For how long does the quality and quantity of residues in the soil affect the carbon compartments and CO sub(2)-C emissions?

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 so...

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Veröffentlicht in:Journal of soils and sediments 2016-10, Vol.16 (10), p.2354-2364
Hauptverfasser: De Almeida, Risely Ferraz, Silveira, Camila Haddad, Mota, Raquel P, Moitinho, Mara, Arruda, Everton Martins, Mendonca, Eduardo De Sa, La Scala, Newton, Wendling, Beno
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Sprache:eng
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Zusammenfassung: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 CO sub(2)-C emission, using multivariate analysis. 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 super(-1) residue), and agronomic rate, AR (20, 8, and 5 Mg ha super(-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 CO sub(2)-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. Higher CO sub(2)-C emissions occurred in the soil with added residue ranging from 0.5 to 1.1 g CO sub(2)-C m super(-2) h super(-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 CO sub(2)-C emission with carbon humin. The sugarcane and soybean residue (20 Mg ha super(-1)) promoted higher CO sub(2)-C emission and the reduction of carbon residue. The addition of residue contributed to an 82.32 % increase in the emission of CO sub(2)-C, being more significant in the residue with higher nitrogen availability. This study shows that the quality and quantity of residue added to soil affects the carbon sequestration and CO sub(2)-C emission. In the first 6 days of incubation, there was a higher CO sub(2)-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 CO sub(2)-C emission.
ISSN:1439-0108
1614-7480
DOI:10.1007/s11368-016-1432-3