Estoques e fluxos de N em sistema agroflorestal, região de Cerrado (Brasil).

Sistemas Agroflorestais surgem como opção na busca por sistemas produtivos conservacionistas, por sua diversificação e promoção de serviços ambientais. O objetivo deste estudo foi avaliar estoques e fluxos de N no sistema solo-planta-serapilheira de um SAF, em região de Cerrado do Brasil Central. O teor médio de N no solo foi 0,18%, decrescendo com a profundidade (0-20cm). O estoque médio de N no solo foi 3,08 Mg.ha-1 (0-20cm). N-NH4+ predominou em relação à N-NO3 ao longo do experimento. Maiores emissões de N2O ocorreram na transição chuva-seca de 2014, com fluxo médio de 45,9 μg m-2 h-1 N2-N2O enquanto na estação seca do mesmo ano foi 16,6 ug m-2 h-1 N2-N2O. A razão C:N da serapilheira apresentou valor médio de 20,4 ± 1,4 e concentração de N de 1,7% ± 0,2, enquanto a perda da massa foliar média no experimento de decomposição por litterbags, aos 120 dias, foi apenas 19,6%. A concentração média de N foliar para as espécies arbóreas avaliadas, foi de 2,3%, enquanto para a serapilheira o valor médio de N foi 1,5%. Assim, espécies frutíferas apresentaram taxa de retranslocação média de N de 36,6% e madeireiras 32,7%. Após ajustar a taxa de retranslocação foliar média de N, encontrou-se a taxa de 49,3%. A disponibilidade de N no solo indicou que a qualidade do material foliar das espécies plantadas, favoreceu a disponibilidade de N no sistema solo-planta-serapilheira. As taxas de retranslocação foliar de N idicaram a importância da ciclagem interna para a manutenção do N no sistema

Latin America's Nitrogen Challenge

Latin America (LA) has many social indicators similar to those of highly developed economies but most frequently falls midway between least developed countries and industrialized regions. To move forward, LA must address uncontrolled urbanization, agricultural production, social inequity, and destruction of natural resources. We discuss these interrelated challenges in terms of human impact on the nitrogen (N) cycle. Human activity has caused unprecedented changes to the global N cycle; in the past century; total global fixation of reactive N (Nr) has at least doubled (1). Excess Nr leaked into the environment negatively affects soils, atmosphere, and water resources in temperate zones (1). In addition to N excess from human impact, mining of natural soil N creates N deficits in some regions (2, 3).Fil: Austin, Amy Theresa. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura; ArgentinaFil: Bustamante, M. M. C.. Universidade Do Brasilia; BrasilFil: Nardoto, G. B.. Universidade Do Brasilia; BrasilFil: Mitre, S. K.. Universidade Do Brasilia; BrasilFil: Pérez, T.. Instituto Venezolano de Investigaciones Cientificas; VenezuelaFil: Ometto, J. P. H. B.. Centro de Previsao de Tempo e Estudos Climaticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Ascarrunz, N. L.. Instituto Boliviano de Investigación Forestal; BoliviaFil: Forti, M. C.. Centro de Previsao de Tempo e Estudos Climaticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Longo, K.. Centro de Previsao de Tempo e Estudos Climaticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Gavito, M. E.. Universidad Nacional Autónoma de México; MéxicoFil: Enrich Prast, A.. Universidade Federal do Rio de Janeiro; BrasilFil: Martinelli, L. A.. Universidade de Sao Paulo; Brasi

Balanço de massa do nitrogênio na Amazônia Brasileira: uma atualização

The main purpose of this study is to perform a nitrogen budget survey for the entire Brazilian Amazon region. The main inputs of nitrogen to the region are biological nitrogen fixation occurring in tropical forests (7.7 Tg. yr(-1)), and biological nitrogen fixation in agricultural lands mainly due to the cultivation of a large area with soybean, which is an important nitrogen-fixing crop (1.68 Tg. yr(-1)). The input due to the use of N fertilizers (0.48 Tg. yr(-1)) is still incipient compared to the other two inputs mentioned above. The major output flux is the riverine flux, equal to 2.80 Tg. yr(-1) and export related to foodstuff, mainly the transport of soybean and beef to other parts of the country. The continuous population growth and high rate of urbanization may pose new threats to the nitrogen cycle of the region through the burning of fossil fuel and dumping of raw domestic sewage in rivers and streams of the region.O principal objetivo deste estudo é realizar um balanço do nitrogênio em toda a Região Amazônica Brasileira. As principais entradas de nitrogênio na região foram a fixação biológica do nitrogênio que ocorre nas florestas tropicais (7,7 Tg.ano–1) e a fixação biológica do nitrogênio em terras agrícolas, que ocorre principalmente devido à existência de grandes áreas de cultivo de soja, uma importante cultura de fixação de nitrogênio (1,68 Tg.ano–1). A entrada em razão do uso de fertilizantes nitrogenados (0,48 Tg.ano–1) ainda é incipiente em comparação com aquelas duas outras \ud entradas mencionadas. Os maiores fluxos de saída foram o fluxo fluvial, que foi igual a 2,80 Tg.ano–1, e a exportação relacionada aos gêneros alimentícios, principalmente a transferência de soja e carne para outras regiões do País. O contínuo crescimento populacional e as elevadas taxas de urbanização podem representar novas ameaças sobre o ciclo do nitrogênio da região por meio da queima de combustíveis fósseis e do despejo de esgoto doméstico nos rios e córregos da região

Basin-wide variations in Amazon forest nitrogen-cycling characteristics as inferred from plant and soil ¹⁵N:¹⁴N measurements

Background: Patterns in tropical forest nitrogen cycling are poorly understood. In particular, the extent to which leguminous trees in these forests fix nitrogen is unclear. Aims: We aimed to determine factors that explain variation in foliar δ¹⁵N (δ¹⁵NF) for Amazon forest trees, and to evaluate the extent to which putatively N₂-fixing Fabaceae acquire nitrogen from the atmosphere. Methods: Upper-canopy δ¹⁵NF values were determined for 1255 trees sampled across 65 Amazon forest plots. Along with plot inventory data, differences in δ¹⁵NF between nodule-forming Fabaceae and other trees were used to estimate the extent of N² fixation. Results: δ¹⁵NF ranged from −12.1‰ to +9.3‰. Most of this variation was attributable to site-specific conditions, with extractable soil phosphorus and dry-season precipitation having strong influences, suggesting a restricted availability of nitrogen on both young and old soils and/or at low precipitation. Fabaceae constituted fewer than 10% of the sampled trees, and only 36% were expressed fixers. We estimated an average Amazon forest symbiotic fixation rate of 3 kg N ha¯¹ year‾¹. Conclusion: Plant δ¹⁵N indicate that low levels of nitrogen availability are only likely to influence Amazon forest function on immature or old weathered soils and/or where dry-season precipitation is low. Most Fabaceae species that are capable of nodulating do not fix nitrogen in Amazonia

Structural, physiognomic and above-ground biomass variation in savanna-forest transition zones on three continents - How different are co-occurring savanna and forest formations?

Through interpretations of remote-sensing data and/or theoretical propositions, the idea that forest and savanna represent "alternative stable states" is gaining increasing acceptance. Filling an observational gap, we present detailed stratified floristic and structural analyses for forest and savanna stands located mostly within zones of transition (where both vegetation types occur in close proximity) in Africa, South America and Australia. Woody plant leaf area index variation was related to tree canopy cover in a similar way for both savanna and forest with substantial overlap between the two vegetation types. As total woody plant canopy cover increased, so did the relative contribution of middle and lower strata of woody vegetation. Herbaceous layer cover declined as woody cover increased. This pattern of understorey grasses and herbs progressively replaced by shrubs as the canopy closes over was found for both savanna and forests and on all continents. Thus, once subordinate woody canopy layers are taken into account, a less marked transition in woody plant cover across the savanna-forest-species discontinuum is observed compared to that inferred when trees of a basal diameter > 0.1 m are considered in isolation. This is especially the case for shrub-dominated savannas and in taller savannas approaching canopy closure. An increased contribution of forest species to the total subordinate cover is also observed as savanna stand canopy closure occurs. Despite similarities in canopy-cover characteristics, woody vegetation in Africa and Australia attained greater heights and stored a greater amount of above-ground biomass than in South America. Up to three times as much above-ground biomass is stored in forests compared to savannas under equivalent climatic conditions. Savanna-forest transition zones were also found to typically occur at higher precipitation regimes for South America than for Africa. Nevertheless, consistent across all three continents coexistence was found to be confined to a well-defined edaphic-climate envelope with soil and climate the key determinants of the relative location of forest and savanna stands. Moreover, when considered in conjunction with the appropriate water availability metrics, it emerges that soil exchangeable cations exert considerable control on woody canopy-cover extent as measured in our pan-continental (forest + savanna) data set. Taken together these observations do not lend support to the notion of alternate stable states mediated through fire feedbacks as the prime force shaping the distribution of the two dominant vegetation types of the tropical lands