RESUMOA cana-de-açúcar é a principal cultura utilizada na produção de etanol biocombustível no Brasil e sua colheita pode ser feita com ou sem queima das folhas, aumentando ou diminuindo a emissão de gases do efeito estufa e a deposição de C no solo. Por meio deste trabalho, avaliou-se o efeito de sistemas de colheita de cana-de-açúcar (com e sem queima da palha, com um, três e seis anos após a última reforma do canavial) sobre os teores e estoques de C no solo, a qualidade física da matéria orgânica e a imobilização de C na biomassa microbiana do solo. As áreas de colheita sem queima apresentaram maior teor de C na camada superficial e maiores estoques de C, independentemente do tempo após a última reforma. Diferenças na qualidade física da matéria orgânica ocorreram principalmente na fração com tamanho entre 53 e 75 µ µ µ µ µm, na qual a proporção de C foi maior nas áreas sem queima. Na camada de 0-10 cm, o sistema sem queima apresentou maior teor de C microbiano. A colheita sem queima da palha é eficiente em acumular C em formas que possuem alto tempo de residência no solo.Termos de indexação: aquecimento global, cana crua, fracionamento físico, manejo do solo, matéria orgânica do solo.

Soil quality (SQ) is the ability of soil to provide ecosystem functions and services. Implementation of a certain agricultural system can affect SQ and therefore play an essential role in achieving sustainable agriculture. The aim of this study was to explore how agricultural systems (conventional vs. organic), grazing regime (non-grazed vs. grazed) and the different proportions of temporary grass-clover leys in crop rotations (ley time proportion, LTP) affect SQ within a mixed (cropping and pasture/dairy system) commercial farming enterprise in the UK. Seven SQ indicators were evaluated, including chemical (pH; available phosphorus (P); potassium (K)), physical (bulk density, BD; aggregate stability, AS) and biological (total carbon (C); microbial biomass carbon, MBC) sectors. All SQ indicators were measured at three depth intervals (0-0.15, 0.15-0.30, 0.30-0.60 m), except for AS and MBC, which were only considered for the topsoil (0-0.15 m). The findings reflected existing knowledge on the advantages of organic vs. conventional systems for SQ indicators, with the former showing higher MBC and similar K, BD, AS and C in the 0-0.30-m compared to the latter. Lower topsoil available P in organic systems can be related to the lack of measurements in all P pools. When grazing was included: (a) both agricultural systems showed higher topsoil available P, C and MBC; and (b) there was a

No abstract

Bioenergy crops, such as sugarcane, have the potential to mitigate greenhouse gas emissions through fossil fuel substitution. However, increased sugarcane propagation and recent management changes have raised concerns that these practices may deplete soil carbon (C) stocks, thereby limiting the net greenhouse gas benefit. In this study, we use both a measured and modelled approach to evaluate the impacts of two common sugarcane management practices on soil C sequestration potential in Brazil. We explore how transitions from conventional (mineral fertiliser/burning) to improved (vinasse application/unburned) practices influence soil C stocks in total and in physically fractionated soil down to one metre. Results suggest that vinasse application leads to an accumulation of soil C of 0.55 Mg ha−1yr−1 at 0–30 cm depth and applying unburned management led to gains of ∼0.7 Mg ha−1yr−1 at 30–60 cm depth. Soil C concentration in the Silt+Clay fraction of topsoil (0–20 cm) showed higher C content in unburned management but it did not differ under vinasse application. The CENTURY model was used to simulate the consequences of management changes beyond the temporal extent of the measurements. Simulations indicated that vinasse was not the key factor driving increases in soil C stocks but its application may be the most readily available practice to prevent the soil C losses under burned management. Furthermore, cessation of burning may increase topsoil C by 40% after ∼50 years. These are the first data comparing different sugarcane management transitions within a single area. Our findings indicate that both vinasse application and the cessation of burning can play an important role in reducing the time required for sugarcane ethanol production to reach a net C benefit (payback time).

Organic systems, integrated crop-livestock systems (ICL) and leys are posited as strategies to increase soil carbon (C) stocks. However, previous studies have: (i) only considered one driver of change; (ii) evaluated soil C content instead of stocks; (iii) been limited to the 0.20 m depth; (iv) used short-term leys; and (v) rarely assessed the distribution of C among soil organic matter (SOM) fractions, which relates to C stabilization. The aim of this study was to investigate the impact of conventional vs. organic agricultural systems, grazing regimes (non-grazed vs. grazed) and different proportions of temporary grass-clover leys in crop rotations (ley time proportion -LTP) on soil C stocks and C distribution among SOM fractions down to 0.60 m soil depth. SOM fractions assessed were particulate organic matter (POM > 53 μm), heavy fraction (HF > 53 μm) and mineral-associated silt and clay fraction (SC < 53 μm). There were no differences in soil C stocks between the conventional and the organic system, but the former had higher SC-C in the 0.15 m depth. Increasing the LTP associated with livestock grazing increased: (a) soil C stocks in the topsoil (0.30 m); and (b) POM-C and HF-C in the 0.15 m and POM-C in the 0.30-0.60 m depth under both agricultural systems.The inclusion of the longer grazed grass-clover leys was especially important for topsoil POM-C and HF-C under the conventional system. These results suggest that ICL systems with increasing LTP in crop rotations can play an important role in achieving a net C benefit.

Adaptations in crop rotation with the inclusion of temporary grass-clover leys and organic amendments, have been promoted as effective ways to improve soil carbon (C) sequestration and mitigate climate change in agricultural systems. However, there are still a lot of uncertainties related to i) the combined effects of different crop rotations and different fertilisation sources, e.g., organic amendments, on soil C stocks; and ii) their potential effect on C stabilisation. The objective of this study was to evaluate the effect of different arable crop rotations with varying degrees of diversity in crop type and lengths of grass-clover ley periods and fertilisation sources on soil C stocks and C stabilisation down to 0.60 m soil depth. This was investigated in a long-term factorial field experiment-combining different crop rotation (cereal-intensive conventional vs. diversified legume-intensive organic) with different lengths of grass-clover ley periods (2 vs. 3 years), fertilisation sources (mineral vs. compost), and years (samples taken at the beginning and at the last year of one complete cycle of rotation; 8 years apart)-to explore their individual and interactive effect on soil C stock and C stabilisation at two soil depths (0–0.30 and 0.30–0.60 m). Soil C stabilisation was assessed using a unique combination of three different techniques: physical fractionation for separation of C associated to organic and mineral fractions, thermal analysis combined with differential scanning calorimetry and a quadrupole mass spectrometry (TG-DSC-QMS) for physical-chemical aspects, and pyrolysis coupled with gas chromatography-mass spectrometry (Py-GC/MS) for molecular structural information. The findings showed higher soil C stocks under the diversified organic rotation with 3 years of grass-clover ley period at both soil depths, regardless of the fertilisation source or sampling year. However, the organic rotation seemed to deliver stable soil C stocks only in the subsoil layer. Compost fertilisation, in turn, increased topsoil C stocks between the two sample dates under both rotations, and it appears to be stable. These results suggested that combining a diversified organic rotation with 3 years grass-clover ley with compost fertilisation could be one way for agricultural systems to deliver stable soil C sequestration.

No abstract

No abstract