O cultivo de plantas de cobertura, no outono/inverno, na região do Planalto do Rio Grande Sul contribui para o sucesso do sistema plantio direto. No entanto, informações relativas à produção de fitomassa e decomposição de resíduos dessas espécies ainda são escassas para a região, sobretudo para espécies consorciadas. O experimento foi conduzido em Não-Me-Toque, RS, em um Latossolo Vermelho distrófico típico, avaliando-se nove tratamentos, sendo quatro constituídos por plantas de cobertura em culturas puras [centeio (Secale cereale L.), aveia-preta (Avena strigosa Schreb), ervilha forrageira (Pisum sativum subesp. arvense) e nabo forrageiro (Raphanus sativus L. var. oleiferus Metzg)] e cinco por consórcios [(centeio + ervilha forrageira, centeio + nabo forrageiro, aveia + nabo forrageiro, centeio + ervilhaca (Vicia sativa L.) e aveia + ervilhaca)]. A dinâmica de decomposição dos resíduos culturais das plantas de cobertura foi avaliada em bolsas de decomposição, as quais foram distribuídas na superfície do solo e coletadas aos sete, 14, 21, 28, 57, 117 e 164 dias. O consórcio entre leguminosas e crucífera com gramíneas resultou em maior produção de fitomassa em relação ao cultivo destas em culturas puras. O nitrogênio (N) acumulado na parte aérea dos consórcios formados por ervilha forrageira e nabo com centeio e aveia foi semelhante ao da leguminosa e da crucífera em culturas puras e superou em 220,4 % os valores de N observados para as gramíneas em culturas puras. Por meio do consórcio entre as espécies de cobertura foi possível reduzir a taxa de decomposição dos resíduos culturais, em comparação com as culturas puras da leguminosa e da crucífera.

Crop residues decomposition are controlled by chemical tissue components. This study evaluated changes on plant tissue components, separated by the Van Soest partitioning method, during cover crop decomposition. The Van Soest soluble fraction was the first to be released from the crop residues, followed by cellulose and hemicellulose. Lignin was the crop residue component that suffered the least degradation, and for certain crop residue types, lignin degradation was not detected. The degradation of the main components of crop residues (soluble fraction, cellulose, hemicellulose and lignin) is determined by the chemical and structural composition of each fraction.

Pastures are of central importance in food production and provide multiple ecosystem services. The objective of this paper was to determine whether the intensification of pasture-based animal production systems, through practices such as fertilization and improved pasture species, has a higher capacity in the short-term (five years) to sequester carbon in the soil compared to (1) natural grassland without anthropogenic interactions, (2) natural grassland fertilized and overseeded with exotic species, and (3) annual pastures with frequent soil disturbance. The study assessed the organic carbon stock (OCS), total organic carbon (TOC), particle size, porosity, and density at different soil strata, as well as the root system and forage production. Forage dry matter (DM) production varied significantly with means ranging from 6615 to 13,000 kg ha^–1 year^–1 for natural grassland (NG) and permanent pasture (PP), respectively. Improved natural grassland (ING) and NG presented a higher density and root diameter than PP and annual pasture (AP). Forage systems significantly influenced soil porosity and density, with NG and ING showing lower soil densities and higher soil porosities. The OCS (0–100 cm) was similar between NG (270 Mg ha^–1), ING (255 Mg ha^–1), PP (274 Mg ha^–1), and AP systems (256 Mg ha^–1). Over a period of five years, the intensification of pasture-based animal production systems did not have a significant impact on OCS in the soils of a Brazilian subtropical highland.

Native grassland supports extensive livestock production in the Pampas of South America, but the impact of cattle excreta on nitrous oxide (N2O) emissions remains unknown in this biome. The objective of this study was to determine the N2O emission factor (EF-N2O, % of N applied that is emitted as N2O) for urine and dung from beef cattle grazing on native grasslands. A field trial was conducted under low and moderate forage allowances (FA4 and FA12; i.e. 4 and 12 kg dry matter/100 kg live weight respectively) during the 30th year of a long-term grassland experiment on a Typic Paleudult in South Brazil. Urine and dung were applied onto separate patches, at rates equivalent to one average urination or defecation; and N2O fluxes were monitored with closed static chambers over 338 days. In adjacent microplots receiving the same excreta treatment, water-filled pore space, nitrate, ammonium and extractable dissolved organic carbon were monitored in the top 0.1 m of soil. Averaged across the forage allowances, daily soil N2O fluxes were low in the control without excreta (1.3 g N ha–1), but increased upon application of dung (3.8 g N ha–1) and urine (66 g N ha–1). The annual N2O emission and the EF-N2O for urine were greater under FA12 than FA4, but no difference was observed for dung. The positive relationships between N2O-N emissions and ammonium intensity and nitrate intensity suggest that N2O may have been produced concurrently by nitrification, nitrifier/denitrification and denitrification. On average, the EF-N2O was almost 10 times higher for urine than for dung (0.74% vs 0.08%), both much lower than the IPCC’s Tier 1 default value of 2%. Our findings reinforce the need for disaggregating the EF-N2O for urine and dung and of revising the IPCC’s Tier 1 EF-N2O.