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LCA Food 2012 in Saint Malo, France! - Manifestations et colloques ...

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PARALLEL SESSION 2B: EMISSIONS MODELLING 8 th Int. Conference on <strong>LCA</strong> <strong>in</strong> the<br />

Parallel session 2b: Emissions Mode ll<strong>in</strong>g<br />

Agri-<strong>Food</strong> Sector, 1-4 Oct <strong>2012</strong><br />

Soil, climate and cropp<strong>in</strong>g system effects on N2O account<strong>in</strong>g <strong>in</strong> the<br />

<strong>LCA</strong> of faba bean and cereals<br />

Pi<strong>et</strong>ro Goglio 1, 2,* , Carol<strong>in</strong>e Colnenne-David 3,4 , Claudia Di Bene 2 , Simona Bosco 2 , Patricia Laville 1 , Roma<strong>in</strong><br />

Roche 1 , Giorgio Ragagl<strong>in</strong>i 2 , Thierry Doré 4,3 , Marco Mazzonc<strong>in</strong>i 5,6 , Benoit Gabrielle 1 , Enrico Bonari 2<br />

1<br />

UMR INRA-AgroParisTech Environnement <strong>et</strong> Grandes Cultures, 78850 Thiverval-Grignon, <strong>France</strong><br />

2<br />

Landlab, Institute of Life Sciences, Scuola Superiore Sant’Anna, Via Santa Cecilia 3, 56127 Pisa, Italy<br />

3<br />

INRA, UMR 211, BP 01, 78850 Thiverval-Grignon, <strong>France</strong><br />

4<br />

AgroParisTech, UMR 211, BP 01, 78850 Thiverval-Grignon, <strong>France</strong><br />

5<br />

Dipartimento di Agronomia e Gestione dell’Agroecosistema, Faculty of Agriculture, University of Pisa, Via San Michele degli<br />

Scalzi, 2, 56124 Pisa, Italy<br />

6<br />

CIRAA Interdepartimental Centre for Agroenvironmental Research, via Vecchia di Mar<strong>in</strong>a, 6, 56122 San Piero a Grado Pisa, Italy<br />

*<br />

Correspond<strong>in</strong>g author. E-mail: pgoglio@grignon.<strong>in</strong>ra.fr, p.goglio@sssup.it<br />

ABSTRACT<br />

Greenhouse gas (GHG) emissions from soils cause uncerta<strong>in</strong>ties with<strong>in</strong> Agricultural <strong>LCA</strong>. N 2O affects global warm<strong>in</strong>g and is estimated<br />

with IPCC guidel<strong>in</strong>es, agroecosystem models or direct measurements. CERES-EGC model was used to estimate N2O emissions<br />

from faba bean and w<strong>in</strong>ter cereals grown <strong>in</strong> two trials (ICC and CIMAS) with different climates. Model outputs were compared<br />

with IPCC estimates. Simulated N2O emission patterns showed that emissions can be <strong>in</strong>dependent from fertiliser application dates or<br />

rates. This was due to soil moisture, farm<strong>in</strong>g practices such as fertiliser applications and tillage. Results showed the IPCC procedure<br />

estimated higher annual cereals emissions of 740 g N2O-N ha -1 y -1 than simulation results and a lower estimation of 304 g N2O-N ha -1<br />

y -1 for faba bean. Results revealed <strong>in</strong>clusion of climate, soil properties and management resulted <strong>in</strong> major variations of N2O emissions<br />

which CERES-EGC was able to capture. Thus, model estimates may <strong>in</strong>crease accuracy of soil GHG emission <strong>in</strong> Agricultural<br />

<strong>LCA</strong>.<br />

Keywords: agricultural <strong>LCA</strong>, N2O emissions, CERES-EGC model, cereals, faba bean<br />

1. Introduction<br />

Agriculture contributed for 18% to the Greenhouse gases (GHG) emissions of <strong>France</strong> <strong>in</strong> 2010 and 7% for<br />

the Italian emission <strong>in</strong> the same year. Despite this contribution <strong>in</strong> both countries, the agricultural sector was<br />

responsible for 87% of nitrous oxide (N2O) total emissions <strong>in</strong> <strong>France</strong> and 69% <strong>in</strong> Italy (CITEPA, <strong>2012</strong>;<br />

Romano <strong>et</strong> al., <strong>2012</strong>). N2O has a global warm<strong>in</strong>g potential 298 times higher than carbon dioxide (Forster <strong>et</strong><br />

al., 2007).<br />

N2O emissions can be estimated with IPCC emissions factors, agroecosystem models or by direct field<br />

measurements. IPCC m<strong>et</strong>hodology is based on emissions factors and accounts for m<strong>in</strong>eral and organic fertiliser<br />

applications. It also considers crop residues decomposition, organic matter m<strong>in</strong>eralisation and other<br />

sources of organic nitrogen (N) (De Kle<strong>in</strong> <strong>et</strong> al., 2006). N2O emissions from cropp<strong>in</strong>g systems may also be<br />

directly measured <strong>in</strong> field trials us<strong>in</strong>g microm<strong>et</strong>eorological systems or chambers with either automatic or<br />

manual sampl<strong>in</strong>g (Hénault and Germon, 1995, 2000; Laville <strong>et</strong> al., 1999, 2011). N2O field emissions are hard<br />

to d<strong>et</strong>ect due to their low concentration variations; therefore high sensibility and costly <strong>in</strong>struments are<br />

needed. Thus, direct measurements are expensive and time consum<strong>in</strong>g and their use is restricted to a limited<br />

s<strong>et</strong> of experimental fields (Hast<strong>in</strong>gs <strong>et</strong> al., 2010; Laville <strong>et</strong> al., 2009; Roch<strong>et</strong>te and Eriksen-Hamel, 2008).<br />

Agroecosystem models simulate most of the processes govern<strong>in</strong>g N2O emissions and their controls.<br />

They may compare favourably with field observations for assess<strong>in</strong>g GHG emissions, but require d<strong>et</strong>ailed<br />

<strong>in</strong>puts and are complex to run (Del Grosso <strong>et</strong> al., 2008). For N2O emissions, DAYCENT, DNDC, CERES-<br />

EGC models have been extensively used for various types of ecosystems (Chen <strong>et</strong> al., 2008; Del Grosso <strong>et</strong><br />

al., 2008; Gabrielle and Gagnaire, 2008; Lehuger <strong>et</strong> al., 2009; Hast<strong>in</strong>gs <strong>et</strong> al., 2010). CERES-EGC was<br />

adapted from the CERES suite of soil-crop models (Jones and K<strong>in</strong>iry, 1986), with a focus on the simulation<br />

of environmental outputs such as N2O and NO to the atmosphere. It was tested and calibrated for these environmental<br />

impacts mostly with data com<strong>in</strong>g from Europe, with reasonable success due to a Bayesian calibration<br />

procedure that proved effective when test<strong>in</strong>g the model aga<strong>in</strong>st <strong>in</strong>dependent field data (Gabrielle and<br />

Gagnaire, 2008; Lehuger <strong>et</strong> al., 2009, 2011).<br />

N2O emissions, like all the other GHG emissions from soils, are a major source of uncerta<strong>in</strong>ties with<strong>in</strong><br />

Agricultural <strong>LCA</strong>, such as soil erosion, soil organic matter dynamics, biodiversity estimation (Gu<strong>in</strong>ée <strong>et</strong> al.,<br />

2009) and ecotoxicity (Margni <strong>et</strong> al., 2002; van Zelm <strong>et</strong> al., 2009). Indeed, <strong>in</strong> recent years <strong>LCA</strong> has been<br />

used for a wide range of agricultural systems and proved to be an effective assessment to evaluate environmental<br />

impacts (Nemecek <strong>et</strong> al., 2011a, 2011b; Goglio <strong>et</strong> al., <strong>2012</strong>). Notwithstand<strong>in</strong>g <strong>in</strong> most cases soil born<br />

emissions were estimated with the IPCC m<strong>et</strong>hod which often proved to be less accurate than agroecosystem<br />

models (Gabrielle and Gagnaire, 2008).<br />

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