dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorUniversidade Federal de Uberlândia (UFU)
dc.contributorUniversidade Federal do Espírito Santo (UFES)
dc.date.accessioned2018-12-11T17:28:03Z
dc.date.accessioned2022-12-19T17:20:12Z
dc.date.available2018-12-11T17:28:03Z
dc.date.available2022-12-19T17:20:12Z
dc.date.created2018-12-11T17:28:03Z
dc.date.issued2016-10-01
dc.identifierJournal of Soils and Sediments, v. 16, n. 10, p. 2354-2364, 2016.
dc.identifier1614-7480
dc.identifier1439-0108
dc.identifierhttp://hdl.handle.net/11449/177982
dc.identifier10.1007/s11368-016-1432-3
dc.identifier2-s2.0-84964562301
dc.identifier2-s2.0-84964562301.pdf
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5363288
dc.description.abstractPurpose: The mineralization/immobilization of nutrients from the crop residues is correlated with the quality of the plant material and carbon compartments in the recalcitrant and labile soil fractions. The objective of this study was to correlate the quality and quantity of crop residues incubated in the soil with carbon compartments and CO2-C emission, using multivariate analysis. Materials and methods: The experiment was conducted in factorial 4 + 2 + 5 with three replicates, referring to three types of residues (control, sugarcane, Brachiaria, and soybean), and two contributions of the crop residues in constant rate, CR (10 Mg ha−1 residue), and agronomic rate, AR (20, 8, and 5 Mg ha−1 residue, respectively, for sugarcane, soybean, and Brachiaria), evaluated five times (1, 3, 6, 12, and 48 days after incubation). At each time, we determined the CO2-C emission, nitrogen and organic carbon in the soil, and the residues. In addition, the microbial biomass and water-soluble, labile, and humic substance carbons fractionated into fulvic acids, humic acids and humin were quantified. Results and discussion: Higher CO2-C emissions occurred in the soil with added residue ranging from 0.5 to 1.1 g CO2-C m−2 h−1 in the first 6 days of incubation, and there was a positive correlation with the less labile organic soil fractions as well as residue type. In the final period, after 12 days of soil incubation, there was a higher relation of CO2-C emission with carbon humin. The sugarcane and soybean residue (20 Mg ha−1) promoted higher CO2-C emission and the reduction of carbon residue. The addition of residue contributed to an 82.32 % increase in the emission of CO2-C, being more significant in the residue with higher nitrogen availability. Conclusions: This study shows that the quality and quantity of residue added to soil affects the carbon sequestration and CO2-C emission. In the first 6 days of incubation, there was a higher CO2-C emission ratio which correlates with the less stable soil carbon compartments as well as residue. In the final period of incubation, there is no effect of quality and quantity of residue added to soil on the CO2-C emission.
dc.languageeng
dc.relationJournal of Soils and Sediments
dc.relation0,919
dc.rightsAcesso aberto
dc.sourceScopus
dc.subjectMultivariate analysis
dc.subjectResidue
dc.subjectSoil carbon pools
dc.subjectSoil respiration
dc.titleFor how long does the quality and quantity of residues in the soil affect the carbon compartments and CO2-C emissions?
dc.typeArtículos de revistas


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