constraints to crop growth reduce organic inputs.

  • Erosion events remove topsoil which contains the bulk of a soil’s organic matter. This can take years of good management to replace.

  • Miro-organisms breakdown soil organic carbon for energy-this occurs faster when the soil is moist, warm and when cultivation aerates and exposes carbon protected in soil aggregates.

  • Gravel in soils will ‘dilute’ the total carbon in your paddock when total organic carbon is calculated on a per hectare basis.



The term organic is used to describe materials relating to or derived from living organisms. Management practices and plant inputs influence both the quantity and quality of soil organic matter, which directly impacts on soil productivity, soil resilience and soil sustainability. Soil organic matter plays a key role in nutrient cycling and can help improve soil structure.

Carbon makes up approximately 50% and nitrogen 0.5-10% (dependent on residue type) of the molecules in organic matter; some of which turns over rapidly (labile fraction) and is available to plants, whilst other more recalcitrant forms (passive, slow turnover fractions) contribute to the stable organic pools. Soil micro-organisms breakdown (i.e. decompose, mineralise) organic matter to obtain carbon, nitrogen and other nutrients for their own growth and activity. In doing so they release carbon dioxide (CO2) into the atmosphere.


The role of organic carbon

Total organic carbon influences many soil characteristics including colour, nutrient holding capacity (cation and anion exchange capacity) and, nutrient turnover and stability, which in turn influence water relations, aeration and workability.

In soils with high clay content the contribution to cation exchange from the organic fraction is generally small compared to that from clay. In sandier soils the relative contribution of the organic fraction is higher because there is less clay, even though the amount of total organic carbon present may be similar to, or less than, that in clays.

By providing a food source for micro-organisms, organic carbon can help improve soil stability by micro-organisms binding soil particles together into aggregates or ‘peds’. Bacteria excretions, root exudates, fungal hyphae and plant roots can all contribute to better soil structure.

Moist, hot and well-aerated conditions favour rapid decay of organic additions. If the rate of organic matter addition is greater than the rate of decomposition, the organic fraction in a soil will increase (figure 1). Conversely, if the rate at which organic matter is added to soil is lower than the decomposition rate, the organic fraction will decline.

At a steady state level, the rate of addition is equal to the rate of decomposition. Large organic additions can temporarily increase the organic fraction in a soil, but unless additions are maintained, the soil will revert to its steady state equilibrium, which is usually low.


Figure 1: An example of organic carbon levels over time under different management systems.



An understanding of the different components of soil organic matter is required to best use it to improve farming systems.

Total carbon is the sum of three carbon forms: organic, elemental (which is insignificant in most soils) and inorganic (usually carbonates and bicarbonates). Total carbon is different to total organic carbon.

Total organic carbon forms are derived from the decomposition of plants and animals. They are capable of decay or are the product of decay. They contain organic compounds whose molecules contain carbon, oxygen, nitrogen and hydrogen; therefore carbonates, bicarbonates and elemental carbon, like graphite, are not organic carbon. Total organic carbon, soil organic carbon and organic carbon are the same.

Organic matter is commonly, and incorrectly, used to describe the same soil fraction as total organic carbon. Organic matter is different to total organic carbon in that it includes all the elements (hydrogen, oxygen, nitrogen, etc.) that are components of organic compounds, not just carbon. Organic matter is difficult for laboratories to measure directly, so they usually measure total organic carbon. This is probably why organic matter and organic carbon are often confused. A conversion factor of 1.72 is commonly used to convert organic carbon to organic matter:

Organic matter (%) = Total organic carbon (%) x 1.72

This conversion factor assumes organic matter contains 58% organic carbon. However this can vary with the type of organic matter, soil type and soil depth. Conversion factors can be as high as 2.50, especially for subsoils.

Total organic carbon can be further defined as fractions that vary in size and decomposability. The ‘passive’ fraction is chemically stable and can take more than 2500 years to turnover. Consequently, it is the largest pool and the least likely to be influenced by changes in management practice.

The ‘stable’ fraction, with a turnover rate of 20-40 years, consists primarily of organic compounds that are either resistant to decomposition or physically protected. Soil manipulations that disrupt soil aggregates (e.g. tillage) can influence the turnover of this pool, by exposing previously protected organic material to microbial decomposition.

The ‘active’ or ‘labile’ fraction consists of smaller pools that can be readily utilised by micro-organisms. This fraction originates from new residues and living organisms (including micro-organisms) and turnover generally occurs within 2-3 years. The microbial component of this fraction represents only 1-5% of total soil organic matter. However, since this soil fraction is more sensitive to changes in management practices, significant differences can generally be measured earlier than in the larger, more stable pools. The capacity of a soil to supply nutrients is often defined by the proportion of total organic carbon that is labile.


Gravel in soil

In converting total organic carbon (%) to a tonne per hectare basis, it is important to account for gravel content in the soil. Total organic carbon is measured only on those soil particles that are less than 2 mm, everything larger is classed as gravel. If there is a significant gravel fraction in your soil, this means that the organic carbon is concentrated into only the less than 2 mm component of the soil. So for any measured total organic carbon (%), the more gravel in the soil, the lower the tonnes of organic carbon per hectare when gravel is taken into account.


Organic carbon in your paddock

Soil organic carbon is usually reported as a percentage of your topsoil (0-10 cm). This value can be converted to a meaningful volume for a paddock. For example:

i.e. 10 000 m2 in one hectare × 0.1 m soil depth × 1.4 g/cm3 bulk density × 1.2% = 16.8 t/ha.


Further reading and references

The New South Wales Department of Primary Industries has further information on soil carbon (online)

Authors: Wayne Pluske (Nutrient Management Systems), Daniel Murphy (The University of Western Australia), Jessica Sheppard (Avon Catchment Council)

Revised for NSW: Abigail Jenkins (New South Wales Department of Primary Industries), 2015

The National Soil Quality Monitoring Program is being funded by the Grains Research and Development Corporation, as part of the second Soil Biology Initiative.

The participating organisations accept no liability whatsoever by reason of negligence or otherwise arising from the use or release of this information or any part of it.

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