dc.creatorVarela, María Florencia
dc.creatorBarraco, Miriam Raquel
dc.creatorGili, Adriana Anahí
dc.creatorTaboada, Miguel Angel
dc.creatorRubio, Gerardo
dc.date.accessioned2018-08-22T11:48:21Z
dc.date.accessioned2023-03-15T13:55:41Z
dc.date.available2018-08-22T11:48:21Z
dc.date.available2023-03-15T13:55:41Z
dc.date.created2018-08-22T11:48:21Z
dc.date.issued2017-01
dc.identifier0002-1962
dc.identifier1435-0645
dc.identifierhttps://doi.org/10.2134/agronj2016.03.0168
dc.identifierhttp://hdl.handle.net/20.500.12123/3139
dc.identifierhttps://dl.sciencesocieties.org/publications/aj/abstracts/109/1/317?access=0&view=pdf
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/6206388
dc.description.abstractUnder no-tillage field conditions, cover crop (CC) residues remain on the soil surface and decompose at a slow rate. We used three CC species (oat, Avena sativa L.; rye, Secale cereale L.; and ryegrass, Lolium multiflorum L.) to evaluate the residue biomass decomposition and P pools release–total phosphorus (Pt), inorganic phosphorus (Pi), and organic phosphorus (Po)–under no-tillage field conditions. The dynamics of biomass and P in CC residues was evaluated through the litterbag method during two annual periods in a long-term field experiment. Exponential decay models were fitted to each variable. Biomass decomposition and P release followed asymptotic decay models for the less labile residues (oat and rye) and single exponential decay models for the more labile ryegrass residues. Biomass and Pt showed rather equivalent dynamics, but Pi release was faster (Pi rates were three times higher and Pi plateaus were two to four times lower than biomass values). The release of Pt from CC residues reached agronomically significant quantities (2–16 kg ha–1) during the cash crop growing season and most of this Pt was released as Pi (53–100%). A positive tradeoff was observed between the release of Pi, potentially available for subsequent crop, and the residue biomass remaining over the soil. This means that Pi was released from residues, but enough biomass remained on the soil surface for erosion control. These results can be incorporated into predictive models on the contribution of CC residues to soil coverage and P nutrition of subsequent crops.
dc.languageeng
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.sourceAgronomy journal 109 (1) : 317-326. (2017)
dc.subjectBiomasa
dc.subjectPlantas de Cobertura
dc.subjectFósforo
dc.subjectCero-labranza
dc.subjectForrajes
dc.subjectBiomass
dc.subjectCover Plants
dc.subjectPhosphorus
dc.subjectZero Tillage
dc.subjectForage
dc.titleBiomass Decomposition and Phosphorus Release from Residues of Cover Crops under No-Tillage
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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