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organics
                                       Compost Use
                                       Mitigates
                                       Climate Change
 FACT SHEET

It is well documented that preventing organic residues from going to landfill avoids
methane emissions, and also preserves organic carbon and nutrients for beneficial use
in land management and food production. It is equally well known that on-going use of
compost improves physical, chemical and biological soil properties, and delivers a wide
range of agronomic and environmental benefits. By supplying both stable and labile
organic compounds, as well as plant nutrients and beneficial organisms, the agricultural
and horticultural use of compost also supports climate change mitigation on two fronts:
1. Removal of atmospheric carbon through soil carbon sequestration, achieved directly
   through storage of compost carbon, and indirectly through enhanced plant growth,
   which in turn contributes also to increased soil carbon levels;
2. Reduction of greenhouse gas (GHG) emissions, e.g. through reduced production and
   use of chemical fertiliser and pesticides, and through reduced irrigation.


Preventing Methane Generation                             decline depends primarily on initial soil carbon
                                                          levels, soil texture (clay content), rainfall and
In 2006/07, the Australian Organics Recycling             agricultural activities (Fig 1).
Industry diverted at least 3.7 million tonnes of
organic residues from landfill, comprising materials
such as garden and food organics, wood & timber,
biosolids, sludges, and the like. Diverting these
materials from landfill and recycling them prevented
the generation of methane equivalent to 4.28 million
tonnes CO2-e, which is almost as much as what was
recovered from landfill in 2007 (4.5 Mt CO2-e)

In addition, a minimum of 600,000 tonnes of manure
and other agricultural residues were composted,
which is recognised by the IPCC as superior manure
management compared to deep litter or dry storage,
let alone pit or liquid storage.

Declining Soil Carbon                                     Figure 1      Long-term decline of organic carbon in
The clearing of native land for agricultural use,         three soils (top 10 cm) in Southern Queensland
particularly when it involves soil cultivation, results   (Source: Dalal and Chan, 2001)
in considerable decline of soil carbon levels. It is
estimated that soil carbon levels in Australia            However, the decline of soil carbon is not a historic
declined 30% to 60% after land clearing for               phenomenon – it still is widespread today as many
cropping some 60 to 100 years ago. The rate of            soils have not yet reached new steady state carbon
                                                          levels, and as agricultural production still intensifies.
Declining Soil Productivity                                       Compost Use Sequesters Carbon
Soil organic matter (or carbon) levels are closely                Many trials in Australia and overseas have
linked with soil fertility and soil productivity.                 demonstrated that on-going compost use increases
Hence, declining organic matter results also in                   soil carbon levels. However, there are very few
diminishing soil fertility, namely in less favourable             longer-term trials that enable the modelling of
soil physical characteristics, reduced water storage              carbon sequestration associated with compost use.
and availability, and reduced nutrient (N, P, K, trace            Fortunately however, a considerable number of
elements) supply capacity.                                        long-term (50 – 160 yrs) field trials in Europe and
                                                                  North America have demonstrated the benefits of
Mineralisation of organic matter provides a constant              farmyard manure in increasing soil carbon levels. In
slow-release nutrient source in natural and also                  the short to medium term, a considerably higher
agricultural ecosystems. Hence, declining soil carbon             proportion of carbon applied in compost is retained
also delivered significant benefits: approx. 1,200 kg             in the soil then when carbon is applied in manure.
of N and 100 kg of P per hectare (at soil bulk density            With manure, 5% to 20% of applied carbon is
of 1.2 t/m3) were released per one percentage point of            retained, while carbon retention for compost ranges
carbon lost. Agriculture production benefited from                between 10% and more than 50%. Hence, it can be
this effect for a long time. However, increasingly                assumed that compost is also considerably more
unfavourable soil conditions and diminishing soil                 effective in sequestering carbon in the long-term,
nutrient supplies due to organic matter decline                   than manure is.
resulted in growing needs for mineral fertiliser and
other external inputs.                                            While it is acknowledged that increases in soil
                                                                  carbon levels will diminish over time and be limited
                                                                  by new carbon equilibria, the current assumption
Using Compost is the Solution
                                                                  that this point will be reached after about 20 years
Using compost has a two-fold benefit, as it is ideal              will have to be revised upward. Soil organic matter
for helping re-build soil fertility and re-plenish soil           levels still showed linear increases after 9 and 12
carbon and nutrient stocks, while at the same time                years of continuous compost use (Figure 2). Over a
helping mitigate climate change.                                  12-year period, around 1 tonne of carbon per hectare
                                                                  and year was sequestered for every 10 tonnes of dry
Compost contains macro and micro nutrients, a                     matter compost (garden and food organics) applied
diverse microbial population, stable organic                      per hectare. The sequestration of 1 tonne of carbon
compounds (e.g. humic compounds), and also labile                 equates to 3,670 kg of CO2-e abatement.
organic matter, which is an important source of food
and energy for the soil food web. Hence, compost is
                                                          Increase soil organic matter level (percentage-point)




not ‘naked carbon’, but rather ‘humus in the
                                                                                                                                                               Trend
making’.

The conversion of compost into humus continues
after compost is added to soil. This means that the
transformation of organic matter into microbial
biomass, energy, CO2 and stable organic
compounds, i.e. humus, continues. Although this
mineralisation process reduces the amount of
compost carbon that remains in the soil, it also
releases nutrients necessary for plant growth. Apart                                                                                           Organic matter increase
from soil type and agricultural activity, the degree to                                                                                        y = 0.012 x OM
                                                                                                                                               R2 = 0.43
which compost carbon is converted into CO2
depends on the type and age (maturity) of compost
used, as well as on environmental conditions,
                                                                                                                  Addition of compost organic matter (t DM ha-1)
primarily temperature and moisture. Research has
shown for example that 17% of the total organic
carbon added with garden and food organics                        Figure 2    Effect of long-term (9 / 12 yrs) compost
compost was converted into CO2 during a one-year                  use on soil organic matter (0 - 30 cm) in five
                                                                  locations (Fo, We, St, El, He) in Southern Germany
period. This means that 83% of all carbon added
                                                                  (Source: LTZ, 2008)
with compost was still in the soil after one year.
In line with this, a simple carbon sequestration                                 accordingly, emissions from fertilizer production
model for compost use in European conditions                                     will be reduced by around 180 kg CO2-e. Savings
predicts that a new equilibrium will be reached only                             are obviously considerably higher, if compost with
within a time frame of probably 200 and 300 years                                higher nutrient concentrations is used, such as
for annual application rates of 10 and 15 tonnes per                             products that contain food organics, biosolids or
hectare, respectively (Figure 3). Annual application                             manure. Also, while the above calculation assumes
rates between 2.5 and 5.0 tonnes per hectare prevent                             that plants utilise approximately 40% of nitrogen
further decline in soil carbon levels.                                           supplied with compost over four years, others
                                                                                 (Favoino and Hogg, 2008) have assumed that this
                                                                                 amounts to 100%, resulting also in markedly higher
                                                                                 GHG savings.

                                                                                 Most nitrogen (> 90%) contained in compost is
Soil organic matter (%)




                                                                                 organically bound, and released slowly over time.
                                                                                 Hence, if compost is applied regularly, soil nitrogen
                                                                                 and phosphorous reserves will build up in parallel to
                                                                                 increasing soil carbon levels. For each tonne of
                                                                                 carbon that is stored in the soil, i.e. converted into
                                                                                 humus, approximately 85 kg of N, 20 kg of P and 14
                                                                                 kg of S are stored also. These nutrients will be
                                                                                 released slowly and become available for plant up-
                                                                                 take at a later stage as the humus is mineralized.
                                                                                 Over time, nutrient reserves will build up, so that
                                                                                 probably 80 kg or more of N per hectare will be
Figure 3  A simple carbon sequestration model for                                supplied annually from the soil nitrogen pool (Figure
compost use (Source: Favoino and Hogg, 2008)                                     4). This resembles farming conditions shortly after
                                                                                 land clearing when soil humus levels were still high.
Based on available research data, it is estimated that
45%, 35% and 10% of carbon contained in mature
garden organics compost is retained in the soil over                                             Application: 8 t DM/ha/yr
                                                         N mineralisation from compost (kg/ha)




20, 50 and 100 year timer-frames, respectively.                                                  N content: 1.6% DM
                                                                                                 N mineralisation: 1. year = 10%; 2. year = 4%; subsequent = 2%
Hence, use of such compost at rates of 10 t DM ha-1
will be sequester carbon that is equivalent to around
• 5,000 kg CO2-e over 20 years
• 3,500 kg CO2-e over 50 years
•    1,000 kg CO2-e over 100 years


Replacement of Mineral Fertilisers
The production of mineral fertilisers is quite energy
and GHG intensive, particularly for nitrogenous
fertilisers. The supply of plant nutrients through                                                                                Years
compost use allows for a reduction in using mineral
fertiliser, and hence also a cut in GHG emissions                                Figure 4    Increasing nitrogen mineralisation due
caused by fertiliser production.                                                 to the long-term annual application of compost [8 t
                                                                                 dry matter ha-1] (Source: Amlinger et al., 2003)
The degree to which this is achieved depends on
factors such as nutrient density in compost, nutrient
                                                                                 Reduction of Nitrous Oxide Emissions
replacement efficiency, compost application rate and
the global warming potential allocated to fertilizer                             Despite the fact that nitrous oxide (N2O) emissions
manufacturing. If, for example garden organics                                   represent less than 10% of the mitigation potential
compost (N: 1.1%, P: 0.2%, K: 0.55%) is applied                                  from cropland globally, they can have a significant
annually at 10 tonnes dry matter per hectare, it could                           impact, as their global warming potential is almost
replace the use of approximately 44kg of N, 20kg of                              300 times higher than that of CO2. Consequently,
P and 55 kg of K from mineral fertilizer per year. If                            increased N2O emissions from agricultural activities
the use of urea and single superphosphate is reduced                             can negate substantial carbon sequestration gains.
The production of N2O in soil is governed by            equivalent to 5,200 kg CO2-e over a 20 year time
available mineral nitrogen (both from soil and          frame, 3,700 CO2-e over 50 years and 1,200 kg CO2-
fertilisation), soil aeration, moisture (water filled   e over 100 years. In addition, there are other,
pore space), temperature, dissolved and readily         unaccounted reductions of GHG emissions.
degradable carbon, and soil pH and salinity.
However, the overarching determinants for N2O           Hence, the use of compost
emissions are nitrogen fertilisation, nitrogen use      • can contribute to mitigating climate change,
efficiency, and oxygen supply.                          • can help open a window of opportunity (20 – 40
                                                            years) to find other means (technologies) of
The effects of compost use on N2O emissions are not         reducing / mitigating emissions,
yet clearly established, probably because compost       • is one of the fastest means of improving soil
has the potential to both reduce and enhance                carbon levels,
emissions. Generally speaking, compost has low          • is ideally suited as mitigation measure in
nitrogen concentration (ca. 1 – 3% DM), and only a          productive agricultural soils,
small proportion is present in mineral form (ca. 0 –    • fits easily into the Australian National Carbon
10% of total N). Hence, from that perspective,              Accounting System, and
compost poses little risk of causing N2O emissions.     • can attract carbon credits.
The soil aeration effect of using compost also helps
to reduce N2O release. However, on the other hand,      It is important to understand that using compost not
improved soil water holding capacity and the supply     only helps to sequester carbon and mitigate climate
of dissolved / readily degradable carbon might          change, but also delivers many agronomic,
enhance N2O emissions.                                  environmental and societal benefits. Hence,
                                                        composting and compost use must be one of the best
Other GHG Savings                                       options available for mitigating climate change,
                                                        while also enhancing agricultural production.
The use of compost delivers a further range of other
savings on GHG emissions, which are more difficult
to measure and quantify. These savings include the      References
following:
                                                        Amlinger, F., Peyer, S., Dreher, P. (2003). Current
• Reduced energy use for irrigation, due to             knowledge about nitrogen leaching in agricultural
     improved water storage and water use               systems that use compost. Final Report (in German).
     efficiency,                                        Austrian Federal Ministry for Agriculture and
• Reduced need for biocides results in reduced          Forestry, 91 pp.
     GHG emissions associated with biocide              Dalal, R. C., and Chan, K. Y. (2001). "Soil organic
     production, due to improved soil and plant         matter in rainfed cropping systems of the Australian
     health,                                            cereal belt." Australian Journal of Soil Research 39
• Reduced diesel use for soil cultivation, due to       (3): 435-464.
     improved tilth,                                    Favoino, E. and Hogg, D. (2008). “The potential role
• Increased carbon sequestration from higher            of compost in reducing greenhouse gases.” Waste
     biomass production, due to improved soil           Management & Research 26: 61-69.
     productivity,                                      LTZ [Landwirtschaftliches Technologiezentrum
• Reduced nitrogen loss that causes secondary           Augustenberg] (2008). Sustainable compost use in
     N2O emissions, due to lower nitrogen surplus       agriculture. Final Report (in German), 126 pp.
     and leaching,
• Reduced erosion that causes loss of nutrients
     and organic matter, resulting in secondary N2O
     emissions and those associated with replacing
     lost nutrients.

Summary and Outlook                                                                   The Organic Force

Apart from the prevention of methane emissions          Contact:       Johannes Biala
from landfill and the recovery of key carbon and                       The Organic Force
nutrient resources, the use of mature garden organics                  Ph 07 – 3901 1152
compost at a rate of 10 tonnes dry matter per hectare
                                                                       E: biala@optusnet.com.au
results also in GHG abatement due to carbon
sequestration and fertiliser replacement, which is

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Using Compost Mitigates Climate Change Through Carbon Sequestration

  • 1. organics Compost Use Mitigates Climate Change FACT SHEET It is well documented that preventing organic residues from going to landfill avoids methane emissions, and also preserves organic carbon and nutrients for beneficial use in land management and food production. It is equally well known that on-going use of compost improves physical, chemical and biological soil properties, and delivers a wide range of agronomic and environmental benefits. By supplying both stable and labile organic compounds, as well as plant nutrients and beneficial organisms, the agricultural and horticultural use of compost also supports climate change mitigation on two fronts: 1. Removal of atmospheric carbon through soil carbon sequestration, achieved directly through storage of compost carbon, and indirectly through enhanced plant growth, which in turn contributes also to increased soil carbon levels; 2. Reduction of greenhouse gas (GHG) emissions, e.g. through reduced production and use of chemical fertiliser and pesticides, and through reduced irrigation. Preventing Methane Generation decline depends primarily on initial soil carbon levels, soil texture (clay content), rainfall and In 2006/07, the Australian Organics Recycling agricultural activities (Fig 1). Industry diverted at least 3.7 million tonnes of organic residues from landfill, comprising materials such as garden and food organics, wood & timber, biosolids, sludges, and the like. Diverting these materials from landfill and recycling them prevented the generation of methane equivalent to 4.28 million tonnes CO2-e, which is almost as much as what was recovered from landfill in 2007 (4.5 Mt CO2-e) In addition, a minimum of 600,000 tonnes of manure and other agricultural residues were composted, which is recognised by the IPCC as superior manure management compared to deep litter or dry storage, let alone pit or liquid storage. Declining Soil Carbon Figure 1 Long-term decline of organic carbon in The clearing of native land for agricultural use, three soils (top 10 cm) in Southern Queensland particularly when it involves soil cultivation, results (Source: Dalal and Chan, 2001) in considerable decline of soil carbon levels. It is estimated that soil carbon levels in Australia However, the decline of soil carbon is not a historic declined 30% to 60% after land clearing for phenomenon – it still is widespread today as many cropping some 60 to 100 years ago. The rate of soils have not yet reached new steady state carbon levels, and as agricultural production still intensifies.
  • 2. Declining Soil Productivity Compost Use Sequesters Carbon Soil organic matter (or carbon) levels are closely Many trials in Australia and overseas have linked with soil fertility and soil productivity. demonstrated that on-going compost use increases Hence, declining organic matter results also in soil carbon levels. However, there are very few diminishing soil fertility, namely in less favourable longer-term trials that enable the modelling of soil physical characteristics, reduced water storage carbon sequestration associated with compost use. and availability, and reduced nutrient (N, P, K, trace Fortunately however, a considerable number of elements) supply capacity. long-term (50 – 160 yrs) field trials in Europe and North America have demonstrated the benefits of Mineralisation of organic matter provides a constant farmyard manure in increasing soil carbon levels. In slow-release nutrient source in natural and also the short to medium term, a considerably higher agricultural ecosystems. Hence, declining soil carbon proportion of carbon applied in compost is retained also delivered significant benefits: approx. 1,200 kg in the soil then when carbon is applied in manure. of N and 100 kg of P per hectare (at soil bulk density With manure, 5% to 20% of applied carbon is of 1.2 t/m3) were released per one percentage point of retained, while carbon retention for compost ranges carbon lost. Agriculture production benefited from between 10% and more than 50%. Hence, it can be this effect for a long time. However, increasingly assumed that compost is also considerably more unfavourable soil conditions and diminishing soil effective in sequestering carbon in the long-term, nutrient supplies due to organic matter decline than manure is. resulted in growing needs for mineral fertiliser and other external inputs. While it is acknowledged that increases in soil carbon levels will diminish over time and be limited by new carbon equilibria, the current assumption Using Compost is the Solution that this point will be reached after about 20 years Using compost has a two-fold benefit, as it is ideal will have to be revised upward. Soil organic matter for helping re-build soil fertility and re-plenish soil levels still showed linear increases after 9 and 12 carbon and nutrient stocks, while at the same time years of continuous compost use (Figure 2). Over a helping mitigate climate change. 12-year period, around 1 tonne of carbon per hectare and year was sequestered for every 10 tonnes of dry Compost contains macro and micro nutrients, a matter compost (garden and food organics) applied diverse microbial population, stable organic per hectare. The sequestration of 1 tonne of carbon compounds (e.g. humic compounds), and also labile equates to 3,670 kg of CO2-e abatement. organic matter, which is an important source of food and energy for the soil food web. Hence, compost is Increase soil organic matter level (percentage-point) not ‘naked carbon’, but rather ‘humus in the Trend making’. The conversion of compost into humus continues after compost is added to soil. This means that the transformation of organic matter into microbial biomass, energy, CO2 and stable organic compounds, i.e. humus, continues. Although this mineralisation process reduces the amount of compost carbon that remains in the soil, it also releases nutrients necessary for plant growth. Apart Organic matter increase from soil type and agricultural activity, the degree to y = 0.012 x OM R2 = 0.43 which compost carbon is converted into CO2 depends on the type and age (maturity) of compost used, as well as on environmental conditions, Addition of compost organic matter (t DM ha-1) primarily temperature and moisture. Research has shown for example that 17% of the total organic carbon added with garden and food organics Figure 2 Effect of long-term (9 / 12 yrs) compost compost was converted into CO2 during a one-year use on soil organic matter (0 - 30 cm) in five locations (Fo, We, St, El, He) in Southern Germany period. This means that 83% of all carbon added (Source: LTZ, 2008) with compost was still in the soil after one year.
  • 3. In line with this, a simple carbon sequestration accordingly, emissions from fertilizer production model for compost use in European conditions will be reduced by around 180 kg CO2-e. Savings predicts that a new equilibrium will be reached only are obviously considerably higher, if compost with within a time frame of probably 200 and 300 years higher nutrient concentrations is used, such as for annual application rates of 10 and 15 tonnes per products that contain food organics, biosolids or hectare, respectively (Figure 3). Annual application manure. Also, while the above calculation assumes rates between 2.5 and 5.0 tonnes per hectare prevent that plants utilise approximately 40% of nitrogen further decline in soil carbon levels. supplied with compost over four years, others (Favoino and Hogg, 2008) have assumed that this amounts to 100%, resulting also in markedly higher GHG savings. Most nitrogen (> 90%) contained in compost is Soil organic matter (%) organically bound, and released slowly over time. Hence, if compost is applied regularly, soil nitrogen and phosphorous reserves will build up in parallel to increasing soil carbon levels. For each tonne of carbon that is stored in the soil, i.e. converted into humus, approximately 85 kg of N, 20 kg of P and 14 kg of S are stored also. These nutrients will be released slowly and become available for plant up- take at a later stage as the humus is mineralized. Over time, nutrient reserves will build up, so that probably 80 kg or more of N per hectare will be Figure 3 A simple carbon sequestration model for supplied annually from the soil nitrogen pool (Figure compost use (Source: Favoino and Hogg, 2008) 4). This resembles farming conditions shortly after land clearing when soil humus levels were still high. Based on available research data, it is estimated that 45%, 35% and 10% of carbon contained in mature garden organics compost is retained in the soil over Application: 8 t DM/ha/yr N mineralisation from compost (kg/ha) 20, 50 and 100 year timer-frames, respectively. N content: 1.6% DM N mineralisation: 1. year = 10%; 2. year = 4%; subsequent = 2% Hence, use of such compost at rates of 10 t DM ha-1 will be sequester carbon that is equivalent to around • 5,000 kg CO2-e over 20 years • 3,500 kg CO2-e over 50 years • 1,000 kg CO2-e over 100 years Replacement of Mineral Fertilisers The production of mineral fertilisers is quite energy and GHG intensive, particularly for nitrogenous fertilisers. The supply of plant nutrients through Years compost use allows for a reduction in using mineral fertiliser, and hence also a cut in GHG emissions Figure 4 Increasing nitrogen mineralisation due caused by fertiliser production. to the long-term annual application of compost [8 t dry matter ha-1] (Source: Amlinger et al., 2003) The degree to which this is achieved depends on factors such as nutrient density in compost, nutrient Reduction of Nitrous Oxide Emissions replacement efficiency, compost application rate and the global warming potential allocated to fertilizer Despite the fact that nitrous oxide (N2O) emissions manufacturing. If, for example garden organics represent less than 10% of the mitigation potential compost (N: 1.1%, P: 0.2%, K: 0.55%) is applied from cropland globally, they can have a significant annually at 10 tonnes dry matter per hectare, it could impact, as their global warming potential is almost replace the use of approximately 44kg of N, 20kg of 300 times higher than that of CO2. Consequently, P and 55 kg of K from mineral fertilizer per year. If increased N2O emissions from agricultural activities the use of urea and single superphosphate is reduced can negate substantial carbon sequestration gains.
  • 4. The production of N2O in soil is governed by equivalent to 5,200 kg CO2-e over a 20 year time available mineral nitrogen (both from soil and frame, 3,700 CO2-e over 50 years and 1,200 kg CO2- fertilisation), soil aeration, moisture (water filled e over 100 years. In addition, there are other, pore space), temperature, dissolved and readily unaccounted reductions of GHG emissions. degradable carbon, and soil pH and salinity. However, the overarching determinants for N2O Hence, the use of compost emissions are nitrogen fertilisation, nitrogen use • can contribute to mitigating climate change, efficiency, and oxygen supply. • can help open a window of opportunity (20 – 40 years) to find other means (technologies) of The effects of compost use on N2O emissions are not reducing / mitigating emissions, yet clearly established, probably because compost • is one of the fastest means of improving soil has the potential to both reduce and enhance carbon levels, emissions. Generally speaking, compost has low • is ideally suited as mitigation measure in nitrogen concentration (ca. 1 – 3% DM), and only a productive agricultural soils, small proportion is present in mineral form (ca. 0 – • fits easily into the Australian National Carbon 10% of total N). Hence, from that perspective, Accounting System, and compost poses little risk of causing N2O emissions. • can attract carbon credits. The soil aeration effect of using compost also helps to reduce N2O release. However, on the other hand, It is important to understand that using compost not improved soil water holding capacity and the supply only helps to sequester carbon and mitigate climate of dissolved / readily degradable carbon might change, but also delivers many agronomic, enhance N2O emissions. environmental and societal benefits. Hence, composting and compost use must be one of the best Other GHG Savings options available for mitigating climate change, while also enhancing agricultural production. The use of compost delivers a further range of other savings on GHG emissions, which are more difficult to measure and quantify. These savings include the References following: Amlinger, F., Peyer, S., Dreher, P. (2003). Current • Reduced energy use for irrigation, due to knowledge about nitrogen leaching in agricultural improved water storage and water use systems that use compost. Final Report (in German). efficiency, Austrian Federal Ministry for Agriculture and • Reduced need for biocides results in reduced Forestry, 91 pp. GHG emissions associated with biocide Dalal, R. C., and Chan, K. Y. (2001). "Soil organic production, due to improved soil and plant matter in rainfed cropping systems of the Australian health, cereal belt." Australian Journal of Soil Research 39 • Reduced diesel use for soil cultivation, due to (3): 435-464. improved tilth, Favoino, E. and Hogg, D. (2008). “The potential role • Increased carbon sequestration from higher of compost in reducing greenhouse gases.” Waste biomass production, due to improved soil Management & Research 26: 61-69. productivity, LTZ [Landwirtschaftliches Technologiezentrum • Reduced nitrogen loss that causes secondary Augustenberg] (2008). Sustainable compost use in N2O emissions, due to lower nitrogen surplus agriculture. Final Report (in German), 126 pp. and leaching, • Reduced erosion that causes loss of nutrients and organic matter, resulting in secondary N2O emissions and those associated with replacing lost nutrients. Summary and Outlook The Organic Force Apart from the prevention of methane emissions Contact: Johannes Biala from landfill and the recovery of key carbon and The Organic Force nutrient resources, the use of mature garden organics Ph 07 – 3901 1152 compost at a rate of 10 tonnes dry matter per hectare E: biala@optusnet.com.au results also in GHG abatement due to carbon sequestration and fertiliser replacement, which is