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hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorDEFOSSEZ, Pauline
hal.structure.identifierUnité de recherche Science du Sol [USS]
dc.contributor.authorRICHARD, Guy
hal.structure.identifierAgroscope
dc.contributor.authorKELLER, T.
hal.structure.identifierAgroressources et Impacts environnementaux [AgroImpact]
dc.contributor.authorADAMIADE, Victor
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorGOVIND, Ajit
hal.structure.identifierAgroressources et Impacts environnementaux [AgroImpact]
dc.contributor.authorMARY, Bruno
dc.date.accessioned2024-04-08T12:03:02Z
dc.date.available2024-04-08T12:03:02Z
dc.date.issued2014
dc.identifier.issn0167-1987
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/196240
dc.description.abstractEnLoss of organic matter has been recognized as being a major threat to soils in Europe with important consequences for the physical functioning of soils. We present the result of a numerical analysis of the integrated effects of changes in soil porosity and soil water status, along with decreased soil organic carbon (SOC) and the subsequent changes in the risk of compaction. This study concerns the impact of straw exportation on the risk of soil compaction. We evaluated the risk of compaction of a cultivated Eutric Cambisol in Northern France having a dominant silt loam soil texture, by simulating vehicle wheeling during sugar beet cropping for contrasting soil organic carbon contents (4.7, 11.1 and 23.4 g kg(-1)). To do this, we coupled two models: (1) a crop model (STICS) to calculate the changes in the water content of the 0-30 cm depth layer; and (2) a compaction model (COMPSOIL) to calculate soil stresses as a function of vehicle characteristics. Our study suggests that a decrease in SOC reduces the risk of topsoil deformation due to a decrease in soil water content, which tends to augment soil precompression stress. The method requires improvement in the future because it is very sensitive to input parameters for soil physical properties. Nevertheless it provides the first method for evaluating the impact of SOC decline on soil compaction. Its genericity permits it further applications to various soil management practices that decrease SOC.
dc.language.isoen
dc.publisherElsevier
dc.subjectCompaction
dc.subject.enCrop residue
dc.subject.enOrganic matter
dc.subject.enSoil quality
dc.title.enModelling the impact of declining soil organic carbon on soil compaction: application to a cultivated Eutric Cambisol with massive straw exportation for energy production in Northern France
dc.typeArticle de revue
dc.identifier.doi10.1016/j.still.2014.03.003
dc.subject.halSciences de l'environnement/Milieux et Changements globaux
dc.subject.halSciences du Vivant [q-bio]/Sciences agricoles
bordeaux.journalSoil and Tillage Research
bordeaux.page44-54
bordeaux.volume141
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-02632335
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-02632335v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Soil%20and%20Tillage%20Research&rft.date=2014&rft.volume=141&rft.spage=44-54&rft.epage=44-54&rft.eissn=0167-1987&rft.issn=0167-1987&rft.au=DEFOSSEZ,%20Pauline&RICHARD,%20Guy&KELLER,%20T.&ADAMIADE,%20Victor&GOVIND,%20Ajit&rft.genre=article


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