Priming of soil organic carbon decomposition induced by corn compared to soybean crops

The rate of soil organic carbon [CS] loss via microbial respiration [decomposition rate k, y-1], and the rate of stabilization of vegetation inputs [CV] into CS [humification rate h, y-1] are usually considered independent of CV. However, short-term laboratory studies suggest that the quality and qu...

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Otros Autores: Mazzilli, Sebastián R., Kemanian, Armen R., Ernst, Oswaldo, Jackson, Robert B., Piñeiro, Gervasio
Formato: Artículo
Lenguaje:Español
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Acceso en línea:http://ri.agro.uba.ar/files/intranet/articulo/2014mazzilli.pdf
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Aporte de:Registro referencial: Solicitar el recurso aquí
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024 |a 10.1016/j.soilbio.2014.04.005 
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245 1 0 |a Priming of soil organic carbon decomposition induced by corn compared to soybean crops 
520 |a The rate of soil organic carbon [CS] loss via microbial respiration [decomposition rate k, y-1], and the rate of stabilization of vegetation inputs [CV] into CS [humification rate h, y-1] are usually considered independent of CV. However, short-term laboratory studies suggest that the quality and quantity of CV controls k, which is often referred to as a priming effect. We investigated how the chemical composition of different residues, [corn and soybean] controls k and h under field conditions in a no-till ecosystem. Using CV-driven shifts in ?13C, we estimated changes in carbon [C] stocks, k and h of both the labile particulate organic matter fraction [CPOM] and the stabilized mineral associated organic matter fraction [CMAOM]. After two years of high C inputs [corn: 4.4Mgha-1y-1 aboveground and C:N=78; soybean: 3.5Mgha-1y-1, C:N=17], we found no changes in CPOM and CMAOM stocks in the top 5-cm of soil or in deeper layers. However, CMAOM in corn had higher k [0.06y-1] and C output fluxes [0.67Mgha-1y-1] than in soybean [0.03y-1 and 0.32Mgha-1y-1], but similar rates and fluxes in CPOM in the top 5-cm of soil. In addition, while C inputs to CPOM were also similar for both crops, C inputs from CV to CMAOM were higher in corn [0.51Mgha-1y-1] than in soybean [0.19Mgha-1y-1]. Overall, corn plots had higher k and C inputs into CMAOM and therefore higher C cycling in this fraction. Our data suggests that the type of crop residue strongly influences C cycling in the topsoil of no-till cropping systems by affecting both the stabilization and the decomposition of soil organic matter. 
650 |2 Agrovoc  |9 26 
653 0 |a AGRICULTURAL WASTES 
653 0 |a BIODEGRADATION 
653 0 |a BIOGEOCHEMISTRY 
653 0 |a BIOLOGICAL MATERIALS 
653 0 |a CARBON FLUX 
653 0 |a CHEMICAL COMPOSITION 
653 0 |a COMPARATIVE STUDY 
653 0 |a CORN 
653 0 |a CROP RESIDUE 
653 0 |a CROPS 
653 0 |a DECOMPOSITION 
653 0 |a HUMIFICATION 
653 0 |a HUMIFICATION RATE 
653 0 |a IN-FIELD 
653 0 |a MAIZE 
653 0 |a MICROBIAL ACTIVITY 
653 0 |a ORGANIC COMPOUNDS 
653 0 |a PARTICULATE ORGANIC MATTER 
653 0 |a PRIMING EFFECT IN FIELD CONDITIONS 
653 0 |a QUALITY CONTROL 
653 0 |a SOIL CARBON 
653 0 |a SOIL ORGANIC CARBON 
653 0 |a SOIL ORGANIC CARBON DECOMPOSITION 
653 0 |a SOIL ORGANIC MATTER 
653 0 |a SOIL RESPIRATION 
653 0 |a SOILS 
653 0 |a SOYBEAN 
653 0 |a STABILIZATION 
653 0 |a TOPSOIL 
653 0 |a ZERO TILLAGE 
700 1 |a Mazzilli, Sebastián R.  |9 71691 
700 1 |a Kemanian, Armen R.  |9 71692 
700 1 |a Ernst, Oswaldo  |9 42558 
700 1 |9 67510  |a Jackson, Robert B. 
700 1 |9 22554  |a Piñeiro, Gervasio 
773 |t Soil Biology and Biochemistry  |g vol.75 (2014), p.273-281 
856 |u http://ri.agro.uba.ar/files/intranet/articulo/2014mazzilli.pdf  |i En reservorio  |q application/pdf  |f 2014mazzilli  |x MIGRADOS2018 
856 |u http://www.elsevier.com/  |x MIGRADOS2018  |z LINK AL EDITOR 
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