Nitrogen Use Efficiency in an Agrisilviculture System with Gliricidia sepium in the Cerrado Region.

Gliricidia (Gliricidia sepium) is a tree legume that has great potential for use in agriculture because of its multiple-use characteristics. However, there is little information in the literature about the effect of agrisilvicultural systems on nitrogen (N) cycling. This study evaluated the effect of densities of gliricidia on N cycling under an agrisilvicultural system. The treatments were composed of different densities of gliricidia: 667, 1000 and 1333 plants ha-1, with a fixed spacing of 5 m between the alleys. The efficiency of N use was investigated by using the 15N isotope tracer. In each plot, a transect perpendicular to the tree rows was established in two positions: (i) in the corn (Zea mays) row adjacent to the trees, and (ii) in the corn row in the center of the alley. The N fertilizer recovery efficiency ranged from 39% in the density of 667 plants ha-1 to 89% with 1000 plants ha-1. The effect of gliricidia on the N uptake by corn was higher in the central position of the alley with 1000 plants ha-1. The agrisilvicultural system with 1000 plants ha-1 was highly efficient in the recovery of mineral N, representing an excellent option for integrated production systems in tropical regions.

Direct and residual effect of biochar derived from biosolids on soil phosphorus pools: A four-year field assessment.

Measures to improve the use of phosphorus (P), either by improved efficiency or reuse, are needed worldwide in order to preserve a finite resource and ensure that farmers have access to it. Currently, the rapidly growing global population has generated an increased demand for this mineral. Sustainably disposing for the massive amount of globally produced biosolids and alternative sources of P for agriculture are two major challenges to address. In this scenario, biosolids-derived biochar (BBC) has been presented as a win-win opportunity. However, the BBC-P dynamics in soil over consecutive cropping seasons remain unclear. Direct (first and second cropping season) and residual (third and fourth cropping season) effects of BBC on soil P fractions, P uptake and corn grain yield were assessed. Additionally, the relationships between soil P pools and grain yield were investigated by multivariate and multiple linear regression analysis. In a field experiment, BBC produced at 300 °C (BC 300) and 500 °C (BC 500) were applied to an Oxisol at a rate of 15 t ha-1. Soil total P and its fractions (organic P, inorganic P, and available P) were determined. Phosphorus uptake and corn grain yield were also evaluated. BBC, regardless of pyrolysis temperature, increased soil total P and all P fractions. Moreover, BBC maintained high soil P contents for at least two years after stopping its application. These results suggest that BBC may act as a slow-release P fertilizer. Surprisingly, soil P fractions were unaffected by different pyrolysis temperatures, but BC 300 promoted higher grain yield than BC 500 in the third and fourth cropping seasons. Overall, the results confirmed that under direct application both biochars can replace mineral fertilization for corn production; and when considering the residual effect, BC 300 showed a higher potential to be utilized as a soil amendment for P supply.

Recuperação de carbono obtida por três métodos em frações da matéria orgânica de latossolo, sob consórcio milho-forrageiras, no cerrado / Carbon recovery obtained by three methods in organic matter fractions of latosol under maize-grass intercropping in the cerrado

A dinâmica da matéria orgânica do solo (MOS) pode ser melhor compreendida após identificadas suas frações lábeis (> 53 µm) e estáveis (< 53 µm). Diante da importância crescente do uso de técnicas de fracionamento físico da MOS, torna-se necessário avaliar se a recuperação de carbono nessas frações é influenciada pelos métodos utilizados para sua determinação. O objetivo deste trabalho foi avaliar os teores de carbono, por três métodos, em diferentes frações da matéria orgânica, num Latossolo Vermelho-Amarelo distrófico sob consórcio milho-forrageiras e em sistema solteiro. Foram determinados os teores de carbono das frações: (i) particulada da matéria orgânica (COP) e naquela (ii) associada aos minerais da matéria orgânica (COM). Determinou-se ainda, o teor de (iii) carbono orgânico total do solo (COT) na matéria orgânica não fracionada. Três métodos de determinação do carbono orgânico do solo foram utilizados: (i) Walkley & Black modificado, (ii) Mebius modificado, e (iii) combustão via seca, em analisador elementar (CHN). Foram utilizadas amostras de solos de três sistemas de manejo dispostos em delineamento em blocos casualizados, com três repetições para determinação do carbono orgânico do solo: (i) milho solteiro; (ii) milho consorciado com capim colonião (Panicum maximum cv. Aruana); e (iii) milho consorciado com braquiária (Brachiaria humidicola). As amostras de solo foram coletadas na profundidade de 0 ­ 5 cm. O método Walkley & Black apresentou menores valores de COT em relação ao CHN nos sistemas de manejo milho/braquiária e milho solteiro, e mostrou valores de COP semelhantes àqueles obtidos pelo CHN nos sistemas de manejo milho solteiro e milho/braquiária. Valores de COT, COP e COM obtidos pela metodologia de Mebius modificado foram semelhantes àqueles obtidos pelo analisador elementar, para todos os sitemas de manejo. O COP, quando avaliado pelas metodologias de Mebius e CHN, mostrou-se significativamente mais sensível às alterações de manejo em relação ao COT e COM.

Soil organic matter alterations can be better understood when it is fractionated for the identification of its labile (> 53 µm) and stable (< 53 µm) fractions. Because of the increasing and important use of soil organic matter fractionation techniques, it becomes necessary to evaluate if the carbon recovery in these fractions is influenced by methods used for its determination. The aim of this work was to evaluate the content of organic carbon in soil organic matter fractions, by three different methods, under maize-grass intercropping and sole maize in a dystrophic Red-Yellow Latosol (Oxisol). The following carbon contents were determined from the fractions: (i) of the particulate soil organic matter (POM) and from that (ii) of mineral-associated soil organic matter (MOC). The content of total organic carbon (TOC) was also determined in the non-fractionated soil organic matter. Three methods for the determination of soil organic carbon were used: (i) Walkley & Black modified, (ii) Mebius modified, and (iii) dry combustion in a CHN elemental analyzer. The experimental design was a randomized block design with three replications. Soil samples were collected from three management systems: (i) sole corn; (ii) maize-Panicum maximum intercropping; and (iii) maize- Brachiaria humidicola intercropping. Soil samples were collected from the depth of 0 ­ 5 cm. Lower TOC were found in the Walkley & Black method in relation to the CHN elemental analyzer, under the management systems sole maize and maize-Panicum maximum intercropping. However, the Walkley & Black method showed similar POM in relation to CHN analyzer method, under the management systems sole maize and maize-Brachiaria humidicola intercropping. TOC, POM and MOC obtained from the Mebius modified method were similar to those obtained from the elemental analyzer, under the three management systems. The POM when evaluated by the Mebius and CHN methods, showed to be more sensible to soil management alterations.