5 research outputs found

    Root and Shoot Contribution to Carbon and Nitrogen Inputs in the Topsoil Layer in No-Tillage Crop Systems under Subtropical Conditions

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    Recycling of carbon (C) and nitrogen (N) from plants into soils is decisive for maintaining soil organic matter and soil fertility. Therefore, we quantified plant biomass and C and N in the shoots and roots from the topsoil layer for a wide range of annual crops grown under subtropical conditions. We grew 26 species, 13 main crops, and 13 cover crops, in the field in standard sowing arrangements. Root biomass was recovered from the 0.00-0.20 m soil layer at flowering, and shoot biomass was measured at flowering for all crops and at maturity only for the main crops. Root dry matter (DM) exhibited an average of 14.9 ± 5.7 % of the total shoot biomass at flowering, and the mean shoot DM to root DM ratio was 6.9 (2.8-15.0) for the 26 crops considered. Leguminous species had less root DM (0.5 to 1.0 Mg ha-1) than grass species (1.1 to 2.3 Mg ha-1). The shoot C to root C ratio varied consistently with DM, while the root N to shoot N ratio varied considerably among species. Proportionally more biomass, C, and N was allocated to the root systems of grasses (Poaceae species) than non-grass species (especially Fabaceae species). The findings of this study contribute to designing rotations to include species that promote cycling of N and have high potential for adding C to the soil through roots. In this sense, the use of intercropped grasses and legumes is a promising strategy, especially for cover crops

    Root and Shoot Contribution to Carbon and Nitrogen Inputs in the Topsoil Layer in No-Tillage Crop Systems under Subtropical Conditions

    Get PDF
    Recycling of carbon (C) and nitrogen (N) from plants into soils is decisive for maintaining soil organic matter and soil fertility. Therefore, we quantified plant biomass and C and N in the shoots and roots from the topsoil layer for a wide range of annual crops grown under subtropical conditions. We grew 26 species, 13 main crops, and 13 cover crops, in the field in standard sowing arrangements. Root biomass was recovered from the 0.00-0.20 m soil layer at flowering, and shoot biomass was measured at flowering for all crops and at maturity only for the main crops. Root dry matter (DM) exhibited an average of 14.9 ± 5.7 % of the total shoot biomass at flowering, and the mean shoot DM to root DM ratio was 6.9 (2.8-15.0) for the 26 crops considered. Leguminous species had less root DM (0.5 to 1.0 Mg ha-1) than grass species (1.1 to 2.3 Mg ha-1). The shoot C to root C ratio varied consistently with DM, while the root N to shoot N ratio varied considerably among species. Proportionally more biomass, C, and N was allocated to the root systems of grasses (Poaceae species) than non-grass species (especially Fabaceae species). The findings of this study contribute to designing rotations to include species that promote cycling of N and have high potential for adding C to the soil through roots. In this sense, the use of intercropped grasses and legumes is a promising strategy, especially for cover crops

    A Roadmap for HEP Software and Computing R&D for the 2020s

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    Particle physics has an ambitious and broad experimental programme for the coming decades. This programme requires large investments in detector hardware, either to build new facilities and experiments, or to upgrade existing ones. Similarly, it requires commensurate investment in the R&D of software to acquire, manage, process, and analyse the shear amounts of data to be recorded. In planning for the HL-LHC in particular, it is critical that all of the collaborating stakeholders agree on the software goals and priorities, and that the efforts complement each other. In this spirit, this white paper describes the R&D activities required to prepare for this software upgrade.Peer reviewe

    Mineralização do carbono da palha de aveia e dejetos de suínos aplicados na superfície ou incorporados ao solo

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    A mineralização do C de dejetos de suínos e de palhas de cereais é um processo ainda relativamente pouco estudado no Brasil. O objetivo deste trabalho foi avaliar a mineralização do C da palha de aveia, dos dejetos líquidos de suínos e da cama sobreposta de suínos, aplicados na superfície ou incorporados em um Argissolo Vermelho distrófico arênico, em condições de laboratório. Utilizou-se o delineamento inteiramente casualizado, com quatro repetições dos seguintes tratamentos: solo; solo + palha incorporada; solo + palha em superfície; solo + cama sobreposta incorporada; solo + cama sobreposta em superfície; solo + dejetos líquidos incorporados; solo + dejetos líquidos em superfície; solo + palha + dejetos líquidos incorporados; e solo + palha + dejetos líquidos em superfície. Durante 80 dias de incubação, a emissão de CO2 foi medida continuamente. Ao final desse período, observou-se que foram mineralizados 59 % do C dos dejetos líquidos e apenas 23 % do C da cama sobreposta. A incorporação dos materiais orgânicos ao solo não resultou em maior mineralização do C, quando comparado à permanência desses na superfície do solo. O N amoniacal, aplicado com os dejetos líquidos de suínos, não aumentou a mineralização do C da palha de aveia.The C mineralization of pig manure and cereal straw is still relatively little studied in Brazil. The aim of this work was to evaluate C mineralization of oat straw, pig slurry and pig deep-litter, applied on the surface or incorporated in a Hapludalf soil, in laboratory conditions. The experiment was a completely randomized design with four replications of the following treatments: soil; soil + incorporated straw; soil + surface straw; soil + incorporated pig deep-litter, soil + surface pig deep-litter, soil + incorporated pig slurry; soil + surface pig slurry; soil + incorporated straw + pig slurry; and soil + surface straw + pig slurry. During the 80 days of incubation, the CO(2) emission was measured continuously. After this period, 59 % of pig slurry C had been mineralized and only 23 % of deep-litter C. The soil incorporation of organic materials did not result in. higher C mineralization, compared with organic material on the soil surface. Ammoniacal N, applied with pig slurry did not increase C oat straw mineralization

    A Roadmap for HEP Software and Computing R&D for the 2020s

    No full text
    Particle physics has an ambitious and broad experimental programme for the coming decades. This programme requires large investments in detector hardware, either to build new facilities and experiments, or to upgrade existing ones. Similarly, it requires commensurate investment in the R&D of software to acquire, manage, process, and analyse the shear amounts of data to be recorded. In planning for the HL-LHC in particular, it is critical that all of the collaborating stakeholders agree on the software goals and priorities, and that the efforts complement each other. In this spirit, this white paper describes the R&D activities required to prepare for this software upgrade
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