A synthesis of carbon sequestration, carbon emissions, and net carbon flux in agriculture: comparing tillage practices in the United States
2. Zero hunger
13. Climate action
11. Sustainability
0401 agriculture, forestry, and fisheries
04 agricultural and veterinary sciences
15. Life on land
01 natural sciences
7. Clean energy
0105 earth and related environmental sciences
DOI:
10.1016/s0167-8809(01)00233-x
Publication Date:
2002-10-08T11:25:55Z
AUTHORS (2)
ABSTRACT
Abstract The atmospheric CO 2 concentration is increasing, due primarily to fossil-fuel combustion and deforestation. Sequestering atmospheric C in agricultural soils is being advocated as a possibility to partially offset fossil-fuel emissions. Sequestering C in agriculture requires a change in management practices, i.e. efficient use of pesticides, irrigation, and farm machinery. The C emissions associated with a change in practices have not traditionally been incorporated comprehensively into C sequestration analyses. A full C cycle analysis has been completed for agricultural inputs, resulting in estimates of net C flux for three crop types across three tillage intensities. The full C cycle analysis includes estimates of energy use and C emissions for primary fuels, electricity, fertilizers, lime, pesticides, irrigation, seed production, and farm machinery. Total C emissions values were used in conjunction with C sequestration estimates to model net C flux to the atmosphere over time. Based on US average crop inputs, no-till emitted less CO 2 from agricultural operations than did conventional tillage, with 137 and 168 kg C ha −1 per year, respectively. Changing from conventional tillage to no-till is therefore estimated to both enhance C sequestration and decrease CO 2 emissions. While the enhanced C sequestration will continue for a finite time, the reduction in net CO 2 flux to the atmosphere, caused by the reduced fossil-fuel use, can continue indefinitely, as long as the alternative practice is continued. Estimates of net C flux, which are based on US average inputs, will vary across crop type and different climate regimes. The C coefficients calculated for agricultural inputs can be used to estimate C emissions and net C flux on a site-specific basis.
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