ABSTRACT Leaf litter decomposition and the release of nutrients from macauba palm leaves play a major role in nutrient return to the soil in a conservation environment. This study evaluated macauba palm leaf decomposition, macronutrient contents and biochemical composition under contrasting water conditions in the Brazilian Cerrado. Macauba leaves were collected from plants in two different environments (low and high water table conditions), placed in litter bags and evaluated according to their decomposition, macronutrients, lignin, cellulose and hemicellulose for 420 days. In addition, green and dry leaves were collected for macronutrient analyses. Litter decomposition ranged between 49 % and 59 % up to 180 days. The half-life of litter ranged from 141 to 198 days. The leaf litter decomposition of macauba was practically stable during the dry season, whereas at the beginning of the rainy season, decomposition resumed. Nitrogen, P and S were higher in the green leaves, whereas the Ca levels were higher in the dry leaves. In addition, the K levels were twofold higher in the green leaves than in the dry leaves. Lignin release from macauba residues was slower than cellulose and hemicellulose. The decomposition rates of hemicellulose were higher initially due to its high solubility, although it gradually decreased with the decomposition process. Lignin decomposition was also higher at the beginning of the process but stabilized during the drought period. The study indicates that the decomposition process and nutrient cycling of macauba are influenced by its biochemical composition.

ABSTRACT: The Cerrado (Brazilian savannah) is a biome of great socio-economic and environmental importance to Brazil. The rapid agricultural expansion in the Cerrado biome areas promoted biogeochemical cycles that affect nitrogen and carbon dynamics, leading to increased greenhouse gas (GHG) emissions. In Brazil, nitrous oxide (N2O) is the main gas in agriculture, and agricultural practices increase emissions into the atmosphere. This review aimed to assess the influence of agriculture on N2O emissions in the Cerrado region, based on existing data in the literature, and extract patterns of direct N2O emissions in different agricultural systems in the Cerrado from existing data. A systematic review of data from 36 scientific publications in the Cerrado region with several crop systems revealed that N2O emissions varied from 0.15 kg ha-1 in native cerrado to 4.84 kg ha-1 in conventional tillage. Agricultural systems, nitrogen fertilizer application, and crop residues influence N2O emissions. One of the strategies to mitigate emissions is the sustainable intensification of farming systems. Cumulative N2O emissions in the Cerrado range from 0.001 to 4.84 kg ha-1 in different land-use scenarios. Soil under the conventional tillage system (CT) had the highest emissions, with an overall average of 1.58 kg ha-1 of N2O, compared to no-till system (NT) (0.82 kg ha-1) and native Cerrado 0.15 kg ha-1. Integrated crop-livestock (ICL) systems in the Cerrado had emissions with an overall average of 1.68 kg ha-1, integrated crop-livestock-forest systems (ICLF) had 1.20 ha-1, and eucalyptus plantations had 0.48 kg ha-1.

Resumo: O objetivo deste trabalho foi avaliar as frações de carbono no solo, sob plantas de cobertura cultivadas em sucessão ao milho (Zea mays), com ou sem adubação nitrogenada em cobertura, em um experimento de longa duração no Cerrado brasileiro. O experimento foi conduzido em delineamento de blocos ao acaso, em parcelas subdivididas, com três repetições. As parcelas consistiram das plantas de cobertura, e as subparcelas, da presença ou da ausência de adubação nitrogenada em cobertura para o milho. As seguintes plantas de cobertura foram plantadas, após a colheita do milho híbrido 30F53VYHR: guandu 'BRS Mandarim' (Cajanus cajan), crotalária (Crotalaria juncea), nabo-forrageiro (Raphanus sativus) e mucuna-preta (Mucuna aterrima). Após o corte das plantas de cobertura, amostras de solo foram coletadas às profundidades de 0,0‒0,10 e 0,10‒0,20 m. Após a colheita do milho, seus resíduos culturais foram coletados. As plantas de cobertura alteram as frações químicas e físicas do solo, principalmente o ácido fúlvico e o carbono orgânico particulado. A fertilização de N em cobertura no milho diminui o ácido fúlvico, mas aumenta a razão ácido húmico/ácido fúlvico e o carbono orgânico particulado na camada mais profunda do solo.

Abstract: The objective of this work was to evaluate soil carbon fractions under cover crops cultivated after corn (Zea mays), with or without nitrogen topdressing fertilization, in a long-term experiment in the Brazilian Cerrado. The experiment was carried out in a randomized complete block design, in split-plots with three replicates. The plots were represented by the cover crops, and the subplots, by the presence or absence of N topdressing for corn. The following cover crop species were planted after the harvest of the 30F53VYHR corn hybrid: 'BRS Mandarin' pigeonpea (Cajanus cajan), sunn hemp (Crotalaria juncea), oilseed radish (Raphanus sativus), and black mucuna (Mucuna aterrima). After the cutting of the cover crops, soil samples were collected at 0.0‒0.10 and 0.10‒0.20 m soil depths. After corn harvest, samples of its residues were taken. The cover crops alter the soil chemical and physical fractions, especially fulvic acid and soil particulate organic carbon. Nitrogen topdressing for corn decreases fulvic acid, but increases the humic acid/fulvic acid ratio and particulate organic carbon in the deeper soil layer.