Abstract

The estimations of greenhouse gas (GHG) field emissions from fertilization and soil carbon changes are challenges associated with calculating the carbon footprint (CFP) of agricultural products. At the regional level, the IPCC Guidelines for National Greenhouse Gas Inventories (2006a) Tier 1 approach, based on default emission factors, insufficiently accounts for emission variability resulting from pedo-climatic conditions or management practices. However, Tier 2 and 3 approaches are usually considered too complex to be practicable. In this paper, we discuss different readily available medium-effort methods to improve the accuracy of GHG emission estimates. We present four case studies—two wheat crops in Germany and two peach orchards in Italy—to test the performance of Tier 1, 2, and 3 methodologies and compare the estimated results with available field measurements. The methodologies selected at Tier 2 and Tier 3 level are characterized by simple implementation and data collection, for which only a medium level of effort for stakeholders is required. The Tier 2 method consists of calculating direct and indirect N2O, emissions from fertilization with a multivariate empirical model which accounts for pedo-climatic and crop management conditions. The Tier 3 method entails simulation of soil carbon stock change using the Rothamsted carbon model. Relevant differences were found among the tested methodologies: in all case studies, the Tier 1 approach exceeded the Tier 2 estimations for fertilizer-induced emissions (up to +50 %) and the measurements. Using this higher Tier approach reduced the estimated CFP calculation of annual crops by 4 and 21 % and that of the perennial crop by 7 %. Removals related to positive soil carbon change calculated using the Tier 1 approach also exceeded the Tier 3 calculations for the studied annual crops (up to +90 %) but considerably underrated the Tier 3 estimations and measurements for perennial crops (−75 %). In this case, the impact of the selected Tier method on the final CFP results was even more relevant: an increase of 194 and 88 % for the studied annual crops and a decrease of 67 % for the perennial crop case study. The use of higher Tiers for the estimation of land-based emissions is strongly recommended to improve the accuracy of the CFP results. The suggested medium-effort methods tested in this study represent a good compromise between complexity reduction and accuracy improvement and can be considered reliable for the assessment of GHG mitigation potentials.

Highlights

  • Agriculture accounts for one third of global greenhouse gas (GHG) emissions (Lal and Kimble 1997)

  • The aim of the present paper is to provide to carbon footprint (CFP) practitioners higher Tier methods Breadily available^ and Beasy to implement^ to assess field emissions from fertilization and from soil carbon change consequent to crop management change for the inclusion into CFP assessment studies of agricultural products

  • The curves resulting from the Rothamsted C (RothC) simulation are very different, because site 1 is characterized by lower soil clay content and a moister climate, which leads to a slower rate of soil organic carbon (SOC) rise due to the faster decomposition rate of soil C pools

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Summary

Introduction

Agriculture accounts for one third of global greenhouse gas (GHG) emissions (Lal and Kimble 1997). If demand for food and biomasses continues to increase, annual GHG emissions from agriculture may increase proportionally, along with the vulnerability of agro-ecosystems to climate change (Xiong and Khalil 2009). Agriculture has a significant potential to reduce GHG emissions, as soils are the second largest carbon (C) sink after oceans (Lal and Kimble 1997). There are three options for climate change mitigation in agriculture. GHG emissions can be reduced by improving the management of C and nitrogen (N) flows in agro-ecosystems. Increasing the level of temporary C storage through improved agricultural management practices can increase soil C sequestration. The replacement of fossil fuels with renewable fuels such as residues from agricultural crop production is possible

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